A study reconstructed Antarctic Bottom Water (AABW) history over 4.7 million years, revealing collapses tied to intensified Northern Hemisphere glaciation and poor seawater oxygenation, with implications for past and future climate dynamics.
Antarctic bottom water (AABW) covers more than two-thirds of the global ocean bottom, and its formation has recently decreased. However, its long-term variability has not been well understood.
Researchers led by Prof. Chenglong Deng from the Institute of Geology and Geophysics (IGG) of the Chinese Academy of Sciences (CAS) and their collaborators have reconstructed AABW history back to approximately 4.7 million years ago (mya). They found that AABW has collapsed several times and such collapses might have induced moisture transport to fuel the Northern Hemisphere glaciation (NHG).
This work will be published today (February 24, 2023) in the journal Science Advances.
The study was based on a 36-mm (1.4-inch) diameter Fe-Mn nodule from the Eastern Pacific, located 5,050 m (16,568 feet) below sea level. The nodule was collected by Guangzhou Marine Geological Survey, China Geological Survey.
Magnetic scanning was an important factor in providing precise dating results. “This is a key, though the final dating was obtained by an integration with 10Be/9Be, flux of metal Co, and astronomical tuning,” said Dr. Liang Yi from Tongji University, first author of the study and a postdoc at IGG/CAS.
“Since AABW is the main provider of oxygen in the ocean bottom region, we used various scientific methods to identify the relation between metal accumulation in the Fe-Mn nodule and oceanic redox conditions,” said Prof. Deng. “Ni, Mn, and Cu contents are used to indicate AABW changes.”
These results show that seawater oxygen has experienced a linear increase in the Eastern Pacific since around 3.4 mya. This trend agrees with the observation of the Antarctic Ice Sheet (AIS), suggesting a covariation between them.
Comparing the AABW record with other geological records from the past million years, the researchers found a glacial enhancement of oceanic bottom circulation. This observation implies that atmospheric CO2 may have been regularly stored in the deep ocean when Earth’s climate was cold, e.g., during past glacial periods.
The comparisons clearly highlighted seven intervals of poor seawater oxygen, suggesting AABW influence was reduced to a much lower level. These periods are known as AABW collapse and accompanied an enhancement of North Atlantic Deepwater (NADW) as well as key stages of NHG history, such as when NHG became intensified or amplified.
Although we don’t know what will happen in response to ongoing AIS melting and AABW slowing, AABW collapse might have pulled the Earth into a harsher glacial climate several times in the past.
Reference: “Plio-Pleistocene deep-sea ventilation in the eastern Pacific and potential linkages with Northern Hemisphere glaciation” by Liang Yi, Martín Medina-Elizalde, Liangcheng Tan, David B. Kemp, Yanzhen Li, Gunther Kletetschka, Qiang Xie, Huiqiang Yao, Huaiyu He, Chenglong Deng and James G. Ogg, 24 February 2023, Science Advances.
DOI: 10.1126/sciadv.add1467
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4 Comments
“This observation implies that atmospheric CO2 may have been regularly stored in the deep ocean when Earth’s climate was cold, e.g., during past glacial periods.”
Are we to assume then that it is released back into the atmosphere when Earth warms?
Yes, that is the generally accepted model. And there are vast amounts of CO2 to be potentially released, both in the deep ocean and also other sinks in frozen tundra regions.
What does this mean for humans?…what fix is there on a micro and/or macro scale? Is this not being connected to global warming intentionally to keep it out mainstream knowledge?
What does this mean for humans?…what fix is there on a micro and/or macro scale? Is this not being connected to global warming intentionally to keep it out mainstream knowledge?