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  4. Microbial respiration in contrasting ocean provinces via high-frequency optode assays
 
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Microbial respiration in contrasting ocean provinces via high-frequency optode assays

Journal
Frontiers in Marine Science
Journal Volume
11
ISSN
2296-7745
Date Issued
2024-06-05
Author(s)
Cohn, Melanie R.
BRANDON MICHAEL STEPHENS  
Meyer, Meredith G.
Sharpe, Garrett
Niebergall, Alexandria K.
Graff, Jason R.
Cassar, Nicolas
Marchetti, Adrian
Carlson, Craig A.
Gifford, Scott M.
DOI
10.3389/fmars.2024.1395799
URI
https://www.scopus.com/pages/publications/85196319609
https://scholars.lib.ntu.edu.tw/handle/123456789/731177
Abstract
Microbial respiration is a critical component of the marine carbon cycle, determining the proportion of fixed carbon that is subject to remineralization as opposed to being available for export to the ocean depths. Despite its importance, methodological constraints have led to an inadequate understanding of this process, especially in low-activity oligotrophic and mesopelagic regions. Here, we quantify respiration rates as low as 0.2 µmol O2 L-1 d-1 in contrasting ocean productivity provinces using oxygen optode sensors to identify size-fractionated respiration trends. In the low productivity region of the North Pacific Ocean at Station Papa, surface whole water microbial respiration was relatively stable at 1.2 µmol O2 L-1 d-1. Below the surface, there was a decoupling between respiration and bacterial production that coincided with increased phytodetritus and small phytoplankton. Size-fractionated analysis revealed that cells <5 µm were responsible for the majority of the respiration in the Pacific, both at the surface and below the mixed layer. At the North Atlantic Porcupine Abyssal Plain, surface whole water microbial respiration was higher (1.7 µmol O2 L-1 d-1) than in the Pacific and decreased by 3-fold below the euphotic zone. The Atlantic size-fraction contributions to total respiration shifted on the order of days during the evolution of a phytoplankton bloom with regular storm disturbances. The high-resolution optode method used in the Atlantic captured these significant shifts and is consistent with coinciding stain-based respiration methods and historical site estimates. This study highlights the dynamic nature of respiration across vertical, temporal, and size-fractionated factors, emphasizing the need for sensitive, high-throughput techniques to better understand ocean ecosystem metabolism.
Subjects
bacteria
carbon
dissolved oxygen
marine
microbial respiration
ocean
optode
size-fractionated
SDGs

[SDGs]SDG13

[SDGs]SDG14

Publisher
Frontiers Media SA
Type
journal article

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