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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Main Author: Bach, Lennart Thomas
Format: Dataset
Language:English
Published: PANGAEA 2019
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.902901
https://doi.org/10.1594/PANGAEA.902901
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.902901
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.902901 2023-05-15T17:51:52+02:00 KOSMOS 2014 mesocosm study: The influence of plankton community structure on sinking velocity and remineralization rate of marine aggregates Bach, Lennart Thomas LATITUDE: 27.928060 * LONGITUDE: -15.365280 * DATE/TIME START: 2014-09-27T00:00:00 * DATE/TIME END: 2015-10-18T00:00:00 2019-06-24 application/zip, 5 datasets https://doi.pangaea.de/10.1594/PANGAEA.902901 https://doi.org/10.1594/PANGAEA.902901 en eng PANGAEA Taucher, Jan; Bach, Lennart Thomas (2018): KOSMOS 2014 mesocosm study: flow cytometry. PANGAEA, https://doi.org/10.1594/PANGAEA.889745 Taucher, Jan; Nauendorf, Alice (2018): KOSMOS 2014 mesocosm study: chlorophyll a. PANGAEA, https://doi.org/10.1594/PANGAEA.889731 Matlab script and test data for mesocosm model equation, Bach 2019 (URI: https://store.pangaea.de/Publications/Bach_2019/Bach-2019-Script.zip) https://doi.pangaea.de/10.1594/PANGAEA.902901 https://doi.org/10.1594/PANGAEA.902901 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY 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, https://doi.org/10.1029/2019GB006256 BIOACID Biological Impacts of Ocean Acidification Dataset 2019 ftpangaea https://doi.org/10.1594/PANGAEA.902901 https://doi.org/10.1029/2019GB006256 https://doi.org/10.1594/PANGAEA.889745 https://doi.org/10.1594/PANGAEA.889731 2023-01-20T07:34:21Z 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 of picophytoplankton to the total phytoplankton biomass. Cremin was highest during a Synechococcus bloom under oligotrophic conditions and in some mesocosms during the diatom bloom after the deep‐water addition while it was particularly low during harmful algal blooms. The temporal changes were considerably larger in Cremin (max. 15‐fold) than in SV (max. 3‐fold). Accordingly, estimated POC transfer efficiency to 1000 m was mainly dependent on how the plankton community structure affected Cremin. Our approach revealed key players and interactions in the plankton food web influencing POC export efficiency thereby improving our mechanistic understanding of the biological carbon pump. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-15.365280,-15.365280,27.928060,27.928060)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic BIOACID
Biological Impacts of Ocean Acidification
spellingShingle BIOACID
Biological Impacts of Ocean Acidification
Bach, Lennart Thomas
KOSMOS 2014 mesocosm study: The influence of plankton community structure on sinking velocity and remineralization rate of marine aggregates
topic_facet BIOACID
Biological Impacts of Ocean Acidification
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 of picophytoplankton to the total phytoplankton biomass. Cremin was highest during a Synechococcus bloom under oligotrophic conditions and in some mesocosms during the diatom bloom after the deep‐water addition while it was particularly low during harmful algal blooms. The temporal changes were considerably larger in Cremin (max. 15‐fold) than in SV (max. 3‐fold). Accordingly, estimated POC transfer efficiency to 1000 m was mainly dependent on how the plankton community structure affected Cremin. Our approach revealed key players and interactions in the plankton food web influencing POC export efficiency thereby improving our mechanistic understanding of the biological carbon pump.
format Dataset
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://doi.pangaea.de/10.1594/PANGAEA.902901
https://doi.org/10.1594/PANGAEA.902901
op_coverage LATITUDE: 27.928060 * LONGITUDE: -15.365280 * DATE/TIME START: 2014-09-27T00:00:00 * DATE/TIME END: 2015-10-18T00:00:00
long_lat ENVELOPE(-15.365280,-15.365280,27.928060,27.928060)
genre Ocean acidification
genre_facet Ocean acidification
op_source 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, https://doi.org/10.1029/2019GB006256
op_relation Taucher, Jan; Bach, Lennart Thomas (2018): KOSMOS 2014 mesocosm study: flow cytometry. PANGAEA, https://doi.org/10.1594/PANGAEA.889745
Taucher, Jan; Nauendorf, Alice (2018): KOSMOS 2014 mesocosm study: chlorophyll a. PANGAEA, https://doi.org/10.1594/PANGAEA.889731
Matlab script and test data for mesocosm model equation, Bach 2019 (URI: https://store.pangaea.de/Publications/Bach_2019/Bach-2019-Script.zip)
https://doi.pangaea.de/10.1594/PANGAEA.902901
https://doi.org/10.1594/PANGAEA.902901
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.902901
https://doi.org/10.1029/2019GB006256
https://doi.org/10.1594/PANGAEA.889745
https://doi.org/10.1594/PANGAEA.889731
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