High abundance of the epibenthic trachymedusa Ptychogastria polaris Allman, 1878 (Hydrozoa, Trachylina) in subpolar fjords along the West Antarctic Peninsula
High abundance of the epibenthic trachymedusa Ptychogastria polaris Allman, 1878 (Hydrozoa, Trachylina) in subpolar fjords along the West Antarctic Peninsula
Medusae can be conspicuous and abundant members of seafloor communities in deep-sea benthic boundary layers. The epibenthic trachymedusa, Ptychogastria polaris Allman, 1878 (Hydrozoa: Trachylina: Ptychogastriidae) occurs in the cold, high latitude systems of both the northern and southern hemispheres, with a circumpolar distribution in Arctic and sub-Arctic areas, and disjunct reports of a few individuals from Antarctica. In January-February 2010, during benthic megafaunal photosurveys in three subpolar fjords along the West Antarctic Peninsula (Andvord, Flandres and Barilari Bays), P. polaris was recorded in Antarctic Peninsula waters. The trachymedusa, identified from megacore-collected specimens, was a common component of the epifauna in the sediment floored basins at 436–725 m depths in Andvord and Flandres Bays, reaching densities up to 13 m-2, with mean densities in individual basins ranging from 0.06 to 4.19 m-2. These densities are 2 to 400-fold higher than previously reported for P. polaris in either the Arctic or Antarctic. This trachymedusa had an aggregated distribution, occurring frequently in Andvord Bay, but was often solitary in Flandres Bay, with a distribution not significantly different from random. Epibenthic individuals were similar in size, typically measuring 15–25 mm in bell diameter. A morphologically similar trachymedusa, presumably the same species, was also observed in the water column near the bottom in all three fjords. This benthopelagic form attained abundances of up to 7 m-2 of seafloor; however, most P. polaris (~ 80%), were observed on soft sediments. Our findings indicate that fjords provide a prime habitat for the development of dense populations of P. polaris, potentially resulting from high and varied food inputs to the fjord floors. Because P. polaris resides in the water column and at the seafloor, large P. polaris populations may contribute significantly to pelagic-benthic coupling in the WAP fjord ecosystems.
e0168648
Grange, Laura L.
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Smith, Craig R.
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Lindsay, Dhugal J.
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Bentlage, Bastian
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Youngbluth, Marsh J.
bf281f23-8b49-4b9a-a37e-f26b5fb5530e
4 January 2017
Grange, Laura L.
8de65684-8e14-4cc2-89d1-ca20322714e4
Smith, Craig R.
f930361f-9312-4e0a-9832-26008197eb32
Lindsay, Dhugal J.
fb535271-7a69-491f-8a16-34601eced9a7
Bentlage, Bastian
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Youngbluth, Marsh J.
bf281f23-8b49-4b9a-a37e-f26b5fb5530e
Grange, Laura L., Smith, Craig R., Lindsay, Dhugal J., Bentlage, Bastian and Youngbluth, Marsh J.
(2017)
High abundance of the epibenthic trachymedusa Ptychogastria polaris Allman, 1878 (Hydrozoa, Trachylina) in subpolar fjords along the West Antarctic Peninsula.
PLoS ONE, 12 (1), .
(doi:10.1371/journal.pone.0168648).
Abstract
Medusae can be conspicuous and abundant members of seafloor communities in deep-sea benthic boundary layers. The epibenthic trachymedusa, Ptychogastria polaris Allman, 1878 (Hydrozoa: Trachylina: Ptychogastriidae) occurs in the cold, high latitude systems of both the northern and southern hemispheres, with a circumpolar distribution in Arctic and sub-Arctic areas, and disjunct reports of a few individuals from Antarctica. In January-February 2010, during benthic megafaunal photosurveys in three subpolar fjords along the West Antarctic Peninsula (Andvord, Flandres and Barilari Bays), P. polaris was recorded in Antarctic Peninsula waters. The trachymedusa, identified from megacore-collected specimens, was a common component of the epifauna in the sediment floored basins at 436–725 m depths in Andvord and Flandres Bays, reaching densities up to 13 m-2, with mean densities in individual basins ranging from 0.06 to 4.19 m-2. These densities are 2 to 400-fold higher than previously reported for P. polaris in either the Arctic or Antarctic. This trachymedusa had an aggregated distribution, occurring frequently in Andvord Bay, but was often solitary in Flandres Bay, with a distribution not significantly different from random. Epibenthic individuals were similar in size, typically measuring 15–25 mm in bell diameter. A morphologically similar trachymedusa, presumably the same species, was also observed in the water column near the bottom in all three fjords. This benthopelagic form attained abundances of up to 7 m-2 of seafloor; however, most P. polaris (~ 80%), were observed on soft sediments. Our findings indicate that fjords provide a prime habitat for the development of dense populations of P. polaris, potentially resulting from high and varied food inputs to the fjord floors. Because P. polaris resides in the water column and at the seafloor, large P. polaris populations may contribute significantly to pelagic-benthic coupling in the WAP fjord ecosystems.
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Accepted/In Press date: 4 December 2016
e-pub ahead of print date: 4 January 2017
Published date: 4 January 2017
Organisations:
Ocean and Earth Science
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Local EPrints ID: 404553
URI: http://eprints.soton.ac.uk/id/eprint/404553
ISSN: 1932-6203
PURE UUID: a971a6f8-0dca-4b46-9a28-a3b9e2507c90
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Date deposited: 11 Jan 2017 09:35
Last modified: 15 Mar 2024 04:09
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Author:
Craig R. Smith
Author:
Dhugal J. Lindsay
Author:
Bastian Bentlage
Author:
Marsh J. Youngbluth
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