Data from: In situ decrease in rhodolith growth associated with Arctic climate change

Rhodoliths built by crustose coralline algae (CCA) are ecosystem engineers of global importance. In the Arctic photic zone, their three-dimensional growth emulates the habitat complexity of coral reefs but with a far slower growth rate, growing at micrometres per year rather than millimetres. While...

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Main Authors: Teichert, Sebastian, Reddin, Carl, Wisshak, Max
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2024
Subjects:
Online Access:https://doi.org/10.5061/dryad.4j0zpc8m7
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spelling ftzenodo:oai:zenodo.org:11202141 2024-09-15T18:02:11+00:00 Data from: In situ decrease in rhodolith growth associated with Arctic climate change Teichert, Sebastian Reddin, Carl Wisshak, Max 2024-05-16 https://doi.org/10.5061/dryad.4j0zpc8m7 unknown Zenodo https://doi.org/10.5281/zenodo.10974678 https://doi.org/10.5281/zenodo.10974677 https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.4j0zpc8m7 oai:zenodo.org:11202141 info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode crustose coralline algae (CCA) ecosystem engineers Micro-computed tomography Global warming Calcification rhodoliths time series info:eu-repo/semantics/other 2024 ftzenodo https://doi.org/10.5061/dryad.4j0zpc8m710.5281/zenodo.1097467810.5281/zenodo.10974677 2024-07-25T12:46:53Z Rhodoliths built by crustose coralline algae (CCA) are ecosystem engineers of global importance. In the Arctic photic zone, their three-dimensional growth emulates the habitat complexity of coral reefs but with a far slower growth rate, growing at micrometres per year rather than millimetres. While climate change is known to exert various impacts on the CCA's calcite skeleton, including geochemical and structural alterations, field observations of net growth over decade-long timescales are lacking. Here, we use a temporally-explicit model to show that rising ocean temperatures over nearly 100 years were associated with reduced rhodolith growth at different depths in the Arctic. Over the past 90 years, the median growth rate was 85 µm yr -1 but each °C increase in summer seawater temperature decreased growth by a mean of 8.9 µm (95% CIs = 1.32 - 16.60 µm °C -1 , p < 0.05). The decrease was expressed for rhodolith occurrences in 11 and 27 m water depth but not at 46 m, also having the shortest time series (1991 – 2015). Although increasing temperatures can spur plant growth, we suggest anthropogenic climate change has either exceeded the population thermal optimum for these CCA, or synergistic effects of warming, ocean acidification, and/or increasing turbidity impair rhodolith growth. Rhodoliths built by calcitic CCA are important habitat providers worldwide, so decreased growth would lead to yet another facet of anthropogenic habitat loss. Funding provided by: Deutsche Forschungsgemeinschaft Crossref Funder Registry ID: https://ror.org/018mejw64 Award Number: Funding provided by: Dr. Hertha und Helmut Schmauser-Stiftung* Crossref Funder Registry ID: Award Number: Other/Unknown Material Climate change Global warming Ocean acidification Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic crustose coralline algae (CCA)
ecosystem engineers
Micro-computed tomography
Global warming
Calcification
rhodoliths
time series
spellingShingle crustose coralline algae (CCA)
ecosystem engineers
Micro-computed tomography
Global warming
Calcification
rhodoliths
time series
Teichert, Sebastian
Reddin, Carl
Wisshak, Max
Data from: In situ decrease in rhodolith growth associated with Arctic climate change
topic_facet crustose coralline algae (CCA)
ecosystem engineers
Micro-computed tomography
Global warming
Calcification
rhodoliths
time series
description Rhodoliths built by crustose coralline algae (CCA) are ecosystem engineers of global importance. In the Arctic photic zone, their three-dimensional growth emulates the habitat complexity of coral reefs but with a far slower growth rate, growing at micrometres per year rather than millimetres. While climate change is known to exert various impacts on the CCA's calcite skeleton, including geochemical and structural alterations, field observations of net growth over decade-long timescales are lacking. Here, we use a temporally-explicit model to show that rising ocean temperatures over nearly 100 years were associated with reduced rhodolith growth at different depths in the Arctic. Over the past 90 years, the median growth rate was 85 µm yr -1 but each °C increase in summer seawater temperature decreased growth by a mean of 8.9 µm (95% CIs = 1.32 - 16.60 µm °C -1 , p < 0.05). The decrease was expressed for rhodolith occurrences in 11 and 27 m water depth but not at 46 m, also having the shortest time series (1991 – 2015). Although increasing temperatures can spur plant growth, we suggest anthropogenic climate change has either exceeded the population thermal optimum for these CCA, or synergistic effects of warming, ocean acidification, and/or increasing turbidity impair rhodolith growth. Rhodoliths built by calcitic CCA are important habitat providers worldwide, so decreased growth would lead to yet another facet of anthropogenic habitat loss. Funding provided by: Deutsche Forschungsgemeinschaft Crossref Funder Registry ID: https://ror.org/018mejw64 Award Number: Funding provided by: Dr. Hertha und Helmut Schmauser-Stiftung* Crossref Funder Registry ID: Award Number:
format Other/Unknown Material
author Teichert, Sebastian
Reddin, Carl
Wisshak, Max
author_facet Teichert, Sebastian
Reddin, Carl
Wisshak, Max
author_sort Teichert, Sebastian
title Data from: In situ decrease in rhodolith growth associated with Arctic climate change
title_short Data from: In situ decrease in rhodolith growth associated with Arctic climate change
title_full Data from: In situ decrease in rhodolith growth associated with Arctic climate change
title_fullStr Data from: In situ decrease in rhodolith growth associated with Arctic climate change
title_full_unstemmed Data from: In situ decrease in rhodolith growth associated with Arctic climate change
title_sort data from: in situ decrease in rhodolith growth associated with arctic climate change
publisher Zenodo
publishDate 2024
url https://doi.org/10.5061/dryad.4j0zpc8m7
genre Climate change
Global warming
Ocean acidification
genre_facet Climate change
Global warming
Ocean acidification
op_relation https://doi.org/10.5281/zenodo.10974678
https://doi.org/10.5281/zenodo.10974677
https://zenodo.org/communities/dryad
https://doi.org/10.5061/dryad.4j0zpc8m7
oai:zenodo.org:11202141
op_rights info:eu-repo/semantics/openAccess
Creative Commons Zero v1.0 Universal
https://creativecommons.org/publicdomain/zero/1.0/legalcode
op_doi https://doi.org/10.5061/dryad.4j0zpc8m710.5281/zenodo.1097467810.5281/zenodo.10974677
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