Ocean deoxygenation in a warming world.

By R. Keeling, A. Körtzinger, N. Gruber. Annual Review of Marine Science, 2010

1,620 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/6eb84fb35aa3d5c68ce4efcfe43d6958b05b4f99

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In Oceanography

Citations in the corpus

Acute survivorship of the deep-sea coral Lophelia pertusa from the Gulf of Mexico under acidification, warming, and deoxygenation (2014, background): “ORIGINAL RESEARCH ARTICLE published: 19 December 2014 doi: 10.3389/fmars.2014.00078 Acute survivorship of the deep-sea coral Lophelia pertusa from the Gulf of Mexico under acidification, warming, and deoxygenation”
Quantification of ammonia oxidation rates and ammonia‐oxidizing archaea and bacteria at high resolution in the Gulf of California and eastern tropical North Pacific Ocean (2012, background): “Adding to this complexity, OMZs are expanding as a consequence of climate change (Keeling et al. 2010), altering the rates and distribution of N transformations in the water column.”
Deep, diverse and definitely different: unique attributes of the world's largest ecosystem (2010, background): “…gas from methane hydrates, normally kept “frozen” under very proscribed conditions with a positive feedback on global warming (Kenvelvoden, 1988) and an increase in the extension of pelagic and benthic OMZs (Stramma et al., 2008) caused by stratification of the upper ocean (Keeling et al., 2010).”
Beyond the Calvin cycle: autotrophic carbon fixation in the ocean. (2011, background): “In recent years, OMZs have received increased attention as they are expected to increase in response to climate change, with potential deleterious effects to oceanic ecosystems (Keeling et al. 2010).”
Ocean oxygen minima expansions and their biological impacts (2010, background): “, Ocean oxygen minim observing system to track ocean oxygen changes (Keeling et al., 2010).”
Ocean acidification and marine microorganisms : responses and consequences (2015, background): “Current understanding about marine microbial physiology is inadequate to sufficiently understand the consequences of OA (Keeling et al., 2010; Range et al., 2011).”
Oxygen distribution and aerobic respiration in the north and south eastern tropical Pacific oxygen minimum zones (2014, background): “Since oxygen is directly linked to carbon by photosynthesis and respiration, it is a diagnostic of the rate at which organic matter cycles in the Oceans (Keeling et al., 2010; Stramma, 2008).”
Climate change impacts on marine ecosystems. (2012, background): “Projected declines in ocean oxygen levels reflect the combined effects of reduced oxygen solubility from warming and reduced ventilation from stratification and circulation changes (Keeling et al. 2010).”
Man and the Last Great Wilderness: Human Impact on the Deep Sea (2011, background): “Current models predict an oxygen decline of 1% to 7% in the next 100 years [248] with an expansion of pelagic and benthic OMZs [249].”
Future challenges in cephalopod research* (2014, background): “Depending on how widespread this habit is among pelagic cephalopods, changes in the oxygen minimum layer associated with global climate change will have effects on other species (Bograd et al., 2008; Stramma et al., 2008; Keeling et al., 2010; Gilly et al., 2013).”
Zooplankton in the eastern tropical north Pacific: Boundary effects of oxygen minimum zone expansion (2013, neutral): “+1 401874 6523. ner). change (Stramma et al., 2008; Hofmann and Schellnhuber, 2009; Keeling et al., 2010) or natural climate oscillations (Deutsch et al., 2011).”
Effects of seawater pCO2 and temperature on shell growth, shell stability, condition and cellular stress of Western Baltic Sea Mytilus edulis (L.) and Arctica islandica (L.) (2013, background): “edulis if temperatures higher than 20 C coincide with high pCO2 levels—which is likely to occur more often in future (Keeling et al. 2010; Melzner et al. 2012).”