Results 81 to 90 of about 1,403,380 (198)
The Paleocene–Eocene thermal maximum (PETM), a transient period of global warming, is considered to be an important analog for future greenhouse conditions. It was accompanied by a significant carbon cycle perturbation.
Xiao-Dong Jiang +9 more
semanticscholar +1 more source
Marine Functional Connectivity Contributes to Ecosystem Functioning Across Multiple Scales
ABSTRACT The passive transport and active movements of marine organisms between habitats and ecosystems, known as marine functional connectivity, play a critical role in the functioning of marine ecosystems. However, marine functional connectivity, particularly at large spatial scales, is often understudied, and consequently tends to be overlooked in ...
Lucía López‐López +23 more
wiley +1 more source
Multi‐stressor experiments on three coral species demonstrate hypoxia produces mostly additive effects with acidification but synergistically amplifies physiological stress under elevated temperatures. As global and local environmental change increase compound stress events on coral reefs, distinguishing hypoxia‐driven effects and interactive stressor ...
Kelly W. Johnson +4 more
wiley +1 more source
Expanded subsurface ocean anoxia in the Atlantic during the Paleocene-Eocene Thermal Maximum
The ocean has experienced substantial oxygen loss over recent decades, affecting marine ecosystems and fisheries. Investigating ocean deoxygenation during hyperthermal events, such as the Paleocene-Eocene Thermal Maximum (PETM), offers insights into its ...
Weiqi Yao +5 more
doaj +1 more source
Expansion of oceanic anoxia is a prevailing hypothesis for driving the marine end-Permian mass extinction and is mainly based on isotopic geochemical proxies.
Min Zhang +6 more
semanticscholar +1 more source
Abstract Sediments in productive coastal regions are hotspots of hydrogen sulfide (H2S) production through microbial sulfate reduction. Under anoxic seafloor conditions, H2S can escape the sediment and accumulate in bottom waters, where elevated concentrations render the benthic environment toxic, posing ecological and economic risks.
Timo Spiegel +9 more
wiley +1 more source
Climatic controls on metabolic constraints in the ocean [PDF]
Observations and models indicate that climate warming is associated with the loss of dissolved oxygen from the ocean. Dissolved oxygen is a fundamental requirement for heterotrophic marine organisms (except marine mammals) and, since the basal metabolism
P. Mongwe +5 more
doaj +1 more source
Shallow ocean deoxygenation drove trilobite turnover during the late Cambrian SPICE event
The spread of marine anoxia is believed to have played a key role in the development of the SPICE (Steptoean Positive Carbon Isotope Excursion) event and the end-Marjuman extinction in the late Cambrian (∼497.5 m.y.
Aihua Yang +12 more
semanticscholar +1 more source
Sedimentary lycopane/n‐C31 ratio as a proxy for bottom water hypoxia in coastal ocean
Abstract Bottom‐water hypoxia on continental shelves is intensifying under climate change and eutrophication, yet long‐term records remain scarce. Here we show that the sedimentary lycopane/n‐C31 ratio reliably records bottom‐water oxygenation in the seasonally hypoxic Yangtze River Estuary.
Qingnan Song +6 more
wiley +1 more source
Abstract Progressive ocean acidification and deoxygenation are expected to threaten many marine zooplankton, but their combined effects across life stages remain poorly understood. We investigated stage‐specific responses of the egg‐carrying copepod Pseudodiaptomus annandalei to changes in pHT (5.97–8.05) and dissolved oxygen (DO; 0.90–8.20 mg L−1 ...
Weijia Chen, Kunshan Gao
wiley +1 more source

