Abstract
Recent studies on marine heat waves describe water temperature anomalies causing changes in food web structure, bloom dynamics, biodiversity loss, and increased plant and animal mortality. However, little information is available on how water temperature anomalies impact prokaryotes (bacteria and archaea) inhabiting ocean waters. This is a nontrivial omission given their integral roles in driving major biogeochemical fluxes that influence ocean productivity and the climate system. Here we present a time-resolved study on the impact of a large-scale warm water surface anomaly in the northeast subarctic Pacific Ocean, colloquially known as the Blob, on prokaryotic community compositions. Multivariate statistical analyses identified significant depth- and season-dependent trends that were accentuated during the Blob. Moreover, network and indicator analyses identified shifts in specific prokaryotic assemblages from typically particle-associated before the Blob to taxa considered free-living and chemoautotrophic during the Blob, with potential implications for primary production and organic carbon conversion and export.
Originalsprog | Engelsk |
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Artikelnummer | 1217 |
Tidsskrift | Communications Biology |
Vol/bind | 4 |
Udgave nummer | 1 |
Antal sider | 12 |
DOI | |
Status | Udgivet - 2021 |
Bibliografisk note
Funding Information:We would like to thank the captain, crew, and scientists onboard the CCGS John P. Tully for their extraordinary efforts in the field over many years, and Tijana Glavina del Rio at the DOE Joint Genome Institute (JGI) for project management on sample submission and sequencing. We also thank the many undergraduate helpers in the Hallam lab and ocean-going technical support staff including Jade Shiller and Chris Payne for their support in sample collection and processing. This work was performed under the auspices of the Scientific Committee on Oceanographic Research (SCOR), the US Department of Energy (DOE) Joint Genome Institute, an Office of Science User Facility, supported by the Office of Science of the U.S. Department of Energy under Contract DE-AC02-05CH11231, the G. Unger Vetlesen and Ambrose Monell Foundations, the Natural Sciences and Engineering Research Council of Canada, the Canada Foundation for Innovation, and the Canadian Institute for Advanced Research through grants awarded to S.J.H. S.J.T. was supported by the Danish Research Council (grant DFF-7027-00043B) and CTEK by the Tula Foundation.
Publisher Copyright:
© 2021, The Author(s).