Iceberg killing fields limit huge potential for benthic blue carbon in Antarctic shallows

Abstract Climate‐forced ice losses are increasing potential for iceberg‐seabed collisions, termed ice scour. At Ryder Bay, West Antarctic Peninsula ( WAP ) sea ice, oceanography, phytoplankton and encrusting zoobenthos have been monitored since 1998. In 2003, grids of seabed markers, covering 225 m...

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Published in:Global Change Biology
Main Author: Barnes, David K. A.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2016
Subjects:
Online Access:http://dx.doi.org/10.1111/gcb.13523
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fgcb.13523
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spelling crwiley:10.1111/gcb.13523 2024-10-13T14:03:08+00:00 Iceberg killing fields limit huge potential for benthic blue carbon in Antarctic shallows Barnes, David K. A. 2016 http://dx.doi.org/10.1111/gcb.13523 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fgcb.13523 https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.13523 en eng Wiley http://creativecommons.org/licenses/by-nc-nd/4.0/ Global Change Biology volume 23, issue 7, page 2649-2659 ISSN 1354-1013 1365-2486 journal-article 2016 crwiley https://doi.org/10.1111/gcb.13523 2024-09-17T04:51:14Z Abstract Climate‐forced ice losses are increasing potential for iceberg‐seabed collisions, termed ice scour. At Ryder Bay, West Antarctic Peninsula ( WAP ) sea ice, oceanography, phytoplankton and encrusting zoobenthos have been monitored since 1998. In 2003, grids of seabed markers, covering 225 m 2 , were established, surveyed and replaced annually to measure ice scour frequency. Disturbance history has been recorded for each m 2 of seabed monitored at 5–25 m for ~13 years. Encrusting fauna, collected from impacted and nonimpacted metres each year, show coincident benthos responses in growth, mortality and mass of benthic immobilized carbon. Encrusting benthic growth was mainly determined by microalgal bloom duration; each day, nanophytoplankton exceeded 200 μg L −1 produced ~0.05 mm radial growth of bryozoans, and sea temperature >0 °C added 0.002 mm day −1 . Mortality and persistence of growth, as benthic carbon immobilization, were mainly influenced by ice scour. Nearly 30% of monitored seabed was hit each year, and just 7% of shallows were not hit. Hits in deeper water were more deadly, but less frequent, so mortality decreased with depth. Five‐year recovery time doubled benthic carbon stocks. Scour‐driven mortality varied annually, with two‐thirds of all monitored fauna killed in a single year (2009). Reduced fast ice after 2006 ramped iceberg scouring, killing half the encrusting benthos each year in following years. Ice scour coupled with low phytoplankton biomass drove a phase shift to high mortality and depressed zoobenthic immobilized carbon stocks, which has persevered for 10 years since. Stocks of immobilized benthic carbon averaged nearly 15 g m −2 . WAP ice scouring may be recycling 80 000 tonnes of carbon yr −1 . Without scouring, such carbon would remain immobilized and the 2.3% of shelf which are shallows could be as productive as all the remaining continental shelf. The region's future, when glaciers reach grounding lines and iceberg production diminishes, is as a major global sink of ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Iceberg* Sea ice Wiley Online Library Antarctic Antarctic Peninsula Ryder ENVELOPE(-68.333,-68.333,-67.566,-67.566) Ryder Bay ENVELOPE(-68.333,-68.333,-67.567,-67.567) Global Change Biology 23 7 2649 2659
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Climate‐forced ice losses are increasing potential for iceberg‐seabed collisions, termed ice scour. At Ryder Bay, West Antarctic Peninsula ( WAP ) sea ice, oceanography, phytoplankton and encrusting zoobenthos have been monitored since 1998. In 2003, grids of seabed markers, covering 225 m 2 , were established, surveyed and replaced annually to measure ice scour frequency. Disturbance history has been recorded for each m 2 of seabed monitored at 5–25 m for ~13 years. Encrusting fauna, collected from impacted and nonimpacted metres each year, show coincident benthos responses in growth, mortality and mass of benthic immobilized carbon. Encrusting benthic growth was mainly determined by microalgal bloom duration; each day, nanophytoplankton exceeded 200 μg L −1 produced ~0.05 mm radial growth of bryozoans, and sea temperature >0 °C added 0.002 mm day −1 . Mortality and persistence of growth, as benthic carbon immobilization, were mainly influenced by ice scour. Nearly 30% of monitored seabed was hit each year, and just 7% of shallows were not hit. Hits in deeper water were more deadly, but less frequent, so mortality decreased with depth. Five‐year recovery time doubled benthic carbon stocks. Scour‐driven mortality varied annually, with two‐thirds of all monitored fauna killed in a single year (2009). Reduced fast ice after 2006 ramped iceberg scouring, killing half the encrusting benthos each year in following years. Ice scour coupled with low phytoplankton biomass drove a phase shift to high mortality and depressed zoobenthic immobilized carbon stocks, which has persevered for 10 years since. Stocks of immobilized benthic carbon averaged nearly 15 g m −2 . WAP ice scouring may be recycling 80 000 tonnes of carbon yr −1 . Without scouring, such carbon would remain immobilized and the 2.3% of shelf which are shallows could be as productive as all the remaining continental shelf. The region's future, when glaciers reach grounding lines and iceberg production diminishes, is as a major global sink of ...
format Article in Journal/Newspaper
author Barnes, David K. A.
spellingShingle Barnes, David K. A.
Iceberg killing fields limit huge potential for benthic blue carbon in Antarctic shallows
author_facet Barnes, David K. A.
author_sort Barnes, David K. A.
title Iceberg killing fields limit huge potential for benthic blue carbon in Antarctic shallows
title_short Iceberg killing fields limit huge potential for benthic blue carbon in Antarctic shallows
title_full Iceberg killing fields limit huge potential for benthic blue carbon in Antarctic shallows
title_fullStr Iceberg killing fields limit huge potential for benthic blue carbon in Antarctic shallows
title_full_unstemmed Iceberg killing fields limit huge potential for benthic blue carbon in Antarctic shallows
title_sort iceberg killing fields limit huge potential for benthic blue carbon in antarctic shallows
publisher Wiley
publishDate 2016
url http://dx.doi.org/10.1111/gcb.13523
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fgcb.13523
https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.13523
long_lat ENVELOPE(-68.333,-68.333,-67.566,-67.566)
ENVELOPE(-68.333,-68.333,-67.567,-67.567)
geographic Antarctic
Antarctic Peninsula
Ryder
Ryder Bay
geographic_facet Antarctic
Antarctic Peninsula
Ryder
Ryder Bay
genre Antarc*
Antarctic
Antarctic Peninsula
Iceberg*
Sea ice
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Iceberg*
Sea ice
op_source Global Change Biology
volume 23, issue 7, page 2649-2659
ISSN 1354-1013 1365-2486
op_rights http://creativecommons.org/licenses/by-nc-nd/4.0/
op_doi https://doi.org/10.1111/gcb.13523
container_title Global Change Biology
container_volume 23
container_issue 7
container_start_page 2649
op_container_end_page 2659
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