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Bacterioplankton response to physical stratification following deep convection

Bibliographic Data

ID19568413
AuthorsNicholas Baetge (0000-0002-3868-9857, University of California, Santa Barbara), Luis M Bolaños (0000-0002-0832-016X, University of Exeter), Alice Della Penna (0000-0002-7579-3610, University of Auckland), Peter Gaube (0000-0002-3282-5803, University of Washington Applied Physics Laboratory), Shuting Liu (0000-0002-7178-2703, University of California, Santa Barbara), Keri Opalk (0000-0001-7068-0601, University of California, Santa Barbara), Jason R Graff (0000-0003-0029-3299, Oregon State University), Stephen J Giovannoni (0000-0002-2431-4296, Oregon State University), Michael J Behrenfeld (0000-0003-1330-7098, Oregon State University), Craig A Carlson (0000-0003-2591-5293, University of California, Santa Barbara)
Year2022
Volume10
Issue1
Publication date2022-08-02
Open AccessYes
TypeARTICLE
VenueElementa Science of the Anthropocene (JOURNAL)
Journal identifiersISSN: 2325-1026 • E-ISSN: 2325-1026
PublisherUniversity of California Press (PUBLISHER • US)
DOI10.1525/elementa.2021.00078
OpenAlexW4289535388
LanguageEN
References cited104

Dissolved organic carbon (DOC) produced by primary production in the sunlit ocean can be physically transported to the mesopelagic zone. The majority of DOC exported to this zone is remineralized by heterotrophic microbes over a range of timescales. Capturing a deep convective mixing event is rare, as is observing how microbes respond in situ to the exported DOC. Here, we report ship and Argo float observations from hydrostation North Atlantic Aerosols and Marine Ecosystems Study (NAAMES) 2 Station 4 (N2S4; 47.46°N, 38.72°W), a retentive anticyclonic eddy in the subtropical region of the western North Atlantic. Changes in biogeochemistry and bacterioplankton responses were tracked as the water column mixed to approximately 230 m and restratified over the subsequent 3 days. Over this period, rapid changes in bacterioplankton production (BP) and cell abundance were observed throughout the water column. BP increased by 91% in the euphotic zone (0–100 m) and 55% in the upper mesopelagic zone (100–200 m), corresponding to 33% and 103% increases in cell abundance, respectively. Within the upper mesopelagic, BP upon the occupation of N2S4 (20 ± 4.7 nmol C L–1 d–1) was significantly greater than the average upper mesopelagic BP rate (2.0 ± 1.6 nmol C L–1 h–1) at other stations that had been stratified for longer periods of time. BP continued to increase to 31 ± 3.0 nmol C L–1 d–1 over the 3-day occupation of N2S4. The rapid changes in BP in the upper mesopelagic did not coincide with rapid changes in community composition, but the taxa that increased in their relative contribution included those typically observed in the epipelagic zone. We interpret the subtle but significant community structure dynamics at N2S4 to reflect how injection of labile organic matter into the upper mesopelagic zone by physical mixing supports continued growth of euphotic zone-associated bacterioplankton lineages on a timescale of days

Bacterioplankton · Biogeochemistry · Biology · Dissolved organic carbon · Mesopelagic zone · Nutrient · Ocean gyre · Pelagic zone · Photic zone · Phytoplankton · Subtropics · Water column · Zooplankton · Environmental Science · Marine and coastal ecosystems · Marine Biology and Ecology Research · Microbial Community Ecology and Physiology · Ecology · Geology · Oceanography

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