Effects of Ocean Acidification on the Ballast of Surface Aggregates Sinking through the Twilight Zone: organic and inorganic carbon content ...

Incubation Setup The aggregates were placed inside the settling microcosm. The microcosm was filled with GF/F filtered, artificial seawater (32 psu) with a carbonate chemistry adjusted to the present or future conditions. This reduced the biological activity to the community originally present in th...

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Bibliographic Details
Main Authors: Mendes, Pedro André, Thomsen, Laurenz
Format: Dataset
Language:English
Published: PANGAEA 2015
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.846488
https://doi.pangaea.de/10.1594/PANGAEA.846488
id ftdatacite:10.1594/pangaea.846488
record_format openpolar
spelling ftdatacite:10.1594/pangaea.846488 2024-09-15T18:27:53+00:00 Effects of Ocean Acidification on the Ballast of Surface Aggregates Sinking through the Twilight Zone: organic and inorganic carbon content ... Mendes, Pedro André Thomsen, Laurenz 2015 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.846488 https://doi.pangaea.de/10.1594/PANGAEA.846488 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.846489 https://dx.doi.org/10.1371/journal.pone.0050865 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Experimental treatment Carbon dioxide, partial pressure Sample code/label Carbon, organic, particulate Standard deviation Carbon, inorganic, particulate Biological Impacts of Ocean Acidification BIOACID dataset Dataset 2015 ftdatacite https://doi.org/10.1594/pangaea.84648810.1594/pangaea.84648910.1371/journal.pone.0050865 2024-08-01T10:56:44Z Incubation Setup The aggregates were placed inside the settling microcosm. The microcosm was filled with GF/F filtered, artificial seawater (32 psu) with a carbonate chemistry adjusted to the present or future conditions. This reduced the biological activity to the community originally present in the aggregates. The microcosm was continuously pressurized at a rate of 30 MPa/day, until it reached 10 MPa, the equivalent to a depth of 1000 m. The full incubation lasted 80 h. The experiment was triplicated at a pCO2 of 380 µatm and 1100 µatm. Additional incubations of similar duration were done at atmospheric pressure, with triplicates at a pCO2 of 380 µatm and 1100 µatm. These aimed at isolating the effect of the increase in hydrostatic pressure. Determination of Organic and Inorganic Carbon Content Aggregate samples were concentrated onto precombusted Whatman GF/F glass filters and analyzed for organic carbon. The filters were dried at 60°C overnight. After weighting, a section of each filter was placed into a ... Dataset Ocean acidification DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Experimental treatment
Carbon dioxide, partial pressure
Sample code/label
Carbon, organic, particulate
Standard deviation
Carbon, inorganic, particulate
Biological Impacts of Ocean Acidification BIOACID
spellingShingle Experimental treatment
Carbon dioxide, partial pressure
Sample code/label
Carbon, organic, particulate
Standard deviation
Carbon, inorganic, particulate
Biological Impacts of Ocean Acidification BIOACID
Mendes, Pedro André
Thomsen, Laurenz
Effects of Ocean Acidification on the Ballast of Surface Aggregates Sinking through the Twilight Zone: organic and inorganic carbon content ...
topic_facet Experimental treatment
Carbon dioxide, partial pressure
Sample code/label
Carbon, organic, particulate
Standard deviation
Carbon, inorganic, particulate
Biological Impacts of Ocean Acidification BIOACID
description Incubation Setup The aggregates were placed inside the settling microcosm. The microcosm was filled with GF/F filtered, artificial seawater (32 psu) with a carbonate chemistry adjusted to the present or future conditions. This reduced the biological activity to the community originally present in the aggregates. The microcosm was continuously pressurized at a rate of 30 MPa/day, until it reached 10 MPa, the equivalent to a depth of 1000 m. The full incubation lasted 80 h. The experiment was triplicated at a pCO2 of 380 µatm and 1100 µatm. Additional incubations of similar duration were done at atmospheric pressure, with triplicates at a pCO2 of 380 µatm and 1100 µatm. These aimed at isolating the effect of the increase in hydrostatic pressure. Determination of Organic and Inorganic Carbon Content Aggregate samples were concentrated onto precombusted Whatman GF/F glass filters and analyzed for organic carbon. The filters were dried at 60°C overnight. After weighting, a section of each filter was placed into a ...
format Dataset
author Mendes, Pedro André
Thomsen, Laurenz
author_facet Mendes, Pedro André
Thomsen, Laurenz
author_sort Mendes, Pedro André
title Effects of Ocean Acidification on the Ballast of Surface Aggregates Sinking through the Twilight Zone: organic and inorganic carbon content ...
title_short Effects of Ocean Acidification on the Ballast of Surface Aggregates Sinking through the Twilight Zone: organic and inorganic carbon content ...
title_full Effects of Ocean Acidification on the Ballast of Surface Aggregates Sinking through the Twilight Zone: organic and inorganic carbon content ...
title_fullStr Effects of Ocean Acidification on the Ballast of Surface Aggregates Sinking through the Twilight Zone: organic and inorganic carbon content ...
title_full_unstemmed Effects of Ocean Acidification on the Ballast of Surface Aggregates Sinking through the Twilight Zone: organic and inorganic carbon content ...
title_sort effects of ocean acidification on the ballast of surface aggregates sinking through the twilight zone: organic and inorganic carbon content ...
publisher PANGAEA
publishDate 2015
url https://dx.doi.org/10.1594/pangaea.846488
https://doi.pangaea.de/10.1594/PANGAEA.846488
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://dx.doi.org/10.1594/pangaea.846489
https://dx.doi.org/10.1371/journal.pone.0050865
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.84648810.1594/pangaea.84648910.1371/journal.pone.0050865
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