Authors / CoAuthors
Brooke, B.P. | McArthur, M.A. | Woodroffe, C.D. | Linklater, M. | Nichol, S.L. | Anderson, T.A. | Mleczko, R. | Sagar, S.
Abstract
Lord Howe Island in the southwest Pacific Ocean is the subaerial remnant of a Late Miocene hot-spot volcano. Erosion of the island has formed a shallow (20 - 120 m) sub-tropical carbonate shelf 24 km wide and 36 km long. On the mid shelf an extensive relict coral reef (165 km2) surrounds the island in water depths of 30-40 m. The relict reef comprises sand sheet, macroalgae and hardground habitats. Inboard of the relict reef a sandy basin (mean water depth 45 m) has thick sand deposits. Outboard of the relict reef is a relatively flat outer shelf (mean depth 60 m) with bedrock exposures and sandy habitat. Infauna species abundance and richness were similar for sediment samples collected on the outer shelf and relict reef features, while samples from the sandy basin had significantly lower infauna abundance and richness. The irregular shelf morphology appears to determine the distribution and character of sandy substrates and local oceanographic conditions, which in turn influence the distribution of different types of infauna communities.
Product Type
nonGeographicDataset
eCat Id
70977
Contact for the resource
Custodian
Point of contact
Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
Canberra
ACT
2601
Australia
Keywords
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- External PublicationAtlas
- ( Theme )
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- marine biodiversity
- ( Theme )
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- marine survey
- ( Theme )
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- geomorphology
- ( Theme )
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- sedimentology
- ( Theme )
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- bathymetry
- ( Theme )
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- marine
- Australian and New Zealand Standard Research Classification (ANZSRC)
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- Earth Sciences
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- Published_Internal
Publication Date
2010-09-08T00:00:00
Creation Date
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Status
Purpose
Maintenance Information
unknown
Topic Category
geoscientificInformation
Series Information
Lineage
Unknown
Parent Information
Extents
[-33.0, -31.0, 158.0, 160.0]
Reference System
Spatial Resolution
Service Information
Associations
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Source Information
Source data not available.