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Shallow marine ecosystem collapse and recovery during the Paleocene-Eocene Thermal Maximum

Abstract.

"The Paleocene-Eocene Thermal Maximum (PETM), the most well-studied transient hyperthermal event in Earth history, is characterized by prominent and dynamic changes in global marine ecosystems. Understanding such biotic responses provides valuable insights into future scenarios in the face of anthropogenic warming. However, evidence of the PETM biotic responses is largely biased towards deep-sea records, whereas shallow-marine evidence remains scarce and elusive. Here we investigate a shallow-marine microfaunal record from Maryland, eastern United States, to comprehensively document the shallow-marine biotic response to the PETM. We applied birth-death modeling to estimate the local diversity dynamics[...]"

 

Source: Elsevier
Authors: Skye Yunshu Tian  et al.
DOI: https://doi.org/10.1016/j.gloplacha.2021.103649

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Hydrostatic pressure is the universal key driver of microbial evolution in the deep ocean and beyond

Abstract.

"Oceans cover approximately 70% of the Earth’s surface, and microbes comprise 90% of the ocean biomass and are regarded as an important ‘hidden’ driver of essential elemental cycling, such as carbon cycling, in the oceans (Karl, 2007; Salazar and Sunagawa, 2017). Although the general public – even many scientists – think of the oceans as unified, stable water systems, they contain varied environments, including extreme environments such as oxygen-deficient zones, oligotrophic open ocean, polar water regions, deep ocean[...]"

 

Source: Environmental Microbiology Reports
Authors: Xiang Xiao et al.
DOI: 10.1111/1758-2229.12915 

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