Asphalt mounds and associated biota on the Angolan margin

Jones, D.O.B. ORCID: https://orcid.org/0000-0001-5218-1649; Walls, A.; Clare, M. ORCID: https://orcid.org/0000-0003-1448-3878; Fiske, M.S.; Weiland, R.J.; O'Brien, R.; Touzel, D.F.. 2014 Asphalt mounds and associated biota on the Angolan margin. Deep-Sea Research I, 94. 124-136. https://doi.org/10.1016/j.dsr.2014.08.010

Before downloading, please read NORA policies.

Preview

Text
1-s2.0-S0967063714001654-main.pdf - Published Version
Available under License Creative Commons Attribution.
Download (10MB) | Preview

Abstract/Summary

Release of hydrocarbons from sediments is important in increasing habitat heterogeneity on deep ocean margins. Heterogeneity arises from variation in abiotic and biotic conditions, including changes in substratum, geochemistry, fluid flow, biological communities and ecological interactions. The seepage of heavy hydrocarbons to the seafloor is less well studied than most other cold seep systems and may lead to the formation of asphalt mounds. These have been described from several regions, particularly the Gulf of Mexico. Here, we describe the structure, potential formation and biology of a large asphalt mound province in Block 31SE Angola. A total of 2254 distinct mound features was identified by side-scan sonar, covering a total area of 3.7 km2 of seafloor. The asphalt mounds took a number of forms from small (<0.5 m diameter; 13% observations) mounds to large extensive (<50 m diameter) structures. Some of the observed mounds were associated with authigenic carbonate and active seepage (living chemosynthetic fauna present in addition to the asphalt). The asphalt mounds are seabed accumulations of heavy hydrocarbons formed from subsurface migration and fractionation of reservoir hydrocarbons primarily through a network of faults. In Angola these processes are controlled by subsurface movement of salt structures. The asphalt mounds were typically densely covered with epifauna (74.5% of mounds imaged had visible epifauna) although individual mounds varied considerably in epifaunal coverage. Of the 49 non-chemosynthetic megafaunal taxa observed, 19 taxa were only found on hard substrata (including asphalt mounds), 2 fish species inhabited the asphalt mounds preferentially and 27 taxa were apparently normal soft-sediment fauna. Antipatharians (3.6±2.3% s.e.) and poriferans (2.6±1.9% s.e.) accounted for the highest mean percentage of the observed cover, with actinarians (0.9±0.4% s.e.) and alcyonaceans (0.4±0.2% s.e.) covering smaller proportions of the area. Asphalt mounds represent a common and important habitat on several margin systems globally and should be recognised in future environmental assessment and management of these areas.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1016/j.dsr.2014.08.010
ISSN:	0967-0637
Additional Keywords:	6°45′ S 11°00′ E; Deep-sea benthic biology; Megafauna; Hydrocarbon seep; Chemosynthetic environment; Remotely operated vehicle; Seafloor geology; Habitat heterogeneity
Date made live:	05 Sep 2014 09:12 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/508316

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1016/j.dsr.2014.08.010

ISSN:

0967-0637

Additional Keywords:

6°45′ S 11°00′ E; Deep-sea benthic biology; Megafauna; Hydrocarbon seep; Chemosynthetic environment; Remotely operated vehicle; Seafloor geology; Habitat heterogeneity

Date made live:

05 Sep 2014 09:12 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/508316