Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Jesse M. Wilson"'
Autor:
Sonia Marie Vargas, J.S. Karolewski, A E Cairo, J M Beman, Elisabet Perez-Coronel, Scott D. Wankel, Lihini I. Aluwihare, S Vazquez, Irina Koester, Jesse M. Wilson, A Yu, Margot E. White
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-11 (2021)
Nature Communications
Nature Communications
Oceanic oxygen minimum zones (OMZs) are globally significant sites of biogeochemical cycling where microorganisms deplete dissolved oxygen (DO) to concentrations
Oxygen is fundamental for marine life, yet it is absent from large areas of the oce
Oxygen is fundamental for marine life, yet it is absent from large areas of the oce
Publikováno v:
Environmental Microbiology. 23:3225-3239
A multitude of concurrent biological and physical processes contribute to microbial community turnover, especially in highly dynamic coastal environments. Characterizing what factors contribute most to shifts in microbial community structure and the
Autor:
Jennifer B. Glass, Peter T. Doran, Nestor Arandia-Gorostidi, Jesse M. Wilson, Britney E. Schmidt, Jeff S. Bowman, Natalia Erazo, Luke A. Fisher, Douglas H. Bartlett, Avishek Dutta, Christopher E. Carr, Benjamin Klempay, Anne E. Dekas, Alexandra Pontefract, Sanjoy M. Som
Publikováno v:
Environmental Microbiology. 23:3825-3839
Concurrent osmotic and chaotropic stress make MgCl2 -rich brines extremely inhospitable environments. Understanding the limits of life in these brines is essential to the search for extraterrestrial life on contemporary and relict ocean worlds, like
Autor:
Jesse M. Wilson, Natalia Erazo, Elizabeth Connors, Emelia J. Chamberlain, Samantha M. Clements, Melissa L. Carter, Jennifer E. Smith, Jeff S. Bowman
Publikováno v:
Elementa: Science of the Anthropocene. 10
Phytoplankton blooms create organic matter that stimulates entire marine ecosystems, including other components of the microbial community. How the ecosystem responds varies depending on the intensity, duration, and composition of the bloom. When the
Publikováno v:
PLoS ONE, Vol 9, Iss 7, p e99821 (2014)
Community respiration (CR) of organic material to carbon dioxide plays a fundamental role in ecosystems and ocean biogeochemical cycles, as it dictates the amount of production available to higher trophic levels and for export to the deep ocean. Yet
Externí odkaz:
https://doaj.org/article/d3e604b92b1b47d6b8976ef1cf4054c7
Autor:
Sonia Marie Vargas, Jesse M. Wilson, Samantha Vazquez, Ariadna Cairo, Elisabet Perez-Coronel, Angela Yu, J. Michael Beman
Publikováno v:
Environmental microbiologyReferences. 23(6)
Oceanic oxygen minimum zones (OMZs) play a pivotal role in biogeochemical cycles due to extensive microbial activity. How OMZ microbial communities assemble and respond to environmental variation is therefore essential to understanding OMZ functionin
Publikováno v:
Environmental Microbiology Reports. 10:272-282
Respiration of organic material is a central process in the global carbon (C) cycle catalysed by diverse microbial communities. In the coastal ocean, upwelling can drive variation in both community respiration (CR) and the microbial community, but li
Publikováno v:
Scientific Reports
Scientific Reports, Vol 9, Iss 1, Pp 1-12 (2019)
Scientific Reports, Vol 9, Iss 1, Pp 1-12 (2019)
Dissolved oxygen (DO) concentrations shape the biogeochemistry and ecological structure of aquatic ecosystems; as a result, understanding how and why DO varies in space and time is of fundamental importance. Using high-resolution, in situ DO time-ser
Publikováno v:
Environmental Microbiology. 18:4907-4919
Summary Microbial communities consume oxygen, alter biogeochemistry and compress habitat in aquatic ecosystems, yet our understanding of these microbial–biogeochemical–ecological interactions is limited by a lack of systematic analyses of low-oxy
Publikováno v:
Frontiers in Marine Science. 4
Declining ocean oxygen content driven by anthropogenic climate change has wide-ranging ramifications for marine ecosystems. These effects are significant but complex at the upper margins of expanding oxygen minimum zones (OMZs), where deoxygenation a