Showing posts with label Marine. Show all posts
Showing posts with label Marine. Show all posts

June 9, 2009

Controlling river pollution

It is imperative that rather than having a reactive approach, we need to think of a proactive approach to provide a practical and a sustainable solution to river pollution, writes M Ashiqur Rahman


RIVER water is considered polluted when it is altered from the natural state in its physical, chemical and microbiological composition and when its suitability for any safe and beneficial use becomes questionable. The signs of physical water contamination may become obvious through bad taste, offensive odours, unchecked growth of aquatic weeds, decrease in the number of aquatic animals, floating of oil and grease, colouration of water and so on. However, more intensive laboratory testing is required to determine the chemical and microbiological water quality parameters such as pH (to measure the level of acidity or alkalinity), dissolved oxygen, biological and/or chemical oxygen demand, phosphorus and nitrogen ion concentration, dissolved solids, heavy metals, salinity, coliform bacteria count and so forth.
Generally, our rivers are being polluted by the discharge of untreated industrial effluent and urban wastewater, agrochemicals, sewage water, storm runoff, solid waste dumping, oil spillage, sedimentation and encroachment. The water quality also depends on effluent types and discharge quantity from different types of industries, types of agrochemicals used in agriculture, and seasonal water flow and dilution capability by the river system. The river Buriganga is a typical example of serious surface water pollution in our country. In the present scenario this river carries only wastewater during the months (November to April) of the dry season becoming toxic during this period. The level of pollution is so high that no aquatic species can survive in it and the situation is getting worse day by day. Test results during the dry season at eight points along the river found the level of dissolved oxygen within 0.6 to 1.8 mg/l at five points and zero at other points. The requisite level of oxygen is more than 5 mg/l for the survival of aquatic lives. In fact, the Buriganga has become a dumping ground of all kinds of solid, liquid and chemical wastes which are generated by the activities in and around the river. Studies show that up to 18,500 cubic metres of liquid wastes, 19,000 kilograms of solid wastes and 17,600 kilograms of biological oxygen demand load go into the Buriganga each day from these sources. The Bangladesh Inland Water Transport Authority sources confirmed that huge quantities of discarded polythene deposits are unearthed near Sadarghat area during dredging.
Like many other countries of the world, river pollution control in Bangladesh has been a burning issue for at least the past two decades. Moreover, abundant research has been undertaken and many recommendations have been forwarded to protect the rivers from further pollution. At the government level since the late 19th century several rules, regulations, policies and strategies have been formulated and a fairly comprehensive set of environmental laws exist to save our rivers from pollution. However, the implementation and enforcement of the policies and the regulations have so far been very ineffective, leading to poorer river water quality. In addition, in many cases the policies and strategies seem far from being practical in terms of their implementation. Though it may appear to be a nightmare to overcome this serious problem but the reality is that we need to get to the core of the problem and implement strategies to safeguard these precious natural resources for the sake of our own survival. It is imperative that rather than having a reactive approach, we need to think of a proactive approach to provide a practical and a sustainable solution to the problem.
The pollution problem of our rivers have become complex because of its multidimensional nature. There are social, economic, political and environmental dimensions to this issue which need to be addressed simultaneously while attempting a sustainable solution to the problem. It is a mammoth challenge for developing countries like Bangladesh where a speedy economic growth is requisite without compromising with the conservation of the natural environment or endangering the livelihood of a particular community such as the fishermen or the farmers.
Like many other developing countries, river pollution control in Bangladesh relies on expensive and somewhat outdated technological solutions transferred from the ‘west’. Moreover, these technologies from industrial countries are not always suitable or easily adaptable to the socio-economic and environmental conditions of developing countries. So far emphasis has been given either on treatment of pollutants through the set up of effluent treatment plants or augmentation of rivers to increase the flow through the construction of river water diversion structures. Even the relocation of the pollution causing agents may not capacitate a permanent solution to the problem unless the pollutants are controlled at their sources through adopting proactive approaches such as cleaner production, recycling and resource recovery mechanism.
Experiences in countries like the United States, Australia and China show that the proactive approaches are being implemented voluntarily by the polluters to reduce their pollutants once the ‘market-based’ mechanisms are introduced. In these systems polluters are not told how much they can pollute or what technology they must use, but their choices will have financial consequences and this will influence the choices they make. With these policies, emission constraints are not source-specific; rather they provide equal incentives to all polluters by increasing the marginal costs of pollution. Moreover, several stakeholders such as producers, consumers, users, government authorities and local community members get directly involved with this process. The importance of inclusion of all the stakeholders (both who generate and manage the pollution) to develop an effective approach for pollution control cannot be undermined.
It is obvious that to protect our rivers from further pollution we need to look beyond the ineffective conventional policies and strategies. We need alternate, innovative and integrated approaches to be implemented to overcome this problem. In this regard, provisions of monetary incentives, rewards and recognitions for the polluters who reduce their pollution may work effectively for reducing the amounts of pollutants which are being discharged into the rivers. The direct involvement of community and civil society can also play a great role for this purpose.
The rivers of Bangladesh suffer from the pollution problem mostly during the dry season (November to April) but the assimilation and the dilution capacity of most of our rivers increase dramatically during the wet season (May to October). This phenomenon of the rivers overrules the application of a uniform acceptable level of the pollutants throughout the year. This opens the possibility for using ‘non-uniform reduction’ measures for the polluters and thus offers flexibility to them in terms of reducing their harmful pollutants for the water bodies.
Another significant issue is that different polluters have different levels of capacity to reduce their pollutants. Some are better off than others to control their pollutants. This tendency opens the opportunity for the application of a tradable permit system for water pollution control. This system allows pollution to be reduced wherever it is least costly to do so and a ‘cap’ guarantees the total allowable emissions are not exceeded. For instance, the Hunter River Salinity Trading Scheme of Australia leads the world in using such economic instruments for the effective protection of waterways. This scheme involves a number of point sources of salinity in the Hunter River and the average river salinity has been halved since the scheme commenced in1996, while economic activity and employment have grown substantially. It has thus become a classic example of win-win situation for all the stakeholders who are involved with the use of the river.
Regular monitoring of river water quality (physical, chemical and biological composition) is an important aspect to control river pollution. However, this is an expensive and time consuming ongoing activity which might be difficult for any government agency like the Department of Environment alone to perform the task on a regular basis. Even the powerful agencies like the Environmental Protection Agency of the United States assign this task to the community with assistance from the local administration. In Bangladesh we may think of exploring this option to ease the monitoring activity of hundreds of rivers in our country.
We need to shift from the nightmare of river pollution management to the serenity of our beautiful rivers by any means. In summary, a suggestive list of prescription is given below to help make this issue a reality.
* An action plan with its processes has to be developed on the basis of the prospective market-based instruments.
* The method of permit allocation and lifespan of permits need to be addressed.
* An information system should be established to provide potential participants relevant information on river water pollution.
* Procedures for compliance monitoring must be identified for designing a new program.
* A package of incentives, appreciation and recognition of the industries and other polluters who do better work in reducing their pollutants should be developed.
* A system of assessing the environmental reputation of the industries should be developed to measure as criteria in financial lending process.
* A guideline has to be developed for introducing the community monitoring system.
* The concern of the local community regarding the pollution has to be formally recognised by the regulatory authority.
* A strong market pressure should be created on the polluters to shift to cleaner production technologies.
* Environmental education should become mandatory from all primary to tertiary level of educational institutes.
As we would all agree the time has come to take actions to protect our rivers from further degradation and before nature takes revenge on us. However, the prerequisite of taking any action is that we need environmentally aware and enlightened people for the purpose. Awareness about the negative consequences of our harmful activities which ultimately affect our precious natural resources including rivers can minimize the damage caused to them in many folds. That is why it is high time to stress on environmental education from the primary to the tertiary level of studies in our country because learners of today are the leaders of tomorrow.

M Ashiqur Rahman, a senior lecturer of the North South University, is currently on a study leave to pursue PhD in environmental management at the University of Sydney, Australia.

NewAgeBD
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June 7, 2009

Bangladesh PM makes river pledge

In pictures: Bangladesh flood misery

The Bangladeshi Prime Minister, Sheikh Hasina, has pledged to do her utmost to save the country's "severely degraded river systems".

She said that people must be prepared for climate change and engage in more "environmentally-friendly activities".

Bangladesh is criss-crossed by rivers and creeks which are vital for irrigation and transport purposes.

The prime minister also criticised the country's weather forecasters, ordering them to be more alert about cyclones.

Last month Cyclone Aila killed at least 200 people in Bangladesh and India and left 500,000 homeless.

'Imminent catastrophe'

In a speech to mark World Environment Day, the prime minister said it was necessary to protect the country's rivers "to save people from imminent catastrophe".

"All our rivers today have lost the free flows they had in the past due to heavy silt depositions," she said.

"But once the rivers are given back their original beds, frequent overflowing will cease, reducing the negative impact of global climate change in our region."

Sheikh Hasina said that Bangladesh's ample river systems had maintained the "environmental balance since time immemorial".

She said that rivers had been losing their water-retention capacity because of "heavy siltation and unbridled encroachment".

"We must save our rivers," she said, "even though it is going to be a huge, time consuming and challenging project. But we must do it.

"Whatever the costs be, we'll do the job."

She said that rivers could be preserved through dredging and other erosion-countering measures.

The prime minister also said that more must be done to improve the country's food security whenever there are natural disasters such as floods and cyclones.

She said that developing the capacity to store food for at least two to three years was an important first step.

BBC
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June 6, 2009

Bangladesh launches campaign to save rivers

Dhaka, June 2 (IANS) Bangladesh’s lawmakers, media and industry leaders have launched a campaign to ’save’ the rivers around the national capital by evicting encroachers and improving the environment.

Called “Save rivers, Save Dhaka” campaign, the programme was launched Monday by parliament Speaker Abdul Hamid with the participation of The Daily Star newspaper and ‘i’TV channel.

Agriculture Minister Motia Choudhury assured government support. He and Speaker Abdul Hamid resolved to come up with a law that would end encroachment.

The Daily Star has undertaken a mission to focus on the dying rivers Buriganga, Turag, Balu and Shitalakhya that encircle Dhaka, the 400-year-old capital.

The newspaper has been campaigning to end the encroachment. The banks have been encroached and even ’sold’.

Bangladesh is a riverine country with numerous river systems, the larger ones being Padma, Meghna and Brahmaputra.

Poor river management, silting, absence of dredging and the rising population have reduced the country’s riverbed from 5,000 km to 3,600 km, according to a recent report of the Bangladesh Inland Water Transport Authority (BIWTA).

The government is taking measures to carry out dredging of rivers since shipping activity at its river ports, among them Chittagong, Mangla and Khulna has been badly hit.

“We must save our rivers, which have been seriously polluted and partly grabbed. Influential people whoever they are cannot be any barrier to the justified demands of common people,” said Hamid.

Abdur Razzak, chairman of the standing committee on the Ministry of Water Resources, said it is not the absence of laws, but the negligence in their application that has almost killed the rivers surrounding the capital.

News Link
Campaign on Daily Star link
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June 5, 2009

Can river silt save Bangladesh?

By Katherine Harmon in 60-Second Science Blog

Bangladeshis are already feeling the effects of climate change, especially those living on the low-lying river delta near the mouths of the Ganges. Frequent floods and stronger storms have been inundating the area with more water than many local rice growers can cope with, driving thousands to seek work in overcrowded cities.

But some rice and shrimp farmers are holding out hope that the very waters that have oft plagued them might hold the solution – in suspension. River silt, carried down in suspension from the ancient Himalayan mountains hundreds of miles away, might be able to build up land elevation to save the area's livelihoods and homes, The New York Times reports today.

In Bangladesh, deposited sediment has been slowly filling the marshy delta outward into the Bay of Bengal for the past few decades, but engineers are examining ways that it might be used to build the land up rather than out, according to the Times. The goal is to allow water to flood some especially low areas and let it out – through dams and channels – slowly. As the murky water slows, sediment drops out and filters to the bottom, leaving a new bed of silt after the water recedes. Residents in Beel Bhaina discovered this phenomenon after releasing stagnant floodwaters through an embankment; to the surprise of many, the Times reports, three feet (or more) of silt had been deposited, boosting land higher above sea level.

"Usually people are trying to get rid of the sediment," says John Gray, a hydrologist at the U.S. Geological Survey. "But here, people are using it as a resource." But Gray is skeptical that it's a viable answer. One major obstacle, he tells ScientificAmerican.com, is that it would require yet more flooding to achieve decent amount of sediment buildup.

"If they're really talking about building land," he says, "the experimental patches are a good start, but they're really going to have to start working on a much large scale."

Gray praises the effort, noting that it's "laudable" to try to "take something that most consider a nuisance" and turn it into an asset. But he warns that if massive quantities of water are diverted, unexpected consequences, such changes in river behavior, are likely to occur. Gray isn't even sure that it's a surefire stopgap against rising sea levels, which are predicted to top three feet by the end of this century. "The timing of accretion [deposit of the sediment] and the timing of the climate change, he says, "might not be compatible."

Centuries of engineering have gone into clearing river channels and mouths of silt to make them more navigable and easier to control. But as rivers have been carved out and dammed for easier navigation, sediment rushes out to sea, rather than getting deposited in the delta. This means many deltas worldwide, including the Mississippi River Delta in Louisiana, the Nile Delta in Egypt, the Yangtze Delta in China and others, are disappearing, leaving costal towns and cities more vulnerable to increasingly strong storm surges. If Bangladesh succeeds in bracing its floodplains this way, it might be a new safeguard for costal areas across the globe. But the proof will be in the (rice) pudding.

Image of Bangladeshi farmers harvesting rice in flooded fields courtesty of the International Rice Research Institute via Flickr

Scientific American
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June 4, 2009

Laws there, loopholes too

That’s not strawberry ice cream but pure toxic dyes. Untreated wastes from a single dying factory along the river Shitalakkhya create this layer of deadly froth. Hundreds of such factories have turned the river into a lifeless water body. Photo: Amran Hossain

Pinaki Roy

Not a lack of laws, but a lack of proper implementation of the existing laws is the reason for the dire condition of the country's rivers, canals, and other water bodies.

Over the years, successive governments failed to implement relevant laws for conserving the rivers and other natural water resources, resulting in rampant encroachment on those, and in their wholesale pollution by industries, while the Environment Conservation Act 1995 stayed in books.

The definition of a river is also sketchy in the laws. Generally Bangladesh Inland Water Transport Authority (BIWTA) is in charge of the rivers and riverbanks where there are river routes, under the Bengal Port Act 1908.

But if there is no river route then it becomes hard to figure out who has the authority over the rivers, as many authorities including land offices, district administrations, local governments, the water resources ministry, and the Water Development Board -- all have some kind of role or control over the rivers and riverbanks according to relevant laws.

At the moment there is no unified law that clearly defines what is a river, a riverbank, or an off shore, and lawful use of river water is also not well delineated. To save the rivers from encroachment and pollution, a unified law and a dedicated authority that will implement the law as the regulatory body, are imperative.

The first law regarding water bodies was enacted during the British colonial age in 1864 to control and collect tolls from river routes.

The Bengal Canal Act 1864 is the mother of all laws about rivers, canals and other water bodies. Beginning from that act up to the recent Open Space and Water Body Conservation Act 2000, all laws restrict changing of the characteristics of water bodies including rivers and riverbanks.

The Bengal canal act says, "It shall be lawful for the government from time to time to authorise any person to make and open any navigable channel, or to clear and deepen any navigable channel, and to stop any watercourse, make any tracking path, or do any other act necessary for the making or improvement of any such channel."

Under that law the government is authorised to 'take possession for a public purpose of any land that may be necessary for the execution of any of the above mentioned works, under the provisions of the act'.

It goes on, "Any person who shall wilfully cause ........ any obstruction to any line of navigation or any damage to the banks or works of such line of navigation, or who shall wilfully omit to remove such obstruction after being lawfully required to do so, shall be punished on conviction before a magistrate with simple imprisonment which may be extended to one month or with fine which may extend to Tk 50, or with both."

The recent significant law to protect natural water resources is titled, 'Wetland and Open Space Conservation Act, 2000', which extended the fine up to Tk 50,000, and the imprisonment up to five years, or both. But successive governments have not been very sincere to implement the law.

On the other hand, the laws specify what punishments the judiciary may mete out to the violators, but it does not direct the government to recover the original characteristics of water bodies if someone fills them up.

So once someone changes the characteristics of a river, canal, or any other water body -- it does not get back its old shape.

Other relevant laws, rules, and regulations in Bangladesh are -- the Bengal Irrigation Act 1876, East Bengal Embankment and Drainage Act 1952, Inland Water Transport Authorities Ordinance 1958, East Pakistan Irrigation (Imposition of Water Rate) Ordinance 1963, Bangladesh Water and Power Development Boards Order 1972 (President order No 59 of 1972), Bangladesh Water Rate Ordinance 1983, Land Reforms Ordinance 1984, Ground Water Management Ordinance 1985, Water Resources Planning Act 1992, Water Supply and Sewerage Authority Act 1996, National Water policy 1999, and the Act No 27 of 2000.

Daily Star
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June 2, 2009

What lies beneath

10 ft layer of polythene under Buriganga

Morshed Ali Khan

A ten-feet layer of discarded polythene bags, plastics, coconut shells, and heavy sludge created by millions of tons of biodegradable waste from kitchen markets now cover the bed of the river Buriganga.

The highest concentration of these deadly wastes have settled on the bed of the river near Sadarghat launch terminal in the capital, one of the busiest river ports in South-East Asia, according to Bangladesh Inland Water Transport Authority (BIWTA) sources.

One of the main sources of this huge amount of polythene on the riverbed is Dhaka City Corporation's (DCC) conservancy department.

Along Shaheed Nagar, Kamrangir Char, Showari Ghat, Waiz Ghat, and Shyam Bazar -- DCC conservancy workers empty their bins of household rubbish into the river everyday. Household rubbish contains a large number of polythene bags, which are too dirty for the tokais (street urchins) to sort out for sales for recycling.

DCC conservancy department's second-in-command, Dewan Shah Alam, admitted that such irregularities are taking place along the river Buriganga, but added that most of the dumping is done by private household garbage collectors, not the DCC trucks.

"We have strict instructions for all our staff involved in garbage disposal, not to dump waste anywhere other that the designated site at Amin Bazar," Shah Alam said.

BIWTA sources said the situation in the river is almost out of their hand with limited resources and also due to a lack of proper directions. They said they do not have adequate manpower to stop the dumping of rubbish into the river, which takes place all along the flood protection embankment. There are instances when DCC conservancy workers 'signed deals' with river grabbers, and dumped truck loads of household rubbish into the river. Such dumping usually takes place so early in the morning that officials, who should be monitoring, are hardly awake let alone being on the spot.

"I can show you, between Mohammadpur and Postagola more than 50 sites where DCC is dumping rubbish," said a BIWTA official requesting anonymity.

On the slope of the flood protection embankment at Kamrangir Char, dozens of female workers can be regularly found washing and drying huge polythene sheets. They said they buy those sheets from business establishments in Nawabpur and Mitford areas, from garment factories, and from the tokais.

"After buying these dirty sheets we wash and dry them on the embankment and carefully pack them for reselling by weight to buyers, who pay us good prices. Why should we discard them into the river, recycling is our livelihood," said Moina Begum, when asked how so many polythene bags found their way to the riverbed.

Moina's co-worker Hafiza Khatun pointed her finger at a dumping site on the slope of the embankment, and said most of the small polythene in household rubbish piles end up into the river because those cannot be sorted out easily.

On one Friday afternoon, Sadarghat Launch Terminal area was a chaotic crossroad with thousands of passengers, coolies, traders, squatters, and beggars milling around. On the shore between the concrete terminal and the jetty -- human excreta, piles of coconut shells, polythene bags, and an array of rubbish were lying around.

A dozen launches were anchored at the jetty. Vendors selling coconuts, lychees, bombay-mix, puffed rice, bread, and fruits were using the river as a dumping ground.

"The accumulation of polythene and other wastes is so deep and solid that it might not be possible to remove the wastes with a dredger, we might have to do it manually," said an official of BIWTA.

The government banned production, marketing, and use of polythene bags in 2002. An offender under the law may be sentenced to ten years of imprisonment and fined Tk 10 lakh.

Daily Star
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June 1, 2009

Death of a lifeline

Thus die the rivers. Trimohoni, off the river Balu, on the eastern fringe of the capital bears the unbearable testimony of pollution originating mainly from Dhaka Wasa's sewerage system that dumps untreated wastes in the network of canals connected to the river. PHOTO: SK Enamul Haq Inam Ahmed and Morshed Ali Khan

The kingfisher was sitting lonely in the gathering dusk on a dead branch sticking out of tar black water. Our handkerchiefs were proving too inadequate to keep the stench out of our nostrils. With each stroke of the oar, a thick liquid similar to burnt lube oil splashed up. The sound of the oar was blunt and heavy, like hitting mud with a stick.

We were surprised at the kingfisher -- the first sighting of any bird that depends on water for survival. It means there must be fish too in this muck that we still call a river -- Buriganga. Our hope evaporated soon as the kingfisher dived and picked up an insect, looking like the ones you find in your septic tank. When fish is gone, sewage insects are the only feed.

For the last three hours we have been sailing through a river that resembles nothing but pure muck. From Bosila Ghat near the under-construction Third Buriganga Bridge up to as far as you may go towards Munshiganj, the river is just a flowing black sheet of sewage. The stench only increased when the propeller of passing barges whipped up the 'water'. The Buriganga river today is the most stunning monument to an environmental disaster where no vertebrate life form survives. It is a river without fish and water.

One of the main sources of this highly toxic sludge is just on the other side of the river at Hazaribagh of the capital. From there, nearly 250 large leather industries and several hundred small ones have been dumping untreated chemical-mixed water into the river. Every day they pump a staggering 22,000 cubic metres of poison into the Buriganga. According to a World Health Organization (WHO) bulletin, every day these units also dump ten tons of solid waste into the river. Efforts to relocate them to a modern zone in Savar, equipped with effluent treatment plants (ETP), has not worked out in years, as neither the industry owners nor the government want to pay for the relocation cost. Nobody has ever calculated how much these industries contribute to the economy, and how much they destroy.

Polluters vs fishermen
Experts believe Hazaribagh tanneries alone inflict the most severe blow to the air, land, and water in the city. The air within a ten-kilometre radius of the Hazaribagh tanneries is so foul and toxic that thousands of people suffer from various respiratory and skin diseases. Residents in Hazaribagh, Lalbagh, Azimpur, Rayer Bazar, Dhanmondi, and Beri Bandh areas complain of 'corrosion' in their tin roofs and other metal household objects. Housewives even complain of having their ornaments corroded due to the toxicity in the air.

While our industries proudly boast of foreign exchange earnings, no matter how much pollution they are causing by refusing to install ETPs, thousands of traditional fishermen who have been tossed out of the rivers and canals, think if the rivers and canals around the city were clean, they could also bring in a huge amount of foreign currencies, producing and exporting good quality fishes.

Lakhan Rajbangshi from Zaillapara, Basila where a fishermen community of 50 families have lived for over 100 years, said the Buriganga alone could produce enough fish to feed the city population.

"We are spending crores of taka in foreign currencies to import fish from Myanmar, India, and Thailand, but I can assure you, if you return us our river with flow of good quality water we would start exporting river produce within a year," Lakhan, who is now unemployed and miserable, said.

Three days before, we had gone to the Shitalakkhya river near Kanchpur Bridge and saw the unbelievable sight of a swath of 'strawberry shake' tone of purple dye pouring into the river through a drain pipe, frothing and spreading across the river, poisoning everything as it worked through.

At Demra, we again oared through a filthy liquid that is the Shitalakkhya. A small channel that comes parallel to the main river was disgorging effluent at full speed from nearby industries. The refuse then mix with the Shitalakkhya water and ripple down in bubbles poisoning fishes to death, and seeping into the underground aquifer, polluting that as well.

A more horrifying story emerges about the possible contamination of the city's groundwater, as a study jointly done by the World Bank and the Institute of Water Modelling (IWM) warns that the groundwater, on which over 80 percent of the city's population depend, is fast getting contaminated. The contamination mainly occurs at river beds, and at industrial effluent dumping points from where aquifers get recharged. While the Hazaribagh groundwater is classified as the most affected, with time the groundwater pollution is creeping towards other parts of the city too.

Sorry tale of Trimohoni
Residents of Nandigram near the eastern fringe of the city should have been the luckiest people on earth because three rivers -- the Narai, Devdholai, and the Balu -- meet there to form the Trimohoni and pass through the village. Instead local residents consider themselves cursed and doomed. Millions of cubic metres of sewage, and industrial and household wastes generated in the capital's Tejgaon, Dhanmondi, Gulshan, Rajabazar, Maghbazar, Motijheel, Bashabo, and many other densely populated areas fall into the Trimohoni. We, living in plush apartments in the capital, are the source of their misery, as each time we flush our toilets the Trimohoni residents receive it in their rivers through Dhaka Water and Sewerage Authority's (Wasa) outlets at Rampura and Motijheel through Begunbari canal. The Nandigram people are now surrounded by rivers of excreta, where the rivers flow with everything but water.

In Trimohoni area we stood at the doorway of a hut in the smelly village watching a sick child curled up in a bed. Her breaths were shallow. For two days, she had been having a bout of diarrhoea. Her mother had repeatedly warned her not to go near the poisoned river. Still she had taken a dip in the river in a forgetful moment. And now she was in a terrible state.

Pitch black effluents from Tejgaon Industrial Area containing heavy metals such as lead, cadmium, and magnesium are causing serious pollution in Begunbari and Narai canals, leading to pollution of the Balu river. Interestingly, the same river is one of the major sources of water for Saidabad Water Treatment Plant for Dhaka city in the downstream, where it joins the Shitalakkhya. Experts already warned that the river water around the metropolis is so contaminated that it is 'beyond treatment'. Our lack of foresight in planning is well established in the setting up of the water treatment plant at Saidabad before thinking about installing ETPs in our highly polluting industrial units. There is no data to indicate contamination of the supplied water, but frequent outbreaks of waterborne diseases surely suggest an alarming level of contamination in our tap water.

Turag, Buriganga, Shitalakkhya
The Turag river is another bead in the string of the dying rivers that surround the capital. Only a trickle of black liquid represents the river that serves as the lifeline of the southern fringe of the capital. Not only pollution, currently there are more earth filling projects in the Turag than in any other river of the city.

The existence of all these rivers has been pushed to a further edge by a free-for-all encroachment galore. We sailed for miles up and down the four rivers and saw the chilling evidence of how criminals and renowned business enterprises are taking their claims in the rivers at will. And there is no one to stop them; no vigil to identify them.

As we sailed through the Buriganga, we spotted a vast swath of the river fenced off with bamboo poles near Kholamora. Dredgers were moored there that roared sand-filled water inside the fenced area. The river was being filled up, slowly. Already about 500 feet of the river has been turned into land where stands a concrete structure. Another 500 feet or so are in the process of being filled. We stood there and searched for the original river boundary, and finally located the embankment about half a kilometre away that once marked the beginning of the river. That half a kilometre is already gone to meet the appetite of the encroachers. Another half a mile will be gone, in who knows how many months, or days.

A few hundred yards down, we found a few hundred acres of land jutting out into the river in the name of 'Titanic Housing', the same crook is filling up more sections of the river with earth and nobody to stop it. A building is standing right in the middle of the river. Fresh signs of earth-filling of the river are everywhere. It is an awe-striking sight. How effortlessly they are gobbling up the river, making it slimmer and slimmer until nothing will be left.

The same is the case along the Turag and Shitalakkhya. Universities and housing projects have sprung up in the rivers. Sand traders have expanded into the waters, fencing off their own stakes. Industries have found land. It is an unfettered bonanza of river grabbing. You grab it and cook up some documents. Pay tax for the land, which once was part of a river, by some strange manipulation of the system. And it is all yours on the cheap.

Dry canals
The story does not stop here. Just when you think things cannot get any worse, they do. We found canal after canal that either fed into the river systems of Dhaka or fed from them, are choked and dead now. It is mayhem of an unprecedented scale. Even whole river systems have been rendered dry.

Standing on 'a private road' to a brick kiln at Waaspur we witnessed what havoc could be wreaked by a single person. The brick kiln owner built the road chocking the passage for one of the most widely used canals, Atir Khal. As far as the eyes can see, the canal is just a dry gulch. For over 50 years, Atir Khal that winds its way through dozens of important trading centres in Keraniganj and Savar areas, has served millions of farmers and commuters. Today, it could at best be a grazing ground for cattle.

Dhaka by any measure is supposed to be an ideal location for human settlement -- a very few cities have four rivers encircling them. It is supposed to have constant sources of clean surface water supply, a fantastic navigability around the city, which is a source of tourism, and of entertainment for its residents -- all centring the rivers. Because of all these features, the Mughals had chosen it as their capital in Bengal.

But today, the residents of the city have almost forgotten the rivers. In their daily life bound to the traffic packed streets, they do not feel the existence of the Buriganga, Shitalakkhya, Turag, and the Balu. We have let them flow towards extinction.

But the Dhaka residents are already paying for that indifference. Groundwater extraction for supplying household water is dragging down the groundwater table by about 9 feet every year. A big underground void poses the risk that the city might collapse into the pit. It is high time we wake up.

Daily Star
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December 30, 2008

Rare turtles in Cox's Bazar endangered

125 carcases found in one week
Our Correspondent . Cox's Bazar

Existence of different rare species of sea turtles in the Cox's Bazar coast is being endangered due to their unabated killing by wild dogs, jackals and foxes.
Carcases of at least 125 large size sea turtles have been found on the sandy beach of Cox's Bazar in the past one week.
Thirty to thirty-five turtles were found dead in Sonadia island while 90 were found dead along the 90-mile stretch of the sea shore from Cox's Bazar to Teknaf.
Wild dogs, jackals and foxes killed those sea reptiles, witness said.
A good number of turtles are also crushed under the wheels of the travelling jeeps, playing the coastline between Teknaf and Cox's Bazar everyday.
The dogs and foxes also eat up huge eggs of the sea turtles.
The rare turtles are also killed in a large number by the fishermen as they get entangled with their fishing nets.
According to the Upazila Nirbahi Officer, Teknaf, Tofail Islam, and some locals, dogs and foxes killed some 25
large size turtles on Bailakhali sea beach in Teknaf upazila of the district in the past one week.
'It is difficult for the environment department to conserve the endangered species of turtles with its short number of staff,' the UNO added.
Sources said these sea turtles come under attack of the dogs and foxes and are killed as they come ashore to lay eggs at this time of year.
Carcases of some turtles were found on the sandy shore, which were run over by the speedy jeeps.
Abdul Hoque, a crew of a fishing boat of Sonadia under Moheskhali upazila, also informed that at least 32 carcases of large size turtles had been found on Sonadia beach in the past one weak.
Abdul Jalil, an environmentalist, said Lather Bag is a rare species of the turtle family.
They come to the sea shore from Cox's Bazar to Teknaf for breading and are killed by dogs and foxes.
Meanwhile, nine turtle hatcheries have been established on the beaches of Sonadia, Teknaf, Saint Martin Island and Pecherdip of Cox's Bazar by the Environment Department.
Employees of the Environment Department are collecting the turtles' eggs from beaches and tending them.
Locals demand steps for conservation of the sea turtles.

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October 22, 2008

Bay of Bengal 03

South patches located at 91.30ºE to 92.10ºE and 20.55ºS to 21.52ºS, having a total area of 3,662 sq km. Depth ranging from 10m to 100m, but 90% of the total area is less than 40m deep. Bottom sediment is sandy or slightly muddy sand. Nearest distance of the ground from Chittagong and Cox's Bazar is 40 km and 10 km respectively. Salinity in surface water ranges from 26% to 32% and 30% to 35% in bottom water. Water temperature varies between 20 and 28ºC.

South of south patches located at 91.30ºE to 92.20ºE and 20.15ºS 20.50ºS, having an area of 2,538 sq km. The nearest boundary of this area is 5 km from Teknaf. Depth ranges from 10m to 100m. Within this ground 75% of the area is more than 40m deep. Bottom is sandy or muddy sand. Surface salinity ranges from 18% to 34% and bottom water salinity from 28% to 38%. Water temperature ranges between 22ºC and 30ºC.

Middle ground located at 90.20ºE to 91.30ºE and 20.25ºS to 21.20ºS, having a total area of about 4,600 sq km. The nearest distance from Cox's Bazar is about 65 km. The depth of 70% of the total area is more than 40m. Bottom sediment is soft mud or muddy sand. Surface salinity ranges from 22% to 34% and bottom salinity 28% to 35%. Water temperature is between 26ºC and 28ºC.

Swatch of no Ground located at 89.35ºE to 90.10ºE and 20.55ºS to 21.55ºS, about 30 km away from Dublarchar and 40 km from Sunarchar. Total area is about 3,800 sq km, of which 70% is more than 40m deep. Overall depth of the area ranges from 10m to 100m. Bottom sediment consists of muddy sand. Surface salinity is 28% to 34%, while the bottom salinity is 30% to 35%. Water temperature falls within 24ºC to 30ºC.

All these fishing grounds are potential reserves for fish and shrimp. Most of the known commercial species of shrimps and fishes are harvested from these areas by trawlers or mechanized fishing boats. Commercially important shrimp and fish species include tiger shrimp, karuma shrimp, cat fish, Bombay duck, snapper, flounder, Indian salmon, crocker, seabream, jawfish, mullet, pomfret, ribbon fish, anchovy, hilsa, oil sardine, tuna, mackerel and skipjack. [Hossain Zamal]

Pollution marine environment of Bangladesh is directly or indirectly becoming polluted due to addition of so many polluting agents. To protect water pollution and control of mine drainage, large scale drilling and production of natural gas from the Sangu offshore gasfield, discovery of Kutubdia offshore gasfield and exploration of beach sand placer deposits from the offshore islands of Chittagong and Cox's Bazar districts must follow standard regulations both from mine safety and environmental protection point of view. Sangu gasfield is located about 50 km southwest of Chittagong City and stands at a depth of 10m water in the Bay of Bengal. Kutubdia gasfield is about 92 km southwest of chittagong port.

The coastal environment of Bangladesh is contaminated by oil tanker traffic, harbour operations and effluents discharged from petroleum processing. sewage disposal by the karnafuli and pasur rivers into the Bay of Bengal contains higher concentration of Biochemical Oxygen Demand (BOD) and foecal coliform. Moreover, the coastal environment of Bangladesh has also been affected by industrial effluents, agricultural residues, some other human activities like deforestation and irrational expansion of coastal shrimp farming, etc resulting in ecological degradation. Overfishing and dumping of discarded fishes in these areas are becoming a threat to the resourcefulness of the fishing grounds. Only proper management of the existing grounds and finding of new fishing grounds can ensure the continuous harvest of fisheries resources. [Sifatul Quader Chowdhury]
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October 21, 2008

Bay of Bengal 02

Geographical characteristics Hydrological conditions surface hydrology of the Bay of Bengal is basically determined by the monsoon winds and to some extent by the hydrological characteristics of the open part of the Indian Ocean. Fresh water from the rivers largely influences the coastal northern part of the Bay. The rivers of Bangladesh discharge the vast amount of 1,222 million cubic metres of fresh water (excluding evaporation, deep percolation losses and evapotranspiration) into the Bay. The temperature, salinity and density of the water of the southern part of the Bay of Bengal is, almost the same as in the open part of the ocean. In the coastal region of the Bay and in the northeastern part of the Andaman Sea where a significant influence of river water is present, the temperature and salinity are seen to be different from the open part of the Bay. The waves and ripples entering from the southern part of the Bay provide the energy for mixing the water and consequently bring uniformity in its chemical and physical properties. Tidal action is also very great in the shallow coastal zones.

Temperature the mean annual temperature of the surface water is about 28°C. The maximum temperature is observed in May (30°C) and the minimum (25°C) in January-February. But the annual variation in temperature is not great, about 2°C in the south and 5°C in the north.

Salinity the surface salinity in the open part of the Bay oscillates from 32% to 34.5% (parts per thousand, ie grams per kilogram of sea water) and in the coastal region varies from 10% to 25%. But at the river mouths, the surface salinity decreases to 5% or even less. The coastal water is significantly diluted throughout the year, although the river water is greatly reduced during winter. Along the coast of the Ganges-Brahmaputra Delta, salinity decreases to 1% during summer and increases up to 15% to 20% in winter. Salinity gradually increases from the coast towards the open part of the Bay. The surface salinity at the mouths of some large rivers like the ganges, brahmaputra, Irrawaddy and some Indian rivers like the Krishna, Godavari, Cauvery and Mahanadi varies widely from one day to another, especially in summer. Salinity of water also changes vertically. The influence of the fresh water is experienced up to depths of 200-300m. From the surface, the salinity gradually increases downward and at about 200-300m it reaches 35% and at about 500m the salinity is more than 35.10%, but at 1,000m it decreases slightly and attains 34.95%. With further increase of depth salinity decreases and at 4,500m it is close to 34.7%.

Tides the semi-diurnal type of tides, ie two high and two low tides during the period of 24 hours and 52 minutes. The highest tide is seen where the influence of bottom relief and the configuration of the coast are prominent, ie in shallow water and in the Bay and estuary. The average height of tidal waves at the coast of Sri Lanka is 0.7m and in the deltaic coast of the Ganges it is 4.71m. In the Bay of Bengal tidal currents specially develop in the mouths of the rivers, like the Hooghly and the meghna.

Colour and water transparency the colour of the water in the open part of the Bay is dark blue which gradually changes to light blue to greenish towards the coast. Transparency is great, 40-50m in some places. In the central part of the Bay of Bengal, the anticyclone circulation is generated and in the centre of this lies the zone of convergence. This region is characterised as a rule by high transparency of water. Regions of low transparency and turbid water are available in the limited area of the pre-deltaic part of the rivers Ganges and Brahmaputra.

Sea Level due to the influence of water density and wind the seasonal changes of the sea level in the Bay are remarkable and one of the highest in the world. The range at Khidirpur is 166 cm, at Kolkata 130 cm and at Chittagong 118 cm. But towards the southwestern coast at Madras and Vishakhapatnam [Vishakhapatnam] the range is small compared to the northern and northeastern coasts of the Bay. The lowest variation of sea level at the southeastern coast of India is due to its geographical location at the edge of a comparatively deep sea.

Ocean Current surface circulation is found to be generally clockwise from January to July and counter-clockwise from August to December, in accordance with the reversible monsoon wind systems. The flow is not constant and depends on the strength and duration of the winds. The effects of a strong wind blowing for a few consecutive days are reflected in the rate of flow. Currents to the northeast generally persist longer and flow at greater speed because of the stronger southwest monsoons. An important vertical circulation in the Bay of Bengal is up-welling. In this process, sub-surface water is brought toward the surface, and conversely a downward displacement is called down-welling or sinking.

Up-welling and down-welling are seasonal, being created by monsoon winds that blow from the southwest during the summer, then reverse direction and come from the northeast during the winter. The persistence of the monsoon, especially from the southwest and the orientation of the coasts cause up-welling to occur along most of the east coast of India. That is why in the east coast of India the up-welling takes place in summer and down welling in winter, and in the eastern part of the Bay of Bengal and in the Myanmar coast, up-welling occurs in winter and the down-welling in summer. However, the duration and intensity of vertical movement of water on both sides of the Bay of Bengal is not as great as on the Somali or North and South American coasts. But it does have a profound effect on the food economy of the sea through its influence on chemical properties and biological populations. [Subash Chandra Das]

Biological characteristics the occurrence of marine species - both plants and animals - has largely been controlled by the physico-chemical properties of ocean water. Water discharges from the surrounding river catchments carry huge influx of sediments full of nutrients to the Bay, particularly along the near shore region. This has turned the Bay into a fertile marine fishing ground of the region. The near-shore up-welling zone not only has a high yield of nutrients, but also is a high primary production area for the phytoplankton and related zooplankton zones.

Fishing the hydrological conditions of the Bay of Bengal is favourable for a variety of shrimps and fishes. Although fishes remain scattered in the Bay in some places they get concentrated and constitute important fishing grounds. Four fishing grounds have been identified so far. They are south patches, south of south patches, middle ground and Swatch of no Ground.

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October 20, 2008

Bay of Bengal 01

Bay of Bengal a northern extended arm of the indian ocean, is located between latitudes 5°N and 22°N and longitudes 80°E and 100°E. It is bounded in the west by the east coasts of Sri Lanka and India, on the north by the deltaic region of the Ganges-Brahmaputra-Meghna river system, and on the east by the Myanmar peninsula extended up to the Andaman-Nicobar ridges. The southern boundary of the Bay is approximately along the line drawn from Dondra Head in the south of Sri Lanka to the north tip of Sumatra. The Bay occupies an area of about 2.2 million sq km and the average depth is 2,600m with a maximum depth of 5,258m. Bangladesh is situated at the head of the Bay of Bengal.

Bottom topography characterised by a broad U-shaped basin with its south opening to the Indian Ocean. A thick uniform abyssal plain occupies almost the entire Bay of Bengal gently sloping southward at an angle of 8°-10°. In many places underwater valleys dissect this plain mass.

Continental Shelf the width of the continental shelf off the coast of Bangladesh varies considerably. It is less than 100 km off the south coast between Hiron Point and the swatch of no ground and more than 250 km off the coast of cox's bazar. sediments are fine seaward and westward with the thickest accumulation of mud near the submarine canyon, the Swatch of no Ground. The shallow part (less than 20m) of the continental shelf off the coast of chittagong and teknaf is covered by sand and the intertidal areas show well-developed sandy beaches. The shallower part of southern continental shelf off the coast of the sundarbans, patuakhali and noakhali is covered by silt and clay; and extensive muddy tidal flats are developed along the shoreline. Some of the shoals and sand ridges present on this part of the continental shelf show an elongation pattern pointed towards the Swatch of no Ground.

Swatch of no Ground also known as Ganga Trough. Swatch of no Ground has a comparatively flat floor 5 to 7 km wide and walls of about 12° inclination. At the edge of the shelf, depths in the trough are about 1,200m. The Swatch of no Ground has a seaward continuation for almost 2,000 km down the Bay of Bengal in the form of fan valleys with levees. The sandbars and ridges near the mouth of the ganges-brahmaputra delta pointing toward the Swatch of no Ground showing sediments are tunnelled through this trough into the deeper part of the Bay of Bengal. The Swatch of no Ground is feeding the Bengal Deep Sea Fan by turbidity currents.

Sunda Trench also known as Java Trench. Running parallel along the west side of the arc of the Nicobar and Andaman islands it is extended northward up to 10°N into the Bay and joins the eastern limit of the Himalayan range. It originated tectonically at the junction of the Indian and Myanmar plates.

Ninety East Ridge major feature of the Indian Ocean which runs in a north-south direction approximately along the longitude 90°E. It lies at the immediate outboard of the Sunda Trench between the Bengal Fan and the Nicobar Fan. The Ninety East Ridge has existed since early in the formation of the Bay of Bengal. The ridge represents the trace of a hot spot formed during the northward flight of India and its associated oceanic lithosphere of the Bay of Bengal.

Eighty-five Ridge a ridge along 85°E longitude. More than 5 km thick sediments have been deposited on either sides of the ridge. The main turbidity current channel of the subaerial drainage pattern lies immediately east of the buried ridge.

Bengal Deep Sea Fan the world's largest submarine fan, also known as Bengal Fan. Together with its eastern lobe, the Nicobar fan, it covers an area of 3106 sq km. It is 2,800 to 3,000 km long, 830 to 1,430 km wide and more than 16 km thick beneath the northern Bay of Bengal. Sediments are tunnelled to the fan via a delta-front trough, the Swatch of no Ground. It can be divided into three parts: upper fan, middle fan and lower fan. Rapid terrigenous sedimentation on an incipient Bengal fan began in the Eocene age (58 to 37 million years ago) as a response to the first intraplate collision and continued to the present, building the world's largest submarine fan. [Mahmood Alam]

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October 18, 2008

বাংলাদেশে যত ডলফিন

বাংলাদেশ হলো বিভিন্ন প্রজাতির বিপুলসংখ্যক জলজ স্তন্যপায়ীর অবাধ বিচরণক্ষেত্র। এশিয়ার অন্যান্য দেশ, যারা বাংলাদেশের প্রতিবেশী, তাদের তুলনায় বাংলাদেশের নদী ও উপকুলীয় এলাকায় বিভিন্ন প্রজাতির জলজ স্তন্যপায়ী অনেক বেশি দেখা যায়। বাংলাদেশের ম্যানগ্রোভ বনাঞ্চল, উপকুলীয় ও গভীর সমুদ্রের জলভাগ অসাধারণ সব প্রজাতির জলজ স্তন্যপায়ীর জন্য খুবই উপযোগী বাসস্থান।

বাংলাদেশের সবচেয়ে বেশি পরিচিত ডলফিন হলো শুশুক। এরা সত্যিকারের নদীর ডলফিন। বিশেষ আকৃতির লম্বা ঠোঁট, পিঠের ছোট ডানা আর দুই পাশের বড় পাখনার কারণে শুশুক দেখতে একটু অদ্ভুত। পদ্মা, মেঘনা, যমুনা নদীর সব জায়গাতেই শুশুকের বাস। সত্যিকারের নদীর ডলফিন সাগরের ডলফিনের দুরসম্পর্কের আত্মীয়। এদের ঠোঁট লম্বা এবং চোখ খুব ছোট। শুশুকের দৃষ্টিশক্তি খুবই দুর্বল। নদীর যে ঘোলা পানিতে এদের বসবাস, সেখানে দৃষ্টিশক্তির খুব একটা প্রয়োজন হয় না। এর বদলে এদের ইকোলোকেশনের শক্তি অনেক প্রখর। চলাচলের সময় জলজ স্তন্যপায়ীরা প্রতিধ্বনিত শব্দ দিয়ে মস্তিষ্কেক প্রতিচ্ছবি তৈরি করে।

শুশুকের শরীরের দুই পাশের বড় পাখনা ও নমনীয় ঘাড়ের জন্য এরা সহজে চলাচল করতে পারে। অনেক সময় দেখা যায়, এরা কাত হয়ে সাঁতার কাটে। বড় পাখনার সাহায্যে এরা নদীর তলদেশ ছুঁয়ে পথ নির্ধারণ করে। এরা কিন্তু মোটেই সমাজবদ্ধ নয়। সাধারণত একাই থাকে। তবে অনেক সময় নদীর বাঁকে ও মোহনায় ছোট ছোট দলে দেখা যায়।

কিছু প্রজাতির ডলফিন নদী ও সাগর উভয় স্থানেই দেখা যায়। যেমন ইরাবতী ডলফিন। আমাদের দেশে এরা সুন্দরবনের মিঠা পানির নদী আর বঙ্গোপসাগরের উপকুলীয় অঞ্চলে বাস করে। নদীসহ যেসব উপকুলীয় জলাশয়ে নদী থেকে মিঠা পানি আসে, সেসব স্থানে ইরাবতী ডলফিন দেখা যায়। সুন্দরবন ম্যানগ্রোভ বনাঞ্চলের জলপথে এরা শুশুকের সঙ্গে মিলেমিশেই থাকে।

গোলাপি ডলফিন বা ফিনলেস পরপয়েসকে মাঝেমধ্যে সুন্দরবনের নদীতে দেখা গেলেও এরা আসলে উপকুলীয় জলভাগে বাস করে, যেখানে পদ্মা, মেঘনা, যমুনা নদী থেকে মিঠা পানি আসে।

প্রথম আলো, ১৭, অক্টোবর, ২০০৮
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October 17, 2008

ডলফিনের জন্য ভালোবাসা

একসময় বাংলাদেশের খুব কম নদনদীই ছিল যেখানে শুশুক দেখা যেত না। প্রতিকুল পরিবেশ, মানুষের বৈরিতায় আস্তে আস্তে বড় কিছু নদী ছাড়া আর সব জলাশয় থেকেই প্রায় হারিয়ে গেছে ডলফিনের এ প্রজাতি। তার পরও সাম্প্রতিক কিছু জরিপ বলছে, এখনো আশপাশের দেশের তুলনায় আমাদের দেশে ডলফিনের সংখ্যা নেহাত কম নয়। বাংলাদেশে ডলফিনের অবস্থা নিয়ে আমাদের এই প্রতিবেদন।

ফারহানা আলম

ডলফিন নিয়ে আলাদা করে কোনো আগ্রহ রুবাইয়াত মনসুর মুগলির ছিল না। তাঁকে আগ্রহী করে তোলেন ওয়াইল্ড লাইফ কনজারভেশন সোসাইটির প্রকল্প পরিচালক ব্রায়ান স্মিথ। ২০০০ সালে বাংলাদেশে এসেছিলেন ভদ্রলোক। বেসরকারি পর্যটন সংস্থা দ্য গাইড ট্যুরস লিমিটেডের ভ্রমণতরীতে করে সুন্দরবন গিয়েছিলেন তিনি। সুন্দরবন যাওয়ার পথে নদীতে শুশুকসহ অনেক ডলফিন দেখলেন ব্রায়ান। ওই অঞ্চলের নদীর পানিতে জলজ স্তন্যপায়ী গোত্রের প্রাণী দেখে গাইড ট্যুরসের মুগলিকে গল্প শোনাতে লাগলেন তিনি। সেই প্রথম মুগলি জানলেন, বাংলাদেশের নদনদী ও বঙ্গোপসাগরে নানা জাতের ডলফিন আছে। গভীর সমুদ্রে আরও আছে ডলফিনেরই জাতভাই তিমি। ব্যস, আর যায় কোথায়! এই বিষয়ে খোঁজ-খবর নিতে শুরু করলেন রুবাইয়াত মুগলি। আর তাঁকে বিভিন্ন সময় সহযোগিতা করার জন্য ব্রায়ান স্মিথ তো ছিলেনই।

২০০২ সালের ফেব্রুয়ারিতে ওয়াইল্ড লাইফ কনজারভেশন সোসাইটির জন্য বাংলাদেশ পররাষ্ট্র মন্ত্রণালয়, তিমি ও ডলফিন সংরক্ষণ সংস্থা এবং কনভেনশন অন মাইগ্রেটরি স্পিসিজের সমর্থনে মূলত ব্রায়ান স্মিথের আয়োজনে প্রথমবারের মতো শুরু হয় রুবাইয়াতের ডলফিন নিয়ে জরিপের কাজ। জরিপে অংশ নেন ভারত, বাংলাদেশ, যুক্তরাজ্য, যুক্তরাষ্ট্রের বিজ্ঞানীরা। জরিপের জন্য তাঁরা ঘুরে বেড়িয়েছেন সুন্দরবনের সব নদী ও খাল। আইইউসিএনের সঙ্গে যৌথভাবে আবার সুন্দরবনের জলপথ ধরে চলে গবেষণা। বাংলাদেশের জলসীমায় থাকা স্তন্যপায়ী প্রাণিবৈচিত্র্যের সন্ধান করা এবং সেগুলো যেন বিলুপ্ত হয়ে না যায় সে লক্ষ্যে কী কী পদক্ষেপ নেওয়া উচিত, তার অনুসন্ধানই ছিল রুবাইয়াতের মূল লক্ষ্য।

২০০৪ সালে বাংলাদেশের উপকুল ধরে মিয়ানমারের সীমানা থেকে অর্থাৎ নারিকেল জিঞ্জিরার উপকুল থেকে সুন্দরবনের বাংলাদেশ অংশের শেষ সীমা পর্যন্ত চালানো হয় আরেকটি জরিপ। এই জরিপেও বাংলাদেশ, ভারত, মিয়ানমার, শ্রীলঙ্কার ১৫ জন বিজ্ঞানী অংশ নেন। তখনই তাঁরা এই অঞ্চলে সামুদ্রিক ডলফিন ও তিমির দেখা পান। সেই সঙ্গে সুন্দরবনের গভীর সমুদ্রের গিরিখাদ বা অতলস্পর্শে ডলফিনের বৈচিত্র্য ও এদের অবাধ বিচরণ দেখেন।

২০০৫ সালে আবার এ জায়গায় জরিপের সময় তাঁরা প্যানট্রপিক্যাল স্পটেড ডলফিন ও স্পিনার ডলফিনের অস্তিত্ব খুঁজে পান।
বিভিন্ন সময় বিভিন্ন জরিপ চলতে থাকলেও কোনো আনুষ্ঠানিক ভিত্তি না থাকায় রুবাইয়াত ২০০৬ সালের জুলাই মাসে এসে গঠন করেন বাংলাদেশ সেটেশন ডাইভার্সিটি প্রজেক্ট (বিসিডিপি)। রুবাইয়াতও পুরোদমে প্রধান গবেষক হিসেবে কাজ শুরু করেন।
ছয় বছরের জরিপের ফলাফলে মোটামুটি একটা সংখ্যা বের হয়ে এসেছে। গাইড ট্যুরসের ভ্রমণতরী এমভি অবসর, এমভি ছুটি ও এমভি বনবিবির সারেংরাও এই জরিপে অংশ নেন। তাঁরা দল, একক ও বাচ্চা−এই তিনটি ভাগে জরিপটি পরিচালনা করেন। সেই হিসাবমতো শুশুকের এক হাজার পাঁচটি দল, একক এক হাজার ৯৯৩টি এবং বাচ্চা ২৩৫টি গণনা করা হয়। আর ইরাবতী ডলফিনের ২৮১টি দল, একক ৫৬৬টি এবং বাচ্চা ৩২টি দেখা গেছে। এই জরিপ করা হয়েছে সুন্দরবনের সংরক্ষিত ম্যানগ্রোভ বনাঞ্চলের ২৬ হাজার কিলোমিটার এলাকাজুড়ে।

সামগ্রিক জরিপে বাংলাদেশের জলসীমায় প্রায় ছয় হাজার ইরাবতী ডলফিনের অস্তিত্ব সম্পর্কে নিশ্চিত হওয়া গেছে। কিন্তু শুধু অস্তিত্ব থাকলেই হবে না; তাদের অস্তিত্ব যেন বিলুপ্তির দিকে না যায় সেই লক্ষ্যেই কাজ করতে হবে। তাই বিসিডিপি কিছু লক্ষ্য নির্ধারণ করেছে। জনসচেতনতা তৈরি করতে তারা মানুষের কাছে পৌঁছে দিচ্ছে নানা ধরনের বইপত্র, যেখানে ডলফিন ও তিমিবিষয়ক নানা তথ্য দেওয়া আছে। আবার সামাজিকভাবে সংঘবদ্ধ করে আলোচনার ব্যবস্থা করা হচ্ছে। স্থানীয় নেতা এবং স্কুল-কলেজের শিক্ষকেরাও এই সচেতনতা সৃষ্টির লক্ষ্যে কাজ করছেন। খেলাধুলা ও ছবির মাধ্যমেও প্রাণিবৈচিত্র্য সংরক্ষণের বিষয়টি নিয়ে আলোচনা হচ্ছে। সেই সঙ্গে একটি তথ্যচিত্র জাতীয় গণমাধ্যমে বা স্থানীয়ভাবে দেখানোর ব্যবস্থা করা হবে। জলজ স্তন্যপায়ী আর নিজেদের নিরাপত্তার জন্য জেলেরা যাতে নিরাপদ জলপথ ব্যবহার করতে পারে সেই লক্ষ্যে কম খরচে ও সহজবোধ্য গ্লোবাল পজিশনিং সিস্টেমের ব্যবস্থা করার পরিকল্পনাও আছে। আছে আশপাশের এলাকার গ্রামবাসী ও জেলেদের জলজ স্তন্যপায়ীর বিচরণক্ষেত্র, জীবনাচরণ পর্যালোচনা, প্রশিক্ষণ দেওয়া এবং সচেতনতা বাড়ানোর পরিকল্পনা। সমুদ্রপৃষ্ঠের উচ্চতা বৃদ্ধি, জলবায়ুর পরিবর্তন, বাঁধের কারণে সুন্দরবন ও মোহনায় নদীর পানির স্বল্পতার মধ্যেও জলজ স্তন্যপায়ীর জীবনধারণ লক্ষ করে এদের বৈচিত্র্য সংরক্ষণ করা।

জলজ স্তন্যপায়ীদের জন্য একটি সংরক্ষিত এলাকা নির্ধারণের প্রস্তাব করেছে বিসিডিপি। দক্ষিণে বঙ্গোপসাগর আর উত্তরে মংলা বন্দর, পূর্বে বলেশ্বর আর পশ্চিমে পশুর নদকে সীমা ধরে মাঝখানে পূর্ব সুন্দরবনের নির্ধারিত অংশকে এই সংরক্ষিত এলাকা হিসেবে চিহ্নিত করা হয়েছে। এখানে সংরক্ষিত এলাকায় চিংড়ি মাছের পোনা ধরায় সুক্ষ্মজালের ব্যবহার বন্ধ ও পানিদুষণ রোধ করা গেলেই জলজ স্তন্যপায়ী প্রাণীরা অবাধে বিচরণ করতে পারবে।

জলজ স্তন্যপায়ীর অবাধ বিচরণ ও বৈচিত্র্য বৃদ্ধির লক্ষ্যেই বিসিডিপি ৯ থেকে ১২ অক্টোবর শিশু একাডেমীতে আয়োজন করে বাংলাদেশে প্রথম শুশুক মেলা। চার দিনব্যাপী এই মেলায় বিপুলসংখ্যক দর্শক উপস্থিতি প্রমাণ করে জলজ স্তন্যপায়ী প্রাণিবৈচিত্র্যের প্রতি মানুষের আগ্রহ আছে। বললেন বিসিডিপির শিক্ষা ও প্রশিক্ষণ সমন্বয়কারী এলিজাবেথ ফাহরনি মনসুর।

প্রথম আলো, ১৭, অক্টোবর, ২০০৮
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October 2, 2008

Swatch of no Ground

Swatch of no Ground a trough-shaped marine valley or canyon that cross the continental shelf diagonally and situated on the south of the Ganges-Brahmaputra delta. It is also known as Ganga Trough. Similar delta-front troughs are found off the mouth of the Indus River known as Indus Trough and off the West Side of the Mississipi delta, the Mississipi Trough. Swatch of no Ground has a comparatively flat floor 5 to 7 km wide and walls of about 12° inclination. At the edge of the shelf, depths in the trough are about 1,200m. It has been suggested that the Swatch of no Ground has a seaward continuation for almost 2,000 km down the bay of bengal in the form of fan valleys with levees. The sandbars and ridges near the mouth of the Ganga-Brahmaputra delta pointing toward the Swatch of no Ground indicate that sediments are tunnelled through this trough into the deeper part of the Bay of Bengal. Slumps, growth faults and evidence of mass movement coupled with high sedimentation rates near the Swatch of no Ground provide dramatic evidence that modern sediment is being channelled off-shelf through the submarine canyon to the Bengal Fan. Studies on the bengal deep sea fan suggest that Swatch of no Ground is feeding the Bengal Fan by turbidity currents. Most of the sediment of the Bengal Deep Sea Fan has been derived from the confluent of ganges and brahmaputra rivers, which drain the south and north slopes of the Himalayan, respectively. Under the present condition perhaps low-density turbidity currents and sand cascading are perhaps dominating process of sediment transport from the shelf to the deep sea through the Swatch of no Ground.

There is some controversy regarding the origin of Swatch of no Ground. However, it is generally believed that during the Pleistocene (2-0.1million years ago) lower sea level, Ganga-Brahmaputra River was discharging its sediment load directly on the shelf edge. Combination effect of river flow and turbidity currents generated at the shelf break and upper slope was responsible for the formation of the Swatch of no Ground. Evidence from the Bengal Deep-Sea Fan also tends to support this view. It has been observed that turbidity currents during the Pleistocene lower sea level dominated sedimentation on the Bengal Deep-Sea Fan and the sediments were distributed on the fan by a system submarine channel originating from the Swatch of no Ground. [Mahmood Alam]
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August 29, 2008

Global Warming: The Fate of Bangladesh

Bangladesh is set to disappear under the waves by the end of the century - A special report by Johann Hari

Bangladesh, the most crowded nation on earth, is set to disappear under the waves by the end of this century – and we will be to blame. Johann Hari took a journey to see for himself how western profligacy and indifference have sealed the fate of 150 million people went to see for himself the spreading misery and destruction as the ocean reclaims the land on which so many millions depend

Alamy

Battling the waves: many Bangladeshis depend on the ocean

This spring, I took a month-long road trip across a country that we – you, me and everyone we know – are killing. One day, not long into my journey, I travelled over tiny ridges and groaning bridges on the back of a motorbike to reach the remote village of Munshigonj. The surviving villagers – gaunt, creased people – were sitting by a stagnant pond. They told me, slowly, what we have done to them.

Ten years ago, the village began to die. First, many of the trees turned a strange brownish-yellow colour and rotted. Then the rice paddies stopped growing and festered in the water. Then the fish floated to the surface of the rivers, gasping. Then many of the animals began to die. Then many of the children began to die.

The waters flowing through Munshigonj – which had once been sweet and clear and teeming with life – had turned salty and dead.

Arita Rani, a 25-year-old, sat looking at the salt water, swaddled in a blue sari and her grief. "We couldn't drink the water from the river, because it was suddenly full of salt and made us sick," she said. "So I had to give my children water from this pond. I knew it was a bad idea. People wash in this pond. It's dirty. So we all got dysentery." She keeps staring at its surface. "I have had it for 10 years now. You feel weak all the time, and you have terrible stomach pains. You need to run to the toilet 10 times a day. My boy Shupria was seven and he had this for his whole life. He was so weak, and kept getting coughs and fevers. And then one morning..."

Her mother interrupted the trailing silence. "He died," she said. Now Arita's surviving three-year-old, Ashik, is sick, too. He is sprawled on his back on the floor. He keeps collapsing; his eyes are watery and distant. His distended stomach feels like a balloon pumped full of water. "Why did this happen?" Arita asked.

It is happening because of us. Every flight, every hamburger, every coal power plant, ends here, with this. Bangladesh is a flat, low-lying land made of silt, squeezed in between the melting mountains of the Himalayas and the rising seas of the Bay of Bengal. As the world warms, the sea is swelling – and wiping Bangladesh off the map.

Deep below the ground of Munshigonj and thousands of villages like it, salt water is swelling up. It is this process – called "saline inundation" – that killed their trees and their fields and contaminated their drinking water. Some farmers have shifted from growing rice to farming shrimp – but that employs less than a quarter of the people, and it makes them dependent on a fickle export market. The scientific evidence shows that unless we change now, this salt water will keep rising and rising, until everything here is ocean.

I decided to embark on this trip when, sitting in my air-conditioned flat in London, I noticed a strange and seemingly impossible detail in a scientific report. The International Panel on Climate Change (IPCC) – whose predictions have consistently turned out to be underestimates – said that Bangladesh is on course to lose 17 per cent of its land and 30 per cent of its food production by 2050. For America, this would be equivalent to California and New York State drowning, and the entire mid-West turning salty and barren.

Surely this couldn't be right? How could more than 20 million Bangladeshis be turned into refugees so suddenly and so silently? I dug deeper, hoping it would be disproved – and found that many climatologists think the IPCC is way too optimistic about Bangladesh. I turned to Professor James Hansen, the director of Nasa's Goddard Institute for Space Studies, whose climate calculations have proved to be more accurate than anybody else's. He believes the melting of the Greenland ice cap being picked up by his satellites today, now, suggests we are facing a 25-metre rise in sea levels this century – which would drown Bangladesh entirely. When I heard this, I knew I had to go, and see.

1. The edge of a cliff

The first thing that happens when you arrive in Dhaka is that you stop. And wait. And wait. And all you see around you are cars, and all you hear is screaming. Bangladesh's capital is in permanent shrieking gridlock, with miles of rickshaws and mobile heaps of rust. The traffic advances by inches and by howling. Each driver screams himself hoarse announc-ing – that was my lane! Stay there! Stop moving! Go back! Go forward! It is a good-natured shrieking: everybody knows that this is what you do in Dhaka. If you are lucky, you enter a slipstream of traffic that moves for a minute – until the jams back up and the screaming begins once more.

Around you, this megalopolis of 20 million people seems to be screaming itself conscious. People burn rubbish by the roadside, or loll in the rivers. Children with skin deformities that look like infected burns try to thrust maps or sweets into your hand. Rickshaw drivers with thighs of steel pedal furious-ly as whole families cling on and offer their own high-volume traffic commentary to the groaning driver, and the groaning city.

I wanted to wade through all this chaos to find Bangladesh's climate scientists, who are toiling in the crannies of the city to figure out what – if anything – can be saved.

Dr Atiq Rahman's office in downtown Dhaka is a nest of scientific reports and books that, at every question, he dives into to reel off figures. He is a tidy, grey-moustached man who speaks English very fast, as if he is running out of time.

"It is clear from all the data we are gathering here in Bangladesh that the IPCC predictions were much too conservative," he said. He should know: he is one of the IPCC's leading members, and the UN has given him an award for his unusually prescient predictions. His work is used as one of the standard textbooks across the world, including at Oxford and Harvard. "We are facing a catastrophe in this country. We are talking about an absolutely massive displacement of human beings."

He handed me shafts of scientific studies as he explained: "This is the ground zero of global warming." He listed the effects. The seas are rising, so land is being claimed from the outside. (The largest island in the country, Bhola, has lost half its land in the past decade.) The rivers are super-charged, becoming wider and wider, so land is being claimed from within. (Erosion is up by 40 per cent). Cyclones are becoming more intense and more violent (2007 was the worst year on record for intense hurricanes here). And salt water is rendering the land barren. (The rate of saline inundation has trebled in the past 20 years.) "There is no question," Dr Rahman said, "that this is being caused primarily by human action. This is way outside natural variation. If you really want people in the West to understand the effect they are having here, it's simple. From now on, we need to have a system where for every 10,000 tons of carbon you emit, you have to take a Bangladeshi family to live with you. It is your responsibility." In the past, he has called it "climatic genocide".

The worst-case scenario, Dr Rahman said, is if one of the world's land-based ice-sheets breaks up. "Then we lose 70 to 80 per cent of our land, including Dhaka. It's a different world, and we're not on it. The evidence from Jim Hansen shows this is becoming more likely – and it can happen quickly and irreversibly. My best understanding of the evidence is that this will probably happen towards the end of the lifetime of babies born today."

I walked out in the ceaseless churning noise of Dhaka. Everywhere I looked, people were building and making and living: my eyes skimmed up higher and higher and find more and more activity. A team of workers were building a house; behind and above them, children were sewing mattresses on a roof; behind and above them, more men were building taller buildings. This is the most cramped country on earth: 150 million people living in an area the size of Iowa. Could all this life really be continuing on the crumbling edge of a cliff?

2. 'It is like the Bay is angry'

I was hurtling through the darkness at 120mph with my new driver, Shambrat. He was red-eyed from chewing pan, a leaf-stimulant that makes you buzz, and I could see nothing except the tiny pools of light cast by the car. They showed we were on narrow roads, darting between rice paddies and emptied shack-towns, in the midnight silence. I kept trying to put on my seatbelt, but every time Shambrat would cry, "You no need seatbelt! I good driver!" and burst into hysterical giggles.

To see if the seas were really rising, I had circled a random low-lying island on the map called Moheshkhali and asked Shambrat to get me there. It turned out the only route was to go to Coxs Bazar – Bangladesh's Blackpool – and then take a small wooden rowing boat that has a huge chugging engine attached to the front. I clambered in alongside three old men, a small herd of goats, and some chickens. The boat was operated by a 10-year-old child, whose job is to point the boat in the right direction, start the engine, and then begin using a small jug to frantically scoop out the water that starts to leak in. After an hour of the deafening ack-ack of the engine, we arrived at the muddy coast of Moheshkhali.

There was a makeshift wooden pier, where men were waiting with large sacks of salt. As we climbed up on to the fragile boards, people helped the old men lift up the animals. There were men mooching around the pier, waiting for a delivery. They looked bemused by my arrival. I asked them if the sea levels were rising here. Rezaul Karim Chowdry, a 34-year-old who looked like he is in his fifties, said plainly: "Of course. In the past 30 years, two-thirds of this island has gone under the water. I had to abandon my house. The land has gone into the sea." Immediately all the other men start to recount their stories. They have lost their houses, their land, and family members to the advance.

They agreed to show me their vanishing island. We clambered into a tuc-tuc – a motorbike with a carriage on the back – and set off across the island, riding along narrow ridges between cordoned-off areas of sand and salt. The men explained that this is salt-farming: the salt left behind by the tide is gathered and sold. "It is one of the last forms of farming that we can still do here," Rezaul said. As we passed through the forest, he told me to be careful: "Since we started to lose all our land, gangs are fighting for the territory that is left. They are very violent. A woman was shot in the crossfire yesterday. They will not like an outsider appearing from nowhere."

We pulled up outside a vast concrete structure on stilts. This, the men explained, is the cyclone shelter built by the Japanese years ago. We climbed to the top, and looked out towards the ocean. "Do you see the top of a tree, sticking out there?" Rezaul said, pointing into the far distance. I couldn't see anything, but then, eventually, I spotted a tiny jutting brown-green tip. "That is where my house was." When did you leave it? "In 2002. The ocean is coming very fast now. We think all this" – he waved his hand back over the island – "will be gone in 15 years."

Outside the rusty house next door, an ancient-looking man with a long grey beard was sitting cross-legged. I approached him, and he rose slowly. His name was Abdul Zabar; he didn't know his age, but guessed he is 80. "I was born here," he said. "There" – and he points out to the sea. "The island began to be swallowed in the 1960s, and it started going really quickly in 1991. I have lost my land, so I can't grow anything... I only live because one of my sons got a job in Saudi Arabia and sends money back to us. I am very frightened, but what can I do? I can only trust in God." The sea stops just in front of his home. What will you do, I asked, if it comes closer? "We will have nowhere to go to."

I was taken to the island's dam. It is a long stretch of hardened clay and concrete and mud. "This used to be enough," a man called Abul Kashin said, "but then the sea got so high that it came over the dam." They have tried to pile lumps of concrete on top, but they are simply washed away. "My family have left the island," he continued, "They were so sad to go. This is my homeland. If we had to leave here to go to some other place, it would be the worst day of my life."

Twenty years ago, there were 30,000 people on this island. There are 18,000 now – and most think they will be the last inhabitants.

On the beach, there were large wooden fishing boats lying unused. Abu Bashir, a lined, thin 28-year-old, pointed to his boat and said, "Fishing is almost impossible now. The waves are much bigger than they used to be. It used to be fine to go out in a normal [hand-rowed] boat. That is how my father and my grandfather and my ancestors lived.

"Now that is impossible. You need a [motor-driven] boat, and even that is thrown about by the waves so much. It's like the bay is angry."

The other fishermen burst in. "When there is a cyclone warning, we cannot go out fishing for 10 days. That is a lot of business lost. There used to be two or three warnings a year. Last year, there were 12. The sea is so violent. We are going hungry."

Yet the islanders insisted on offering me a feast of rice and fish and eggs. I was ushered into the council leader's house – a rusty shack near the sea – and the men sat around, urging me to tell the world what is happening. "If people know what is happening to us, they will help," they said. The women remained in the back room; when I glimpsed them and tried to thank them for the food, they giggled and vanished. I asked if the men had heard of global warming, and they looked puzzled. "No," they said. We stared out at the ocean and ate, as the sun slowly set on the island.

3. No hiding place

Through the morning mist, I peered out of the car window at the cratered landscape. Trees jutted out at surreal angles from the ground. One lay upside down with its roots sticking upwards towards the sky, looking like a sketch for a Dali painting. Shambrat had spat out his pan and was driving slowly now. "There are holes in the ground," he said, squinting with concentration. "From the cyclone. You fall in..." He made a splattering sound.

It was here, in the south of Bangladesh, that on 15 November last year, Cyclone Sidr arrived. It formed in the warmed Bay of Bengal and ripped across the land, taking more than 3,000 people with it. Like Americans talking about 9/11, everybody in Bangladesh knows where they were when Sidr struck. For miles, the upturned and smashed-out houses are intermixed with tents made from blue plastic sheeting. These stretches of plastic were handed out by the charities in the weeks after Sidr, and many families are still living in them now.

There have always been cyclones in Bangladesh, and there always will be – but global warming is making them much more violent. Back in Dhaka, the climatologist Ahsan Uddin Ahmed explained that cyclones use heat as a fuel: "The sea surface temperatures in the Bay of Bengal have been rising steadily for the past 40 years – and so, exactly as you would expect, the intensity of cyclones has risen too. They're up by 39 per cent on average." Again I circled a cyclone-struck island at random and headed for the dot.

The hour-long journey on a wooden rowing boat from the mainland to Charkashem Island passed in a dense mist that made it feel like crossing the River Styx. The spectral outline of other boats could sometimes be glimpsed, before they disappeared suddenly. One moment an old woman and a goat appeared and stared at me, then they were gone.

The island was a tiny dot of mud and lush, upturned greenery. It had no pier, so when the rowing boat bumped up against the sand I had to wade through the water.

I looked out over the silent island, and saw some familiar blue sheeting in the distance. As I trudged towards it, I saw some gaunt teenagers half-heartedly kicking a deflated football. From the sheeting, a man and woman stared, astonished.

"I was in my fields over there," Hanif Mridha said. "I saw the wind start, it was about eight at night, and I saw everything being blown around. I went and hid under an iron sheet, but that was blown away by the wind. The water came swelling up all of a sudden and was crashing all around me. I grabbed one of my children and ran to the forest" – he pointed to the cluster of trees at the heart of the island – "and climbed the tallest one I could reach. I went as high as I could but still the water kept rising and I thought – this is it, I'm going to drown. I'm dying, my children are dying, my wife is dying. I could see everything was under water and people were screaming everywhere. I held there for four hours with my son."

When the water washed away and he came down, everything was gone: his house, his crops, his animals, his possessions. A few days later, an aid agency arrived with some rice and some plastic sheeting to sleep under. Nobody has come since.

His wife, Begum Mridha, took over the story. Their children are terrified of the sea now, and have nightmares every night. They eat once a day, if they're lucky. "We are so hungry," she said. The new home they have built is made from twigs and the plastic sheet. Underneath it, they sleep with their eight children and Begum Mridha's mother. The children lay lethargically there, staring blankly into space over their distended bellies.

Begum Mridha cooks on a lantern. They eat once a day – if that. "It's so cold at night we can't sleep," she said. "The children all have diarrhoea and they are losing weight. It will take us more than two years to save up and get back what we had."

If cyclones hit this area more often, what would happen to you? Hanif looked down. He opened his mouth, but no words came.
Read more »

March 1, 2008

নারিকেল জিঞ্জিরা - পর্ব ২

মুনতাসির মামুন ইমরান

পরদিন সকালে বেরুলাম জরীপ কাজে৷ মূল উদ্দেশ্য শাহপুরি থেকে শুরু হলে আমাদের সাতার সেন্ট মার্টিনের কোথায় শেষ হবে তা ঠিক করা৷ বেশ কঠিন কাজ৷ স্রোত দেখা, গভীরতা মাপা, এটা সেটা কত কি৷ সারা বেলা গেল এই করতেই৷ বিকালে গ্রিল ফিসের সাথে ক্যাম্প ফায়ার৷ আতিক ভাইয়ের ওসিয়ানিক স্কুবা ডাইভিং স্কুলের উঠান তখন ভরপুর৷ এনজেল ডাস্ট এর সাজ্জাদ ভাই, ইকো টুরস্ এর রাকা ভাই, কাশেম মাষ্টার সাহেব, মেম্বার সাহেবেরা আরও কত জন৷ বিশাল এক আয়োজন৷ রান্নার আয়োজক ফারুখ ভাই৷ দৈনিক জনকন্ঠের মাধ্যমে অনেকেই তার রেসিপি পেয়েছেন হয়তো বা৷ রাত ১০টা পর্যন্ত চলল আনন্দ ঘন্টা৷

পরদিন সকালে আতিক ভাইয়ের সাথে সবাই নামলাম সাগরে৷ বিশাল সাগরের উত্তাল জলরাশি কিছুটা কান্ত এই শীতে তাতে কি বাকিটা যা আছে তাও কম কিসে৷ চলল দাপাদাপি৷ সবাই একসাথে৷ বিশাল আকার ধারন করল যখন ছোট ছোট ছেলে মেয়েরা যোগ দিল মিছিলে৷ মহাসমুদ্রের পারে জলত্‍সব৷ এর মাঝে যোগ হল হামিদ ভাইয়ের র্যাফ্ট বোটে মেয়েদের আনন্দ ভ্রমন৷ কেউ সাঁতরে কেউ নৌকায় কেউবা লাইফ জ্যকেটের ভরসায়৷ এর মাঝে ফারক ভাই নামলেন গ্যাস ডাইভিং এ৷ যথেষ্ট আনন্দ উপভোগ করে আমরা গেলাম আসল কাজে৷ পার ধরে বোটে নিয়ে এগিয়ে যেতে থাকলাম ছেড়া দ্বীপের দিকে৷ আমি হামিদ ভাই Sonrkeling করে আর বোটে রিমন, জাহাঙ্গির আর সেলিম ভাই৷ সাগরে সাতার কাটছি৷ একটু অন্যরকম৷ প্রথম দিনে হিসেবে ভাই হলো৷ প্রায় ৪ কিলোমিটার৷ দুপুর হয়ে গেছে৷ ফেরার পালা এবার৷ সমস্যা দেখা দিল তখনই৷ এতোনতো আশা হয়েছে স্রোতের দিকে আর এবার বিপরিতে৷ বোটে তখন ৪ জন৷ একজনকে আগেই নামিয়ে দেয়া হয়েছে৷ তাও কিছুটা যাওয়ার পরই হামিদ ভাই আর সেলিম ভাই নেমে গেলেন৷ প্রায় ১ ঘন্টা অনন্ত চেষ্টা করার পর কিছুটা এগুতে পারলাম৷ এর পর ডাইভ ট্যাঙ্ক কাধে নিয়ে নেমে এলাম৷ মাথার উপর রোদ আর পায়ের নিচে আগুনে গরম বালি৷ অস্থির অবস্থা৷ যখন পৌছলাম আমাদের বেইজ ক্যাম্পে তখন শরীরে শক্তির শেষ রিন্দুটা বাকি বোধ হয়৷ গিয়ার গুলো থেকে লবণ পানি পরিস্কার করে শুকাতে দেয়ার পর নিজের গোসল সেরে খাওয়া দাওয়া৷ তাও ভাল ফারুখ ভাই ছিলেন৷ তাই আলিশান খাওয়া হচ্ছিল বেশ৷ বিকালটা তো কখন গেল বুঝতেই পারলাম না৷ সূর্যাস্থ দেখলাম৷ রাত হলে শুধুই আড্ডা আর আড্ডা৷ পরদিনের পরিকল্পনা করা হলো রাতের খাওয়ার পর৷

সকালের নাস্তা সেরে দল মিলে বেরুলাম৷ আজ সরাসরি চলে গেলাম ছেড়া দ্বীপে, হেটে৷ পথের মাঝেই আমরা না না ধরনের কোরাল দেখতে পেলাম৷ যদিও কোনটাই আর বেচে নেই৷ পানিতে নেমে গেলাম৷ নানা ধরনের নানা বর্ণের কোরাল দেখতে পেলাম, দেখলাম মাছ৷ আমার বাসার একুরিয়ামটা আমার প্রথম দিকে খুব ভাল লাগত৷ কিন্তু এখন আর তেমন না৷ কারন একুরিয়াম খুবই সীমাবন্ধ এক জলাধার৷ কিন্তু এখন আমি যেখানে তা আমার বাসার একুরিয়ামের চেয়ে তো কম নয়ই বরং বিশাল৷ এত মাছ আর কত যে রং৷ অবাক হতে হয় বিশ্ময়কর এই জগত দেখার সৌভাগ্য হয়তো অনেকেরই হয়নি৷ নারিকেল জিনজিরার সৌন্দর্য্য অবাক করা, কোন সন্দেহ নাই৷ কিন্তু এর পানির নিচের অবসথা আরও রোমঞ্চকর৷ আরও সুন্দর৷ সেন্ট মার্টিন কে কেন কোরাল দ্বীপ বলা হয় তা এবার বুঝতে পারলাম৷ হরেক রকমের কোরাল তার প্রকৃষ্ট উদাহরন৷ এখন প্রশ্ন আসতে পারে সেন্ট মার্টিন কে কেন কোরাল আইলেন্ড বলা হয়৷ মুলত এখানে শক্ত এবং কেরালাইন লাইমষ্টোন দেখাতে পাওয়া যায়৷ এগুলোই কোরার কাস্টার হিসেবে পরিবর্তিত হয়ে যায় পরবর্তীকালে। আর সেন্ট মার্টিন এ প্রচুর পরিমানে কোরালের উপস্তিতিই এ দ্বীপকে 'কোরাল দ্বীপ' বলতে বাধ্য করে, যদিও প্রথম দিকে এর কোন বৈজ্ঞানিক ব্যাখ্যা ছিল না৷ কিন্তু ১৯৮৫ সালে নারিকেল জিনজিরা কে জাতীয় মেরিন পার্ক হিসেবে প্রস্তাব করা হয় কোরাল রিফের উপস্থিতির কারনে৷ (খান, ১৯৮৫; আনোয়ার,১৯৮৮)

কোরাল রীফ বলতে আমরা হামেশাই বুঝে ফেলি রং বেরং এর পাথরের আশে পাশে সুন্দর সুন্দর মাছ আর ক্রিস্টাল কিয়ার পানি৷ উপর থেকে তাকালে যেন তলদেশ দেখা যায় (!)৷ ভ্রান্ত ধারনা ছাড়া এটা কিছুই না৷ আসলে কোরাল রীফে সৃষ্টির মূলে রয়েছে নানাবিধ জটিল প্রাকৃতিক প্রক্রিয়া৷ Boitic এবং Abiotic এর ক্রিয়ার মাধ্যমে Calcification, Cementation, Consolidation, Wind, Sea level fluctuation, Current ইত্যাদির নানা ধাপ অতিক্রম করে তৈরি হয় বিভিন্ন আকারের রীফ৷ স্যার চালর্স ডারউন কোরাল রীফ কে তিন ভাগে ভাগ করেছেন, fringing reefs, barrier reefs, Atolls ।

ডারউনের ধারনা অনুযায়ী fringing reefs গুলো সবচেয়ে কম সময়ে তৈরী হয় এবং মূল ভূ খন্ড বা উচু জমির সাথে কোন না কোন ভাবে যুক্ত থাকে৷ কিন্তু অন্যদিকে barrier reefs, Atolls গুলো কিছুটা বেশি সময় নিয়ে তৈরি হয়ে থাকে৷ fringing reefs ধরনের রীফ গুলোকেই উষ্ণ মন্ডলীয় সাগর এবং উপসাগরে বেশি দেখতে পাওয়া যায়৷ সাধারন পর্যটকদের আর্কষন হয়ে দাড়ায় এরাই৷ স্কুবা ডাইভারদের আনন্দের মূল উপাদান হিসেবে পরিচিতি লাভ করে খুব দ্রুত৷ নারিকেল জিনজিরার আশে পাশে অল্প গভীর জলে এধরনের কোরাল দেখা যায় প্রচুর৷ দ্বীপের উত্তর পশ্চিমে এবং দনি পূর্বে বেশ কিছু লেগুন দেখা গেলেও তারা বেরিয়ার রীফের মত মোটেও গভীর নয়৷ এধরনের লেগুন বা খাড়িতে পাওয়া যায় প্রচুর মাছ৷ নদী মাতৃক এদেশে বিদেশী অনেক খেলা প্রচলিত থাকলেও জল কেন্দ্রিক কোন জনপ্রিয় খেলা আছে কিনা আমার জানা নেই৷ থাকলেও ঐ একটাই, নৌকা বাইচ৷ কিন্তু প্রচুর লোকবল দরকার সেখানেও৷ সে হিসেবে water ski, bording, snorkeling, scuba diving ইত্যাদি হতে পারে নারিকেল জিনজিরার অন্যতম আকর্ষনীয় বিনোদন মাধ্যম৷ এধরনের স্পোর্টসের জন্য খুব বেশি পয়সাকড়ি কিংবা লোক বলের প্রয়োজন হয় না৷ তাও ভাল এবারে দেখে এলাম আতিক ভাইয়ের সাহসী উদ্দোগ৷ ব্যবসায়ীক চিন্তা ধারায় তৈরী হলেও প্রসংশার দাবীদার এক বাক্যে৷ পানির নিচের আলাদা জগত্‍টা আমাদের কাছে হয়তো কোন দিনও পরিচিত হত না, ওশিয়ানিক স্কুবা ডাইভিং সার্ভিস এর কল্যানে তাও এখন কিছুটা সম্বব৷

অর্থকরী খরচ করে প্রবাল দ্বীপে যাওয়ার পরে প্রবাল না দেখাটা বোধ করি অন্যায়৷ বিচারে কার সৌন্দর্য বেশি তা আমি বলতে পারব না কিন্তু এটা ঠিক সাগরের নিচটা অসাধারন৷ এর জন্য নিজ থেকে দরকার শারীরীক যোগ্যতা আর সাতার জানা৷ দ্বীপের চারপাশের প্রায় সব জায়গাতেই দেখা যায় হরেক রকমের মাছ৷ আছে জলজ উদ্বিদ আর প্রবাল৷ আর এসব দেখার জন্য মাঝ দরিয়ায় ঝাপ দেয়ার কোন দরকার নাই৷ তীরবর্তী ১০ থেকে ১৫ ফুট গভীরতার মধ্যেই দেখা যাবে এত কিছু৷ এধরনের অল্প গভীর পানিতে থাকে ভাল সূর্যে আলো আর তাই পরিবেশ হয়ে ওঠে আরও দর্শনীয়৷ ভাগ্য ভাল থাকলে দেখা যাবে হাজার হাজার মাছের ঝাক৷ বিলাশ লম্বা মাছের ঝাকের মধ্যে কখন যে ঢুকে পরবেন তা বোঝাও যাবে না৷ আরও কিছুন ধর্য্য ধরলে পাওয়া যাবে বড় মাছের দেখা৷ কারন ছোট মাছ গুলোকে তারা করে নিয়ে চলে বড় মাছ৷ তাই হঠাত্‍ই হতো সামনে চলে আসবে বড় কিছু৷ ভয় পাওয়ার দরকার নাই৷ খুবই নিরিহ এরা৷

প্রবাল গুলোকে কাছ থেকে দেখতে প্রথমে অবশ্যই ভয়ঙ্কর মনে হতে পারে৷ কেমন যেন একটা পরিবেশ৷ একে তো একেবারে অপরিচিত তার উপর বিদঘুটে অবয়ব কোন কোনটার৷ কোটার রং উজ্বল সবুজ আবার কোনটা লালচে ধরনের৷ মৌমাছির চাকের মত দেখতে এক ধরনের প্রবাল৷ তাদের নামও হানিকম্ব৷ এটার নাম ব্রেন কেরাল, উপর থেকে দেখতে অবশ্যই মগজের মতই মনে হয়৷ হালকা বাদামীর মাঝে কিছুটা সবুজে অংশ এটাকে আরও খানিকটা ভয়ংকর করে তোলে৷ কিন্তু কিছুটা সময় এদের মাঝে সাতার কাটলেই বোঝা যাবে এরা কতটা নিরীহ৷ মূলত মাছের খাদ্য হিসেবে এরা ব্যবহৃত হয়৷ সমস্য হলো অন্যখানে, প্রবাল গুলোতে থাকে মারাত্নক ধার৷ একটু অসতর্ক হলেই আর রা নেই৷ দূঘর্টনা হতে বাধ্য৷ সেলিম ভাইয়ের পায়ে যে পরিমান কেটে গিয়েছিল তাদেখে আমরা বেশ ভয়ই পেয়ে গিয়েছিলাম৷ অন্য অবস্থায় হলে আমরা অবশ্যই হাসপাতালে যেতাম৷ কিন্তু এই উন্মুক্ত প্রান্তরে কেন জানি কেউই তারাহুরো দেখালাম না৷ মনে হয় সবাই জানতাম, এখানে এটা এমনি ঠিক হয়ে যাবে৷ ডাইভ বোট থেকে নামার সময় খেয়াল না করায় তার এই অবস্থা৷ ফার্ষ্ট এইড দেয়া হলো৷ কিছুটা রা৷ আমাদের নিজেদের অভিজ্ঞতা মতে দ্বীপের প্রায় সব জায়গায় স্কুবা বা স্নর্কলিং করা গেলেও ছেড়া দ্বীপ এবং এর আশ পাশের জায়গা গুলো প্রায় স্বর্গ ৷ উচু নিচু কেরাল আর পাথরের জন্য মাছ ধরাটা এখানে কিছুটা কম৷ উত্তর পূর্বে সবচেয়ে বেশি সুন্দর৷ এখানে স্কুবা করা যাবে প্রায় অনেক খানি জায়গায়৷ আর যদি আরও খানিকটা বহি সমুদ্রে যাওয়া যায় তবে দেখা যাবে সার্কদের৷ এটা অবশ্য আমার কথা না, বাংলাদেশ নৌ বাহিনীর কয়েকজন ডাইভারের সঙ্গে দেখা হয়ে যাওয়াতে আমি জিজ্ঞেস করেছিলাম৷ হামিদ ভাইও তাই বলেন৷ হয়তোবা কোন একদিন জাতীয় কোন জনপ্রিয় দৈনিকে দেখা যাবে "Guaranteed dive with hammer head Shark" নামের বিজ্ঞাপণ৷ এটা অসম্ভব নয়, শুধু দরকার উদ্যোগ৷ আমরা সবাই যাব ঢাকা থেকে, সারা দেশ থেকে৷ অবাক করা সৌন্দর্য শহর নারিকেল জিনজিরায় আর সাগর তলের দেখা আলোর না দেখা রুপ দেখতে৷ উত্তর পাড়ার বাম পাশটায় দেখা যাবে বেশ কয়েকটা লেগুন৷ ভাটার সময় হাটু পানি৷ আর জোয়ারে বুক৷ বিদেশি বইতে পাওয়া লেগুনের শোভা দেখতে পাওয়া যাবে চোখের সামনে৷ কিছুন ধৈর্য্য আর একটু খেয়াল করলে এমনিতেই দেখা যাবে ঝাক ঝাক মাছ ৷ আর যদি কিছু বিস্কিটের গুড়ো নিয়ে যাওয়া যায় তবে তো আর কথাই নাই৷ সময় হারিয়ে যাবে সমুদ্রের কাছে৷ এখানে একটা কথা বলে রাখা উচিত, খালি পায়ে কোন অবস্থাতেই কোরাল কিংবা তীরে হাটা উচিত না৷ এতে করে পাদুকা জোড়া ভিজে নষ্ট হওয়ার ভয় থাকলেও পায়ের যত্ন আগে নেয়া উচিত, নয়তো সারা ট্রিপই ভন্ডুল৷ চলতে থাকল আমাদের অভিযান, সারা দিন, সারা বেলা, সেই সকাল থেকে বিকাল অবদি কান্তি এলেও হামিদ ভাইয়ের কাছ থেকে ছাড় পাওয়া যেত না৷ আনডার ওয়াটার ফটোগ্রাফি করার সময় তো জান যায় যায়৷ আমার ৩ মি মি পুরু ডাইভ স্যুটটায় ঠান্ডা মানত না ঘন্টা খানেক পর৷ একটার পর একটা ডুবদিয়ে ছবি তোলা৷ তাও মুভমেন্টে ভুল হলে আবার করতে হতো৷ কিছুই করার নাই, শুধু এটাই ভাবি আমি যার সাথে কাজ করছি তার অভিজ্ঞতায় National Geography এর সাথে কাজ করার অভিজ্ঞতা৷ এটা শুধু পাওয়া না যে কারও জন্য ভাগ্য বলা যায়, অন্তত আমার মত কারউ জন্য৷ সমস্যা হলো একদিনে এক রোল ছবির বেশি তোলা যেত না৷ ক্যামেরাটা শুকাতে হত তারপর আবার অন্য আরেকটা রোল৷ পানি থেকে ওঠার পর জেকে বসত ঠান্ডা৷ তাই নিয়েই ছেড়া দ্বীপের মৌসুমি আর সাদ্দামের দোকানে পালা করে চা আর গরম মাছ ভাজা খেতাম৷ দাম একটুও বেশি না৷ বরং মূল বাজারের যে কোন দোকানের চেয়ে বেশ খানিকটা তো কমই৷ তার উপর বাসি খাবার পাওয়ার কোন ভয় নেই৷ বাজারের হোটেল গুলো সাতদিন আগের মাছ আজকের বলে দেধারে চালিয়েদেয়৷ তবে কিছু দোকানের খাবারের কথা না বললেই নয়,উন্মুক্ত সাগরের পারে বসে Angel Dust এর খাবার কারও খারাপ লাগবে বলে মনে হয় না৷ ডেকরেশান এবং অন্যান্য সব কিছুই বেশ আলাদা৷ প্রায়ই আমরা দলবেধে কফি খেতে যেতাম৷ পরন্ত বেলা সূর্যাস্থ দেখা না গেলেও আকাশটা কে ভারি অদ্ভুত লাগত৷ এটাই বা কম কি, এত কম টাকায় এত সুন্দর আকাশ আর কোথায় কেনা যায় ?

রাতের বেলা সেলিম ভাই হঠাত্‍ করেই তাবু থেকে বের হয়ে সবাইকে ডাকাডাকি শুরু করে দিলেন৷ অনেক রাতে ঘুমাতে যাওয়ার পর আবার ডাকাডাকি কেন, যা হোক শোনা গেল, কিছুন আগে ভূমিকম্প হয়ে গেছে৷ আমি অবশ্য কিছুই বুঝিনি৷ প্রথমটা তো আমরা বিশ্বাসই করিনি৷ কিন্তু সকালে ওস্তাদ( নেভির অবসর প্রাপ্ত কমান্ড ডাইভার শাহনেয়াজ ভাই ) এর কাছেও তাই জানা গেল৷ আর এখানে ভুমিকম্প মোটেও নতুন কোন ঘটনা না৷ আসলে আমরা সবাই ভূমিকম্পের ধ্বংসের ঘটনা কমবেশি জানি৷ কিন্তু এটাবোধ হয় জানি না যে পৃথিবীর আকর্ষনীয় কোরাল রীফ গুলো গড়ে ওঠে ভূমিকম্পন প্রবণ এলাকা গুলো থেকে৷ বাংলাদেশের জন্য এটাই সত্য যে ভূমিকম্প এখানে কোরাল রীফ গড়ে তুলতে কার্যকরী ভাবে সাহায্য করেছে৷ যেমনটা দেখা যায় ইন্দোনেশিয়ায়৷ সেখানে ভূকম্পনের ফলে কোরাল রীফের কলোনি তৈরি হয়েছে অনেক৷,সেদেশের আরকিপেলাগো (Archipelago) পৃথিবীর মধ্যে সবচেয়ে বেশি ভূকম্পন প্রবন এলাকা হিসেবে চিহ্নিত৷ আর এখানেই গড়ে উঠেছে অতুলনীয় সব কোরাল সিসটেম৷ নারিকেল জিনজিরার ক্ষেত্রে ধরা হয় বহু বছর আগে বড় বড় পাথরের বোল্ডার গুলো একসাথে জোড়া লেগেছিল এই কোরাল দিয়ে যা দিয়ে রীফ তৈরি হয়৷ আর হয়তোবা বড় ধরনের কোন ভূকম্পের ফলে বোল্ডার গুলো সরে গেছে মূল ভূমি থেকে৷ যদিও তেমন কোন বড় ধরনের ভূমিকম্পের কথা জানা যায় না৷ তবুও বৈজ্ঞানিক ভাবে এটাই ধারনা করা হয়৷ তবে এতটুকু জানা যায় দ্বীপটির উপরিভাগের খানিকটা নিচেই আছে বড় বড় বোল্ডার, যারা নিজেরা সমান্তরাল ভাবে অবস্তিত৷ অনেকের মতে এই পাথরের গঠনই দ্বীপ তৈরির মূল উপাদান এবং এরা ভূমিকম্পনে না হলেও বড় ধরনের সাইকোনিক ঝড়ের কারনেও এরা মূলভূমি কিংবা সমুদ্রতল থেকে চাপের কারনে জেগে উঠেছে৷ তাই এর উত্‍পত্তি নিয়ে আছে মতভেদ৷ বৃদ্ধ ব্যক্তিদের কাছ থেকে জানা যায় আগে নাকি বার্মা আর এই দ্বীপ ছিল পাশাপাশি৷ নাফ নদীটাই ছিল শুধু এদের মাঝে৷ ধীরে ধীরে দ্বীপ সরে আসে, নাফ নদী চওড়া হতে থাকে৷ তার কারন তারা জানেনা৷ তবে এরসবই পৌরাণিক কাহিনীর মত৷

অনিনন্দ্য সুন্দর এই দ্বীপ আমাদের দেশের গর্ব৷ একটু পরিকল্পনা আর দায়িত্বশীল হস্তপেই বদলে দিতে পারে এর পুরো রুপ৷ বর্তমানে দ্বীপটি বেশ কিছু দিক থেকে হুমকির সামনে৷ টুরিজমের নামে ইটের বদলে প্রবালের ব্যবহার, গ্যাস, তেল, নৌকার বর্জ্য ইত্যাদি যত্রতত্র নিক্ষেপ ৷ নোঙ্গর ফেলার ফলে ভেঙ্গে যাচ্ছে তলদেশের প্রবাল গুলো৷ এত সুন্দর এই দ্বীপে কোন স্থায়ী জেটি নেই, নেই কোন ভাসমান Anchorage System, ভাবতে অবাক লাগে ! ছোট ছোট নৌকা গুলোকে তীরে তোলার সময় হয়ে যাচ্ছে অপুরনীয় ক্ষতি, প্রবাল গুলো যাচেছ ভেঙ্গে৷ তার উপরেও তো আছে প্রবাল সংগ্রহকারীদের দৌরাত্ব৷ আমরা যদি এভাবে হিসেব করি, প্রতি বছর সারা দেশ থেকে ৩০,০০০ পর্যটক যদি এ দ্বীপ থেকে মাত্র একটা করে ছোট প্রবালও নিয়ে যায় তবে অবস্থাটা কি হবে? ভাবা উচিত্‍ সবার৷ সরকারী অফিস কিংবা অন্যন্য স্থানে বাগানের আশেপাশে লেখা থাকে ' ফুল ছিড়বেন না ' ইত্যাদি ইত্যাদি, কিন্তু হায় ! এমন একটা লেখাও চোখে এলনা যে প্রবাল ধ্বংস বা সংগ্রহ থেকে দূরে থাকুন৷ অবস্থার পরিবর্তন না হলে হয়তো নিকট ভবিষতে প্রবাল দ্বীপে পা ভেজানর পানি আর ঢাকা থেকে আমদানি করা সামুদ্রিক মাছ পাওয়া গেলেও প্রবাল আর পাওয়া যাবে না৷ তখন বোধ হয় 'গুলিস্তান' সিনেমা হল বিহীন গুলিস্তানের মতোই প্রবালহীন প্রবাল দ্বীপ হবে আমাদের সেইন্ট মার্টিন্স আইলেন্ড৷।
সূত্র: http://www.nature.com.bd
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