A new species of the cheilostome bryozoan Chiastosella in the Southern Ocean, past and present

Understanding whether marine calcifying organisms may acclimatise to climate change is important with regard to their survival over the coming century. Due to cold waters having a naturally higher CO2 uptake, the Southern Ocean provides an especially good opportunity to study the potential impact of...

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Published in:Polar Biology
Main Authors: Ragazzola, F., Taylor, P., Bazzicalupo, P., Okamura, B., Schmidt, D.
Format: Book
Language:English
Published: 2014
Subjects:
Online Access:http://hdl.handle.net/1834/17093
https://doi.org/10.1007/s00300-014-1478-x
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spelling ftoceandocs:oai:aquadocs.org:1834/17093 2024-06-09T07:49:42+00:00 A new species of the cheilostome bryozoan Chiastosella in the Southern Ocean, past and present Ragazzola, F. Taylor, P. Bazzicalupo, P. Okamura, B. Schmidt, D. 2014 pp.773-779 http://hdl.handle.net/1834/17093 https://doi.org/10.1007/s00300-014-1478-x en eng https://doi.org/10.1007/s00300-014-1478-x http://hdl.handle.net/1834/17093 Journal Contribution Refereed 2014 ftoceandocs https://doi.org/10.1007/s00300-014-1478-x 2024-05-15T08:02:16Z Understanding whether marine calcifying organisms may acclimatise to climate change is important with regard to their survival over the coming century. Due to cold waters having a naturally higher CO2 uptake, the Southern Ocean provides an especially good opportunity to study the potential impact of climate change. In 2011, a new cheilostome bryozoan species-Chiastosella ettorina sp. nov.-was dredged from Burdwood Bank, Southern Ocean, at 324-219-m depth during the Nathaniel B Palmer Cruise. This species had previously been collected in 1902 from the same area at 100-m depth, but was incorrectly identified as Chiastosella watersi, an encrusting species from New Zealand. The availability of samples of the same species, from the same general location, but collected 109 years apart allowed us to investigate morphological modifications potentially arising from environmental changes. We found a significant difference in zooid size, with the oldest and shallowest specimens having smaller zooids than the recently collected deeper specimens. This difference in zooid size appears to be unrelated to known sources of environmental variation such as temperature and salinity, and it could represent the extremes of the zooid size range of C. ettorina. An alternative explanation is that acidifying waters may have caused zooids to grow more slowly, resulting in a final larger size. Published Book Southern Ocean IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications Burdwood Bank ENVELOPE(-59.000,-59.000,-54.250,-54.250) New Zealand Southern Ocean Polar Biology 37 6 773 779
institution Open Polar
collection IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications
op_collection_id ftoceandocs
language English
description Understanding whether marine calcifying organisms may acclimatise to climate change is important with regard to their survival over the coming century. Due to cold waters having a naturally higher CO2 uptake, the Southern Ocean provides an especially good opportunity to study the potential impact of climate change. In 2011, a new cheilostome bryozoan species-Chiastosella ettorina sp. nov.-was dredged from Burdwood Bank, Southern Ocean, at 324-219-m depth during the Nathaniel B Palmer Cruise. This species had previously been collected in 1902 from the same area at 100-m depth, but was incorrectly identified as Chiastosella watersi, an encrusting species from New Zealand. The availability of samples of the same species, from the same general location, but collected 109 years apart allowed us to investigate morphological modifications potentially arising from environmental changes. We found a significant difference in zooid size, with the oldest and shallowest specimens having smaller zooids than the recently collected deeper specimens. This difference in zooid size appears to be unrelated to known sources of environmental variation such as temperature and salinity, and it could represent the extremes of the zooid size range of C. ettorina. An alternative explanation is that acidifying waters may have caused zooids to grow more slowly, resulting in a final larger size. Published
format Book
author Ragazzola, F.
Taylor, P.
Bazzicalupo, P.
Okamura, B.
Schmidt, D.
spellingShingle Ragazzola, F.
Taylor, P.
Bazzicalupo, P.
Okamura, B.
Schmidt, D.
A new species of the cheilostome bryozoan Chiastosella in the Southern Ocean, past and present
author_facet Ragazzola, F.
Taylor, P.
Bazzicalupo, P.
Okamura, B.
Schmidt, D.
author_sort Ragazzola, F.
title A new species of the cheilostome bryozoan Chiastosella in the Southern Ocean, past and present
title_short A new species of the cheilostome bryozoan Chiastosella in the Southern Ocean, past and present
title_full A new species of the cheilostome bryozoan Chiastosella in the Southern Ocean, past and present
title_fullStr A new species of the cheilostome bryozoan Chiastosella in the Southern Ocean, past and present
title_full_unstemmed A new species of the cheilostome bryozoan Chiastosella in the Southern Ocean, past and present
title_sort new species of the cheilostome bryozoan chiastosella in the southern ocean, past and present
publishDate 2014
url http://hdl.handle.net/1834/17093
https://doi.org/10.1007/s00300-014-1478-x
long_lat ENVELOPE(-59.000,-59.000,-54.250,-54.250)
geographic Burdwood Bank
New Zealand
Southern Ocean
geographic_facet Burdwood Bank
New Zealand
Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_relation https://doi.org/10.1007/s00300-014-1478-x
http://hdl.handle.net/1834/17093
op_doi https://doi.org/10.1007/s00300-014-1478-x
container_title Polar Biology
container_volume 37
container_issue 6
container_start_page 773
op_container_end_page 779
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