Dissolved organic matter molecular composition and concentrations from a large scale mesocosm study KOSMOS 2013 Kristineberg) on ocean acidification

Marine dissolved organic matter (DOM) represents one of the largest active carbon reservoirs on Earth. Changes in pool size or composition could have major impacts on the global carbon cycle. Ocean acidification is a potential driver for these changes because it influences marine primary production...

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Main Authors: Zark, Maren, Dittmar, Thorsten, Riebesell, Ulf
Format: Dataset
Language:English
Published: PANGAEA 2015
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.846137
https://doi.org/10.1594/PANGAEA.846137
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record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.846137 2023-05-15T17:49:31+02:00 Dissolved organic matter molecular composition and concentrations from a large scale mesocosm study KOSMOS 2013 Kristineberg) on ocean acidification Zark, Maren Dittmar, Thorsten Riebesell, Ulf MEDIAN LATITUDE: 58.266308 * MEDIAN LONGITUDE: 11.478532 * SOUTH-BOUND LATITUDE: 58.263889 * WEST-BOUND LONGITUDE: 11.477300 * NORTH-BOUND LATITUDE: 58.268800 * EAST-BOUND LONGITUDE: 11.479500 * DATE/TIME START: 2013-03-07T00:00:00 * DATE/TIME END: 2013-06-28T23:59:00 2015-05-11 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.846137 https://doi.org/10.1594/PANGAEA.846137 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.846137 https://doi.org/10.1594/PANGAEA.846137 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Zark, Maren; Riebesell, Ulf; Dittmar, Thorsten (2015): Effects of ocean acidification on marine dissolved organic matter are not detectable over the succession of phytoplankton blooms. Science Advances, 1(9), e1500531-e1500531, https://doi.org/10.1126/sciadv.1500531 BIOACID Biological Impacts of Ocean Acidification Dataset 2015 ftpangaea https://doi.org/10.1594/PANGAEA.846137 https://doi.org/10.1126/sciadv.1500531 2023-01-20T07:33:27Z Marine dissolved organic matter (DOM) represents one of the largest active carbon reservoirs on Earth. Changes in pool size or composition could have major impacts on the global carbon cycle. Ocean acidification is a potential driver for these changes because it influences marine primary production and heterotrophic respiration. Here we show that ocean acidification as expected for a 'business-as-usual' emission scenario in the year 2100 (900 µatm) does not affect the DOM pool with respect to its size and molecular composition. We applied ultrahigh-resolution mass spectrometry to monitor the production and turnover of 7,360 distinct molecular DOM features in an unprecedented long-term mesocosm study in a Swedish Fjord, covering a full cycle of marine production. DOM concentration and molecular composition did not differ significantly between present-day and year 2100 CO2 levels. Our findings are likely applicable to other coastal and productive marine ecosystems in general. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science Kristineberg ENVELOPE(18.667,18.667,79.483,79.483) ENVELOPE(11.477300,11.479500,58.268800,58.263889)
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
Zark, Maren
Dittmar, Thorsten
Riebesell, Ulf
Dissolved organic matter molecular composition and concentrations from a large scale mesocosm study KOSMOS 2013 Kristineberg) on ocean acidification
topic_facet BIOACID
Biological Impacts of Ocean Acidification
description Marine dissolved organic matter (DOM) represents one of the largest active carbon reservoirs on Earth. Changes in pool size or composition could have major impacts on the global carbon cycle. Ocean acidification is a potential driver for these changes because it influences marine primary production and heterotrophic respiration. Here we show that ocean acidification as expected for a 'business-as-usual' emission scenario in the year 2100 (900 µatm) does not affect the DOM pool with respect to its size and molecular composition. We applied ultrahigh-resolution mass spectrometry to monitor the production and turnover of 7,360 distinct molecular DOM features in an unprecedented long-term mesocosm study in a Swedish Fjord, covering a full cycle of marine production. DOM concentration and molecular composition did not differ significantly between present-day and year 2100 CO2 levels. Our findings are likely applicable to other coastal and productive marine ecosystems in general.
format Dataset
author Zark, Maren
Dittmar, Thorsten
Riebesell, Ulf
author_facet Zark, Maren
Dittmar, Thorsten
Riebesell, Ulf
author_sort Zark, Maren
title Dissolved organic matter molecular composition and concentrations from a large scale mesocosm study KOSMOS 2013 Kristineberg) on ocean acidification
title_short Dissolved organic matter molecular composition and concentrations from a large scale mesocosm study KOSMOS 2013 Kristineberg) on ocean acidification
title_full Dissolved organic matter molecular composition and concentrations from a large scale mesocosm study KOSMOS 2013 Kristineberg) on ocean acidification
title_fullStr Dissolved organic matter molecular composition and concentrations from a large scale mesocosm study KOSMOS 2013 Kristineberg) on ocean acidification
title_full_unstemmed Dissolved organic matter molecular composition and concentrations from a large scale mesocosm study KOSMOS 2013 Kristineberg) on ocean acidification
title_sort dissolved organic matter molecular composition and concentrations from a large scale mesocosm study kosmos 2013 kristineberg) on ocean acidification
publisher PANGAEA
publishDate 2015
url https://doi.pangaea.de/10.1594/PANGAEA.846137
https://doi.org/10.1594/PANGAEA.846137
op_coverage MEDIAN LATITUDE: 58.266308 * MEDIAN LONGITUDE: 11.478532 * SOUTH-BOUND LATITUDE: 58.263889 * WEST-BOUND LONGITUDE: 11.477300 * NORTH-BOUND LATITUDE: 58.268800 * EAST-BOUND LONGITUDE: 11.479500 * DATE/TIME START: 2013-03-07T00:00:00 * DATE/TIME END: 2013-06-28T23:59:00
long_lat ENVELOPE(18.667,18.667,79.483,79.483)
ENVELOPE(11.477300,11.479500,58.268800,58.263889)
geographic Kristineberg
geographic_facet Kristineberg
genre Ocean acidification
genre_facet Ocean acidification
op_source Supplement to: Zark, Maren; Riebesell, Ulf; Dittmar, Thorsten (2015): Effects of ocean acidification on marine dissolved organic matter are not detectable over the succession of phytoplankton blooms. Science Advances, 1(9), e1500531-e1500531, https://doi.org/10.1126/sciadv.1500531
op_relation https://doi.pangaea.de/10.1594/PANGAEA.846137
https://doi.org/10.1594/PANGAEA.846137
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.846137
https://doi.org/10.1126/sciadv.1500531
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