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: Software
Language:unknown
Published: Zenodo 2024
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.10974676
https://zenodo.org/doi/10.5281/zenodo.10974676
id ftdatacite:10.5281/zenodo.10974676
record_format openpolar
spelling ftdatacite:10.5281/zenodo.10974676 2024-09-09T19:21:33+00:00 Data from: In situ decrease in rhodolith growth associated with Arctic climate change ... Teichert, Sebastian Reddin, Carl Wisshak, Max 2024 https://dx.doi.org/10.5281/zenodo.10974676 https://zenodo.org/doi/10.5281/zenodo.10974676 unknown Zenodo https://dx.doi.org/10.5061/dryad.4j0zpc8m7 https://dx.doi.org/10.5281/zenodo.10974678 MIT License https://opensource.org/licenses/MIT mit crustose coralline algae CCA ecosystem engineers Micro-computed tomography Global warming Calcification rhodoliths time series article Software SoftwareSourceCode 2024 ftdatacite https://doi.org/10.5281/zenodo.1097467610.5061/dryad.4j0zpc8m710.5281/zenodo.10974678 2024-06-17T09:57:42Z 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 ... : Funding provided by: Deutsche ForschungsgemeinschaftCrossref Funder Registry ID: https://ror.org/018mejw64Award Number: Funding provided by: Dr. Hertha und Helmut Schmauser-Stiftung*Crossref Funder Registry ID: Award Number: ... Software Arctic Climate change Global warming DataCite Arctic Hertha ENVELOPE(-60.033,-60.033,-65.167,-65.167)
institution Open Polar
collection DataCite
op_collection_id ftdatacite
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 ... : Funding provided by: Deutsche ForschungsgemeinschaftCrossref Funder Registry ID: https://ror.org/018mejw64Award Number: Funding provided by: Dr. Hertha und Helmut Schmauser-Stiftung*Crossref Funder Registry ID: Award Number: ...
format Software
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://dx.doi.org/10.5281/zenodo.10974676
https://zenodo.org/doi/10.5281/zenodo.10974676
long_lat ENVELOPE(-60.033,-60.033,-65.167,-65.167)
geographic Arctic
Hertha
geographic_facet Arctic
Hertha
genre Arctic
Climate change
Global warming
genre_facet Arctic
Climate change
Global warming
op_relation https://dx.doi.org/10.5061/dryad.4j0zpc8m7
https://dx.doi.org/10.5281/zenodo.10974678
op_rights MIT License
https://opensource.org/licenses/MIT
mit
op_doi https://doi.org/10.5281/zenodo.1097467610.5061/dryad.4j0zpc8m710.5281/zenodo.10974678
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