4.5 Article

Impacts of hypoxic events surpass those of future ocean warming and acidification

Journal

NATURE ECOLOGY & EVOLUTION
Volume 5, Issue 3, Pages -

Publisher

NATURE PORTFOLIO
DOI: 10.1038/s41559-020-01370-3

Keywords

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Funding

  1. Fundacao para a Ciencia e Tecnologia (FCT) [UID/MAR/04292/2019, SFRH/BD/131771/2017, SRFH/SFRH/BD/117890/2016, CEECIND/02484/2018]
  2. European Social Fund (ESF), through the Human Capital Operating Programme and Regional Operation Programme (Lisboa 2020) [UID/MAR/04292/2019, SFRH/BD/131771/2017, SRFH/SFRH/BD/117890/2016, CEECIND/02484/2018]
  3. DFG Centre of Excellence 2117 'Centre for the Advanced Study of Collective Behaviour' [422037984]
  4. NSF [OCE1829623]
  5. NOAA CHRP award [NA18NOS4780172]
  6. PACES programme of the AWI
  7. DFG (German Research Council) [Po 278 16-1, Po 278 16-2]

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The meta-analysis revealed that hypoxia has a larger negative impact on marine organisms compared to warming and acidification, affecting survival, abundance, development, metabolism, growth, and reproduction. This highlights the importance of considering oxygen concentration as a key factor in future experimental studies on global change in marine environments.
A meta-analysis of experimental effects of stressors on marine organisms shows that hypoxia could harm crustaceans, mollusks and fish to a larger extent than warming and acidification. Over the past decades, three major challenges to marine life have emerged as a consequence of anthropogenic emissions: ocean warming, acidification and oxygen loss. While most experimental research has targeted the first two stressors, the last remains comparatively neglected. Here, we implemented sequential hierarchical mixed-model meta-analyses (721 control-treatment comparisons) to compare the impacts of oxygen conditions associated with the current and continuously intensifying hypoxic events (1-3.5 O-2 mg l(-1)) with those experimentally yielded by ocean warming (+4 degrees C) and acidification (-0.4 units) conditions on the basis of IPCC projections (RCP 8.5) for 2100. In contrast to warming and acidification, hypoxic events elicited consistent negative effects relative to control biological performance-survival (-33%), abundance (-65%), development (-51%), metabolism (-33%), growth (-24%) and reproduction (-39%)-across the taxonomic groups (mollusks, crustaceans and fish), ontogenetic stages and climate regions studied. Our findings call for a refocus of global change experimental studies, integrating oxygen concentration drivers as a key factor of ocean change. Given potential combined effects, multistressor designs including gradual and extreme changes are further warranted to fully disclose the future impacts of ocean oxygen loss, warming and acidification.

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