HR: 1340h
AN: B43E-1655 [Abstracts]
TI: Active Venting Sites On The Gas-Hydrate-Bearing Hikurangi Margin, Off New Zealand: ROV Measurements And Observations
AU: Naudts, L
EM: Lieven.Naudts@UGent.be
AF: Renard Centre of Marine Geology, Universiteit Gent, Krijgslaan 281, s8, Gent, B-9000,
Belgium
AU: Poort, J
EM: jeffrey_poort@yahoo.com
AF: Renard Centre of Marine Geology, Universiteit Gent, Krijgslaan 281, s8, Gent, B-9000,
Belgium
AU: Boone, D
EM: Dries.Boone@UGent.be
AF: Renard Centre of Marine Geology, Universiteit Gent, Krijgslaan 281, s8, Gent, B-9000,
Belgium
AU: Linke, P
EM: plinke@ifm-geomar.de
AF: Leibniz-Institut für Meereswissenschaften, Wischhofstrasse 1-3, Kiel, 24148, Germany
AU: Greinert, J
EM: Jens.Greinert@UGent.be
AF: Renard Centre of Marine Geology, Universiteit Gent, Krijgslaan 281, s8, Gent, B-9000,
Belgium
AU: * De Batist, M
EM: Marc.DeBatist@UGent.be
AF: Renard Centre of Marine Geology, Universiteit Gent, Krijgslaan 281, s8, Gent, B-9000,
Belgium
AU: Henriet, J
EM: jeanpierre.henriet@ugent.be
AF: Renard Centre of Marine Geology, Universiteit Gent, Krijgslaan 281, s8, Gent, B-9000,
Belgium
AB:
During R.V. Sonne cruise SO191-3, part of the "New (Zealand Cold) Vents" expedition, RCMG deployed a
CHEROKEE ROV "Genesis" on the Hikurangi Margin. This accretionary margin, on the east coast of New
Zealand, is related to the subduction of the Pacific Plate under the Australian Plate. Several cold vent locations as
well as an extensive BSR, indicating the presence of gas hydrates, have been found at this margin. The aims of
the ROV-work were to precisely localize active methane vents, to conduct detailed visual observations of the vent
structures and activity, and to perform measurements of physical properties and collect samples at and around
the vent locations. The three investigated areas generally have a flat to moderate undulating sea floor with soft
sediments alternating with carbonate platforms. The different sites were sometimes covered with dense fields of
live clams or shell debris, often in association with tube worms, sponges and/or soft tissue corals. Active bubble-
releasing seeps were observed at Faure's site and LM-3 site. Bubble-releasing activity was very variable in time,
with periods of almost non-activity alternating with periods of violent outbursts. Bubble release occurred mainly
from prominent depressions in soft-sediment sea floor. Bottom-water sampling revealed sometimes high
concentrations of methane. Sediment-temperature measurements were largely comparable with the bottom-
water temperature except for a "raindrop site" (with dense populations of polychaetes), where anomalous low
sediment-temperature was measured. Further analysis of the ROV data together with the integration of other
datasets will enable us to produce a model characterizing seep structure and environment.
DE: 0414 Biogeochemical cycles, processes, and modeling (0412, 0793, 1615, 4805, 4912)
DE: 0448 Geomicrobiology
DE: 0452 Instruments and techniques
DE: 0460 Marine systems (4800)
SC: Biogeosciences [B]
MN: 2007 Fall Meeting