Strong and weak monsoons can affect marine productivity in the Bay of Bengal, a study exploring fluctuations in the Indian Summer Monsoon (ISM) over the previous 22,000 years has discovered. Marine productivity is a proxy for plankton progress – the principle supply of nourishment for aquatic life. The study is important provided that a number of local weather fashions warn of vital disruption to the monsoon, beneath the affect of human-caused warming.
The study, which seems in the peer-reviewed, Nature Geoscience, introduced collectively scientists from India, China, Europe and the United States.
“By analysing their chemistry and tracking the abundance of certain types that thrive in productive waters, we reconstructed long-term changes in rainfall, ocean temperatures and marine life in the Bay of Bengal,” mentioned Kaustubh Thirumalai, of the University of Austin and lead writer of the study. “Together, these chemical signals helped us understand how the monsoon and ocean conditions responded to global climate changes over the past 22,000 years.”
Despite overlaying lower than 1% of the world’s ocean space, the Bay of Bengal gives practically 8% of world fishery manufacturing. Its nutrient-rich coastal waters are important to the densely populated communities alongside its shores, many of whom rely closely on fisheries for meals and earnings.
“Millions of people living along the Bay of Bengal rely on the sea for protein, particularly from fisheries,” mentioned Yair Rosenthal, of the Rutgers University and a co-author. “The productivity of these waters – the ability of the ocean to support plankton growth – is the foundation of the marine food web. If ocean productivity declines, it will powerfully affect the ecosystem, ultimately reducing fish stocks and threatening food security for coastal communities.”
The study discovered that each abnormally robust and weak monsoons all through historical past prompted main disruptions in ocean mixing, resulting in a 50% discount in meals for marine life in the floor waters. This happens as a result of excessive monsoon circumstances intrude with the vertical motion of nutrient-rich waters from the deep ocean to the floor, the place plankton—the bottom of the meals chain—flourish.
To reconstruct previous ocean circumstances, scientists analysed fossilised shells of foraminifera, tiny single-celled marine organisms that document environmental information in their calcium carbonate shells. These microfossils have been retrieved from seafloor sediments by scientists aboard the JOIDES Resolution, a analysis ship working beneath the International Ocean Discovery Program.
The researchers discovered that marine productivity declined sharply during times like Heinrich Stadial 1 (a chilly section between 17,500 and 15,500 years in the past) and the early Holocene (about 10,500 to 9,500 years in the past), when monsoons have been both unusually weak or robust. Monsoon rainfall immediately impacts river run-off into the Bay of Bengal, altering ocean salinity and circulation. When an excessive amount of freshwater builds up on the floor, it prevents nutrient mixing. Conversely, weak monsoons scale back wind-driven mixing, additionally ravenous floor waters of vitamins.
“Both extremes threaten marine resource availability,” Mr. Thirumalai mentioned.
By evaluating historical patterns with trendy ocean information and local weather mannequin projections, researchers recognized “worrying” similarities, the authors mentioned in an announcement. Future situations recommend hotter floor waters and stronger freshwater run-off—circumstances linked to previous drops in marine productivity. Additionally, weaker future winds could fail to interrupt by way of ocean stratification and restore nutrient biking.
Published – April 29, 2025 11:19 am IST
