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Vailulu'u seamount, Samoa: life and death on an active submarine volcano 2006

Vailulu'u seamount, Samoa: life and death on an active submarine volcano 2006
Vailulu'u seamount, Samoa: life and death on an active submarine volcano 2006
Submersible exploration of the Samoan hotspot revealed a new, 300-m-tall, volcanic cone, named Nafanua, in the summit crater of Vailulu’u seamount. Nafanua grew from the 1,000-m-deep crater floor in <4 years and could reach the sea surface within decades. Vents fill Vailulu’u crater with a thick suspension of particulates and apparently toxic fluids that mix with seawater entering from the crater breaches. Low-temperature vents form Fe oxide chimneys in many locations and up to 1-m-thick layers of hydrothermal Fe floc on Nafanua. High-temperature (81°C) hydrothermal vents in the northern moat (945-m water depth) produce acidic fluids (pH 2.7) with rising droplets of (probably) liquid CO2. The Nafanua summit vent area is inhabited by a thriving population of eels (Dysommina rugosa) that feed on midwater shrimp probably concentrated by anticyclonic currents at the volcano summit and rim. The moat and crater floor around the new volcano are littered with dead metazoans that apparently died from exposure to hydrothermal emissions. Acid-tolerant polychaetes (Polynoidae) live in this environment, apparently feeding on bacteria from decaying fish carcasses. Vailulu’u is an unpredictable and very active underwater volcano presenting a potential long-term volcanic hazard. Although eels thrive in hydrothermal vents at the summit of Nafanua, venting elsewhere in the crater causes mass mortality. Paradoxically, the same anticyclonic currents that deliver food to the eels may also concentrate a wide variety of nektonic animals in a death trap of toxic hydrothermal fluids.
currents, habitats, hydrothermal vents, eels
0027-8424
6448-6453
Staudigel, H.
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Hart, S.R.
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Pile, A.
87c26b72-f1af-419a-a2de-b58a3d52528d
Bailey, B.E.
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Baker, E.T.
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Brooke, S.
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Connelly, D.P.
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Haucke, L.
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German, C.R.
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Hudson, I.
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Jones, D.
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Koppers, A.A.P.
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Konter, J.
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Lee, R.
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Pietsch, T.W.
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Tebo, B.M.
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Templeton, A.S.
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Zierenberg, R.
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Young, C.M.
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Staudigel, H.
04c901b5-f5ea-4ecc-8097-3fe123314f4f
Hart, S.R.
016d0d77-3053-4d4a-9502-599b03ade351
Pile, A.
87c26b72-f1af-419a-a2de-b58a3d52528d
Bailey, B.E.
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Baker, E.T.
0153c7ce-335a-42ed-ba5a-1f3274263712
Brooke, S.
b3a60e34-2ebf-42ad-8cbe-3f197b78b34c
Connelly, D.P.
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Haucke, L.
c3966175-7a3d-496e-a736-8bca99e52861
German, C.R.
cd0eedd5-1377-4182-9c8a-b06aef8c1069
Hudson, I.
cf9dd6b8-ad1b-494c-9927-1016faac307c
Jones, D.
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Koppers, A.A.P.
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Konter, J.
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Lee, R.
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Pietsch, T.W.
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Tebo, B.M.
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Templeton, A.S.
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Zierenberg, R.
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Young, C.M.
0c561acc-0a69-4fd7-9457-08523d2e00b2

Staudigel, H., Hart, S.R., Pile, A., Bailey, B.E., Baker, E.T., Brooke, S., Connelly, D.P., Haucke, L., German, C.R., Hudson, I., Jones, D., Koppers, A.A.P., Konter, J., Lee, R., Pietsch, T.W., Tebo, B.M., Templeton, A.S., Zierenberg, R. and Young, C.M. (2006) Vailulu'u seamount, Samoa: life and death on an active submarine volcano 2006. Proceedings of the National Academy of Sciences of the United States of America, 103 (17), 6448-6453. (doi:10.1073/pnas.0600830103).

Record type: Article

Abstract

Submersible exploration of the Samoan hotspot revealed a new, 300-m-tall, volcanic cone, named Nafanua, in the summit crater of Vailulu’u seamount. Nafanua grew from the 1,000-m-deep crater floor in <4 years and could reach the sea surface within decades. Vents fill Vailulu’u crater with a thick suspension of particulates and apparently toxic fluids that mix with seawater entering from the crater breaches. Low-temperature vents form Fe oxide chimneys in many locations and up to 1-m-thick layers of hydrothermal Fe floc on Nafanua. High-temperature (81°C) hydrothermal vents in the northern moat (945-m water depth) produce acidic fluids (pH 2.7) with rising droplets of (probably) liquid CO2. The Nafanua summit vent area is inhabited by a thriving population of eels (Dysommina rugosa) that feed on midwater shrimp probably concentrated by anticyclonic currents at the volcano summit and rim. The moat and crater floor around the new volcano are littered with dead metazoans that apparently died from exposure to hydrothermal emissions. Acid-tolerant polychaetes (Polynoidae) live in this environment, apparently feeding on bacteria from decaying fish carcasses. Vailulu’u is an unpredictable and very active underwater volcano presenting a potential long-term volcanic hazard. Although eels thrive in hydrothermal vents at the summit of Nafanua, venting elsewhere in the crater causes mass mortality. Paradoxically, the same anticyclonic currents that deliver food to the eels may also concentrate a wide variety of nektonic animals in a death trap of toxic hydrothermal fluids.

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More information

Published date: 2006
Keywords: currents, habitats, hydrothermal vents, eels
Organisations: National Oceanography Centre,Southampton

Identifiers

Local EPrints ID: 43831
URI: http://eprints.soton.ac.uk/id/eprint/43831
ISSN: 0027-8424
PURE UUID: 2ac65307-ea76-4e07-bf85-6bf403e76cf1

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Date deposited: 30 Jan 2007
Last modified: 15 Mar 2024 08:58

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Contributors

Author: H. Staudigel
Author: S.R. Hart
Author: A. Pile
Author: B.E. Bailey
Author: E.T. Baker
Author: S. Brooke
Author: D.P. Connelly
Author: L. Haucke
Author: C.R. German
Author: I. Hudson
Author: D. Jones
Author: A.A.P. Koppers
Author: J. Konter
Author: R. Lee
Author: T.W. Pietsch
Author: B.M. Tebo
Author: A.S. Templeton
Author: R. Zierenberg
Author: C.M. Young

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