The ocean's chemistry is altering in several ways.
Ocean pH has increased by about 0.1 since the start of the Industrial Revolution, or an increase in acidity of about 30%, and it could increased by 0.2 to 0.3 by 2100 1. Uptake of carbon is the main cause of ocean acidification, or the long-term trend of falling ocean pH. Ocean acidification poses a threat to marine ecosystems.
Class of Life | Survival | Calcification | Growth | Photosynthesis/Development | Abundance |
---|---|---|---|---|---|
Calcifying Algae | ? | --- | ? | -28% | -80% |
Corals | --- | -32% | --- | --- | -47% |
Coccolithophore Plankton | ? | -23% | --- | --- | --- |
Mollusks | -34% | -40% | -17% | -25% | --- |
Echinoderms | --- | --- | -10% | -11% | ? |
Crustaceans | --- | --- | --- | --- | --- |
Fish | ? | ? | --- | ? | ? |
Fleshy Algae | ? | ? | 22% | --- | --- |
Seagrasses | ? | ? | ? | --- | ? |
Diatom Plankton | ? | ? | 17% | 12% | --- |
Ocean acidification has negative impacts of fisheries, the ocean as a carbon sink, and the tourism, scentific, and cultural value of biodiversity 3. Losses has been estimated to reach $1 trillion per year by 2100 under projected CO2 emissions 4.
The ocean is becoming saltier over time, with fresh areas generally become fresher and salty areas become saltier 1. This trend is expected to have a modest warming effect on the climate 5.
The oceans' oxygen content has decreased by about 2% since 1960 6, 7, though oxygen levels have increased in some areas near river mouths due to fertilizer runoff 8. Rising temperature reduces the oceans' ability to take in oxygen, and this may be the main factor in the loss 1. Ocean patches of low oxygen may in turn drive warming by increasing emissions of nitrous oxide 1.
United Nations "The Second World Ocean Assessment". 2021. ↩ ↩2 ↩3 ↩4
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Navrud, S., Seifert-Dähnn, I. "The Economics of Ocean Acidification - A Scoping Study". Fram Centre 57. January 2012. ↩
Secretariat of the Convention on Biological Diversity. An Updated Synthesis of the Impacts of Ocean Acidification on Marine Biodiversity. (Eds: S. Hennige, J.M. Roberts & P. Williamson). Montreal, Technical Series No. 75, 99 pages. 2014. ↩
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Ito, T., Minobe, S., Long, M. C., Deutsch, C. "Upper ocean O2 trends: 1958–2015". Geophysical Research Letters 44(9), pp. 4214-4223. April 2017. ↩
Keeling, R. E., Körtzinger, A., Gruber, N. "Ocean deoxygenation in a warming world". Annual review of marine science 2: pp. 199-229. 2010. ↩