The DOI matches its Crossref record; 67 of the 69 references it cites were found in a registry or an index.
Warming up, turning sour, losing breath: ocean biogeochemistry under global change
Abstract
In the coming decades and centuries, the ocean's biogeochemical cycles and ecosystems will become increasingly stressed by at least three independent factors. Rising temperatures, ocean acidification and ocean deoxygenation will cause substantial changes in the physical, chemical and biological environment, which will then affect the ocean's biogeochemical cycles and ecosystems in ways that we are only beginning to fathom. Ocean warming will not only affect organisms and biogeochemical cycles directly, but will also increase upper ocean stratification. The changes in the ocean's carbonate chemistry induced by the uptake of anthropogenic carbon dioxide (CO(2)) (i.e. ocean acidification) will probably affect many organisms and processes, although in ways that are currently not well understood. Ocean deoxygenation, i.e. the loss of dissolved oxygen (O(2)) from the ocean, is bound to occur in a warming and more stratified ocean, causing stress to macro-organisms that critically depend on sufficient levels of oxygen. These three stressors-warming, acidification and deoxygenation-will tend to operate globally, although with distinct regional differences. The impacts of ocean acidification tend to be strongest in the high latitudes, whereas the low-oxygen regions of the low latitudes are most vulnerable to ocean deoxygenation. Specific regions, such as the eastern boundary upwelling systems, will be strongly affected by all three stressors, making them potential hotspots for change.…
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Self-citationOcean Acidification: The Other CO 2 Problem
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2 of the 69 references couldn’t be matched to a known paper.
Research works printed but not linked: 6
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Multiple stressors of ocean ecosystems in the 21st century: projections with CMIP5 models
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Zalasiewicz, J., Waters, C. N., do Sul, J. A. I., Corcoran, P. L., Barnosky, A. D., Cearreta, A., Edgeworth, M., Gałuszka, A., Jeandel, C., Leinfelder, R., et al. (2016) · Anthropocene · doi:10.1016/j.ancene.2016.01.002 · Cited by 1,019
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Metadata
- Authors
- Gruber, N.
- Affiliations
- ETH Zurich (CH)
- Corresponding author
- Gruber, Nicolas
- ORCID
- Gruber, Nicolas
- Venue
- Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
- Publisher
- The Royal Society
- Published
- 2011-05-28
- Volume
- 369
- Issue
- 1943
- Pages
- 1980-1996
- ISSN
- 1364-503X (ISSN-L)
- 1471-2962
- OpenAlex
- W2155033464
- Cited by
- 588
- References
- 69
- Citations by year
- 2026: 23 · 2025: 38 · 2024: 48 · 2023: 59 · 2022: 43 · 2021: 44 · 2020: 42 · 2019: 40 · 2018: 34 · 2017: 46 · 2016: 42 · 2015: 38 · 2014: 37 · 2013: 24 · 2012: 25
- FWCI
- 20.29
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences (publishedVersion)
- PubMed (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine Plankton and Biogeochemistry
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Ocean Acidification Effects and Responses
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Keywords
- ocean warming, ocean acidification, ocean deoxygenation, marine biogeochemical cycles, ocean stratification, carbonate chemistry, dissolved oxygen, eastern boundary upwelling systems, organic matter export, synergistic effect, global change, anthropogenic CO2 uptake, CO2 emission reduction
- MeSH terms
- Carbon Dioxide, Hydrogen-Ion Concentration, Oceans and Seas, Oxygen, Seawater, Greenhouse Effect, Climate Change, Global Warming
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