Jelly biomass sinking speed reveals a fast carbon export mechanism ...

Sinking of gelatinous zooplankton biomass is an important component of the biological pump removing carbon from the upper ocean. The export efficiency, e.g., how much biomass reaches the ocean interior sequestering carbon, is poorly known because of the absence of reliable sinking speed data. We mea...

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Main Authors: Lebrato, Mario, Mendes, Pedro André, Steinberg, Deborah K, Birsa, Laura M, Benavides, Mar, Oschlies, Andreas
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2013
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.831964
https://doi.pangaea.de/10.1594/PANGAEA.831964
id ftdatacite:10.1594/pangaea.831964
record_format openpolar
spelling ftdatacite:10.1594/pangaea.831964 2024-03-31T07:54:46+00:00 Jelly biomass sinking speed reveals a fast carbon export mechanism ... Lebrato, Mario Mendes, Pedro André Steinberg, Deborah K Birsa, Laura M Benavides, Mar Oschlies, Andreas 2013 application/zip https://dx.doi.org/10.1594/pangaea.831964 https://doi.pangaea.de/10.1594/PANGAEA.831964 en eng PANGAEA https://dx.doi.org/10.4319/lo.2013.58.3.1113 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Biological Impacts of Ocean Acidification BIOACID Supplementary Publication Series of Datasets article Collection 2013 ftdatacite https://doi.org/10.1594/pangaea.83196410.4319/lo.2013.58.3.1113 2024-03-04T13:38:31Z Sinking of gelatinous zooplankton biomass is an important component of the biological pump removing carbon from the upper ocean. The export efficiency, e.g., how much biomass reaches the ocean interior sequestering carbon, is poorly known because of the absence of reliable sinking speed data. We measured sinking rates of gelatinous particulate organic matter (jelly-POM) from different species of scyphozoans, ctenophores, thaliaceans, and pteropods, both in the field and in the laboratory in vertical columns filled with seawater using high-quality video. Using these data, we determined taxon-specific jelly-POM export efficiencies using equations that integrate biomass decay rate, seawater temperature, and sinking speed. Two depth scenarios in several environments were considered, with jelly-POM sinking from 200 and 600 m in temperate, tropical, and polar regions. Jelly-POM sank on average between 850 and 1500 m/d (salps: 800-1200 m/d; ctenophores: 1200-1500 m/d; scyphozoans: 1000-1100 m d; pyrosomes: 1300 ... : Supplement to: Lebrato, Mario; Mendes, Pedro André; Steinberg, Deborah K; Birsa, Laura M; Benavides, Mar; Oschlies, Andreas (2013): Jelly biomass sinking speed reveals a fast carbon export mechanism. Limnology and Oceanography, 58(3), 1113-1122 ... Article in Journal/Newspaper Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) Andreas ENVELOPE(-60.729,-60.729,-64.008,-64.008) Benavides ENVELOPE(-58.267,-58.267,-63.933,-63.933)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Biological Impacts of Ocean Acidification BIOACID
spellingShingle Biological Impacts of Ocean Acidification BIOACID
Lebrato, Mario
Mendes, Pedro André
Steinberg, Deborah K
Birsa, Laura M
Benavides, Mar
Oschlies, Andreas
Jelly biomass sinking speed reveals a fast carbon export mechanism ...
topic_facet Biological Impacts of Ocean Acidification BIOACID
description Sinking of gelatinous zooplankton biomass is an important component of the biological pump removing carbon from the upper ocean. The export efficiency, e.g., how much biomass reaches the ocean interior sequestering carbon, is poorly known because of the absence of reliable sinking speed data. We measured sinking rates of gelatinous particulate organic matter (jelly-POM) from different species of scyphozoans, ctenophores, thaliaceans, and pteropods, both in the field and in the laboratory in vertical columns filled with seawater using high-quality video. Using these data, we determined taxon-specific jelly-POM export efficiencies using equations that integrate biomass decay rate, seawater temperature, and sinking speed. Two depth scenarios in several environments were considered, with jelly-POM sinking from 200 and 600 m in temperate, tropical, and polar regions. Jelly-POM sank on average between 850 and 1500 m/d (salps: 800-1200 m/d; ctenophores: 1200-1500 m/d; scyphozoans: 1000-1100 m d; pyrosomes: 1300 ... : Supplement to: Lebrato, Mario; Mendes, Pedro André; Steinberg, Deborah K; Birsa, Laura M; Benavides, Mar; Oschlies, Andreas (2013): Jelly biomass sinking speed reveals a fast carbon export mechanism. Limnology and Oceanography, 58(3), 1113-1122 ...
format Article in Journal/Newspaper
author Lebrato, Mario
Mendes, Pedro André
Steinberg, Deborah K
Birsa, Laura M
Benavides, Mar
Oschlies, Andreas
author_facet Lebrato, Mario
Mendes, Pedro André
Steinberg, Deborah K
Birsa, Laura M
Benavides, Mar
Oschlies, Andreas
author_sort Lebrato, Mario
title Jelly biomass sinking speed reveals a fast carbon export mechanism ...
title_short Jelly biomass sinking speed reveals a fast carbon export mechanism ...
title_full Jelly biomass sinking speed reveals a fast carbon export mechanism ...
title_fullStr Jelly biomass sinking speed reveals a fast carbon export mechanism ...
title_full_unstemmed Jelly biomass sinking speed reveals a fast carbon export mechanism ...
title_sort jelly biomass sinking speed reveals a fast carbon export mechanism ...
publisher PANGAEA
publishDate 2013
url https://dx.doi.org/10.1594/pangaea.831964
https://doi.pangaea.de/10.1594/PANGAEA.831964
long_lat ENVELOPE(-60.729,-60.729,-64.008,-64.008)
ENVELOPE(-58.267,-58.267,-63.933,-63.933)
geographic Andreas
Benavides
geographic_facet Andreas
Benavides
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://dx.doi.org/10.4319/lo.2013.58.3.1113
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.83196410.4319/lo.2013.58.3.1113
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