KOSMOS 2014 mesocosm study: The influence of plankton community structure on sinking velocity and remineralization rate of marine aggregates ...
Gravitational sinking of photosynthetically fixed particulate organic carbon (POC) constitutes a key component of the biological carbon pump. The fraction of POC leaving the surface ocean depends on POC sinking velocity (SV) and remineralization rate (Cremin), both of which depend on plankton commun...
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ftdatacite:10.1594/pangaea.902901 2024-03-31T07:54:46+00:00 KOSMOS 2014 mesocosm study: The influence of plankton community structure on sinking velocity and remineralization rate of marine aggregates ... Bach, Lennart Thomas 2019 application/zip https://dx.doi.org/10.1594/pangaea.902901 https://doi.pangaea.de/10.1594/PANGAEA.902901 en eng PANGAEA https://store.pangaea.de/Publications/Bach_2019/Bach-2019-Script.zip https://dx.doi.org/10.1029/2019gb006256 https://dx.doi.org/10.1594/pangaea.889745 https://dx.doi.org/10.1594/pangaea.889731 https://store.pangaea.de/Publications/Bach_2019/Bach-2019-Script.zip Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Biological Impacts of Ocean Acidification BIOACID Supplementary Publication Series of Datasets article Collection 2019 ftdatacite https://doi.org/10.1594/pangaea.90290110.1029/2019gb00625610.1594/pangaea.88974510.1594/pangaea.889731 2024-03-04T13:34:28Z Gravitational sinking of photosynthetically fixed particulate organic carbon (POC) constitutes a key component of the biological carbon pump. The fraction of POC leaving the surface ocean depends on POC sinking velocity (SV) and remineralization rate (Cremin), both of which depend on plankton community structure. However, the key drivers in plankton communities controlling SV and Cremin are poorly constrained. In fall 2014, we conducted a 6 weeks mesocosm experiment in the subtropical NE Atlantic Ocean to study the influence of plankton community structure on SV and Cremin. Oligotrophic conditions prevailed for the first 3 weeks, until nutrient‐rich deep water injected into all mesocosms stimulated diatom blooms. SV declined steadily over the course of the experiment due to decreasing CaCO3 ballast and – according to an optical proxy proposed herein – due to increasing aggregate porosity mostly during an aggregation event after the diatom bloom. Furthermore, SV was positively correlated with the contribution ... : Supplement to: Bach, Lennart Thomas; Stange, Paul; Taucher, Jan; Achterberg, Eric Pieter; Algueró-Muñiz, Maria; Horn, H; Esposito, Mario; Riebesell, Ulf (2019): The Influence of Plankton Community Structure on Sinking Velocity and Remineralization Rate of Marine Aggregates. Global Biogeochemical Cycles, 33(8), 971-994 ... Article in Journal/Newspaper Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Biological Impacts of Ocean Acidification BIOACID |
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Biological Impacts of Ocean Acidification BIOACID Bach, Lennart Thomas KOSMOS 2014 mesocosm study: The influence of plankton community structure on sinking velocity and remineralization rate of marine aggregates ... |
topic_facet |
Biological Impacts of Ocean Acidification BIOACID |
description |
Gravitational sinking of photosynthetically fixed particulate organic carbon (POC) constitutes a key component of the biological carbon pump. The fraction of POC leaving the surface ocean depends on POC sinking velocity (SV) and remineralization rate (Cremin), both of which depend on plankton community structure. However, the key drivers in plankton communities controlling SV and Cremin are poorly constrained. In fall 2014, we conducted a 6 weeks mesocosm experiment in the subtropical NE Atlantic Ocean to study the influence of plankton community structure on SV and Cremin. Oligotrophic conditions prevailed for the first 3 weeks, until nutrient‐rich deep water injected into all mesocosms stimulated diatom blooms. SV declined steadily over the course of the experiment due to decreasing CaCO3 ballast and – according to an optical proxy proposed herein – due to increasing aggregate porosity mostly during an aggregation event after the diatom bloom. Furthermore, SV was positively correlated with the contribution ... : Supplement to: Bach, Lennart Thomas; Stange, Paul; Taucher, Jan; Achterberg, Eric Pieter; Algueró-Muñiz, Maria; Horn, H; Esposito, Mario; Riebesell, Ulf (2019): The Influence of Plankton Community Structure on Sinking Velocity and Remineralization Rate of Marine Aggregates. Global Biogeochemical Cycles, 33(8), 971-994 ... |
format |
Article in Journal/Newspaper |
author |
Bach, Lennart Thomas |
author_facet |
Bach, Lennart Thomas |
author_sort |
Bach, Lennart Thomas |
title |
KOSMOS 2014 mesocosm study: The influence of plankton community structure on sinking velocity and remineralization rate of marine aggregates ... |
title_short |
KOSMOS 2014 mesocosm study: The influence of plankton community structure on sinking velocity and remineralization rate of marine aggregates ... |
title_full |
KOSMOS 2014 mesocosm study: The influence of plankton community structure on sinking velocity and remineralization rate of marine aggregates ... |
title_fullStr |
KOSMOS 2014 mesocosm study: The influence of plankton community structure on sinking velocity and remineralization rate of marine aggregates ... |
title_full_unstemmed |
KOSMOS 2014 mesocosm study: The influence of plankton community structure on sinking velocity and remineralization rate of marine aggregates ... |
title_sort |
kosmos 2014 mesocosm study: the influence of plankton community structure on sinking velocity and remineralization rate of marine aggregates ... |
publisher |
PANGAEA |
publishDate |
2019 |
url |
https://dx.doi.org/10.1594/pangaea.902901 https://doi.pangaea.de/10.1594/PANGAEA.902901 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
https://store.pangaea.de/Publications/Bach_2019/Bach-2019-Script.zip https://dx.doi.org/10.1029/2019gb006256 https://dx.doi.org/10.1594/pangaea.889745 https://dx.doi.org/10.1594/pangaea.889731 https://store.pangaea.de/Publications/Bach_2019/Bach-2019-Script.zip |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.90290110.1029/2019gb00625610.1594/pangaea.88974510.1594/pangaea.889731 |
_version_ |
1795035967780814848 |