The discovery of a natural whale fall in the Antarctic deep sea
The discovery of a natural whale fall in the Antarctic deep sea
Large cetacean carcasses at the deep-sea floor, known as ‘whale falls’, provide a resource for generalist-scavenging species, chemosynthetic fauna related to those from hydrothermal vents and cold seeps, and remarkable bone-specialist species such as Osedax worms. Here we report the serendipitous discovery of a late-stage natural whale fall at a depth of 1444 m in the South Sandwich Arc. This discovery represents the first natural whale fall to be encountered in the Southern Ocean, where cetaceans are abundant. The skeleton was situated within a seafloor caldera, in close proximity (<250 m) to active hydrothermal vents. We used a DNA barcoding approach to identify the skeleton as that of an Antarctic minke whale (Balaenoptera bonaerensis). The carcass was in an advanced state of decomposition, and its exposed bones were occupied by a diverse assemblage of fauna including nine undescribed species. These bone fauna included an undescribed species of Lepetodrilus limpet that was also present at the nearby hydrothermal vents, suggesting the use of whale-fall habitats as stepping stones between chemosynthetic ecosystems. Using Remotely Operated Vehicle (ROV) videography, we have quantified the composition and abundance of fauna on the whale bones, and tested a hypothesis that varying concentrations of lipids in the bones of whales may influence the microdistribution of sulfophilic whale-fall fauna. Our data supported the hypothesis that more lipid-rich bones support a greater abundance of sulfophilic bacterial mats, which are also correlated with the abundance of grazing limpets (Pyropelta sp.). The abundance of Osedax sp. on bones however, showed a negative correlation with the bacterial-mat percentage cover, and hence greatest abundance on bones predicted to have lowest lipid content.
Osedax, Whale bone, Lipid, Bacterial mat, Minke whale, Taphonomy
87-96
Amon, Diva J.
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Glover, Adrian G.
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Wiklund, Helena
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Marsh, Leigh
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Linse, Katrin
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Rogers, Alex D.
fb474198-f059-48f7-b637-74617b5023f6
Copley, Jonathan T.
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August 2013
Amon, Diva J.
b700d27b-4c13-484a-bad6-0be8f753b46d
Glover, Adrian G.
91192a3a-fc25-4c1f-b062-2e4da183272e
Wiklund, Helena
7c228af0-33a8-471f-b0f8-bc1e558cf8ed
Marsh, Leigh
b9d089aa-91e4-4a2e-b716-a7352616c6a2
Linse, Katrin
74d7ddc0-74a1-4777-ac1d-3f39ae1935ad
Rogers, Alex D.
fb474198-f059-48f7-b637-74617b5023f6
Copley, Jonathan T.
5f30e2a6-76c1-4150-9a42-dcfb8f5788ef
Amon, Diva J., Glover, Adrian G., Wiklund, Helena, Marsh, Leigh, Linse, Katrin, Rogers, Alex D. and Copley, Jonathan T.
(2013)
The discovery of a natural whale fall in the Antarctic deep sea.
Deep Sea Research Part II: Topical Studies in Oceanography, 92, .
(doi:10.1016/j.dsr2.2013.01.028).
Abstract
Large cetacean carcasses at the deep-sea floor, known as ‘whale falls’, provide a resource for generalist-scavenging species, chemosynthetic fauna related to those from hydrothermal vents and cold seeps, and remarkable bone-specialist species such as Osedax worms. Here we report the serendipitous discovery of a late-stage natural whale fall at a depth of 1444 m in the South Sandwich Arc. This discovery represents the first natural whale fall to be encountered in the Southern Ocean, where cetaceans are abundant. The skeleton was situated within a seafloor caldera, in close proximity (<250 m) to active hydrothermal vents. We used a DNA barcoding approach to identify the skeleton as that of an Antarctic minke whale (Balaenoptera bonaerensis). The carcass was in an advanced state of decomposition, and its exposed bones were occupied by a diverse assemblage of fauna including nine undescribed species. These bone fauna included an undescribed species of Lepetodrilus limpet that was also present at the nearby hydrothermal vents, suggesting the use of whale-fall habitats as stepping stones between chemosynthetic ecosystems. Using Remotely Operated Vehicle (ROV) videography, we have quantified the composition and abundance of fauna on the whale bones, and tested a hypothesis that varying concentrations of lipids in the bones of whales may influence the microdistribution of sulfophilic whale-fall fauna. Our data supported the hypothesis that more lipid-rich bones support a greater abundance of sulfophilic bacterial mats, which are also correlated with the abundance of grazing limpets (Pyropelta sp.). The abundance of Osedax sp. on bones however, showed a negative correlation with the bacterial-mat percentage cover, and hence greatest abundance on bones predicted to have lowest lipid content.
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Published date: August 2013
Keywords:
Osedax, Whale bone, Lipid, Bacterial mat, Minke whale, Taphonomy
Organisations:
Ocean Biochemistry & Ecosystems
Identifiers
Local EPrints ID: 350099
URI: http://eprints.soton.ac.uk/id/eprint/350099
ISSN: 0967-0645
PURE UUID: 55d6b7ff-939b-4afe-8f09-ead27fa4b8a0
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Date deposited: 18 Mar 2013 13:04
Last modified: 15 Mar 2024 02:48
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Contributors
Author:
Diva J. Amon
Author:
Adrian G. Glover
Author:
Helena Wiklund
Author:
Katrin Linse
Author:
Alex D. Rogers
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