VARIATIONS IN THE INVERTEBRATE ABYSSAL MEGAFAUNA IN THE NORTH-ATLANTIC OCEAN

Citation
Mh. Thurston et al., VARIATIONS IN THE INVERTEBRATE ABYSSAL MEGAFAUNA IN THE NORTH-ATLANTIC OCEAN, Deep-sea research. Part 1. Oceanographic research papers, 41(9), 1994, pp. 1321-1348
Citations number
90
Categorie Soggetti
Oceanografhy
ISSN journal
09670637
Volume
41
Issue
9
Year of publication
1994
Pages
1321 - 1348
Database
ISI
SICI code
0967-0637(1994)41:9<1321:VITIAM>2.0.ZU;2-N
Abstract
Epibenthic sledge and otter trawl samples of invertebrate megabenthos were collected from the abyss of the northeastern Atlantic Ocean. Stat ions were selected to have contrasting overlying water column structur e. Strong seasonal pulses of phytodetritus on the sea floor have been recorded on the Porcupine Abyssal Plain (PAP) but not on the Madeira A byssal Plain (MAP). Sledge- and trawl-derived abundances of 13.73 and 8.13 individuals 10(3) m-2 were found at PAP, with corresponding wet b iomass values of 169.4 and 189.2 g 10(3) m-2. Data from sledge hauls t aken at MAP gave an abundance of 7.48 individuals and 5.15g 10(3) m-2. Sledge and trawl abundances at Great Meteor East (GME) were 2.91 and 2.19 individuals 10(3) m-2 and 4.31 and 11.30 g 10(3) m-2. Holothurian s dominated the invertebrate biomass at PAP while Asteroidea and Decap oda Natantia were important taxa at MAP and GME. Otter trawl samples d emonstrated fish to be the major component of total megafaunal biomass and suggest that small fixed-frame trawls give gross underestimates o f fish abundance and biomass. Size spectra based on abundance and biom ass data indicated the megafauna to be a functional group at PAP stati on only. Here peak invertebrate biomass occurred in the 40-80 g wet wt size class. In contrast, no large invertebrates (> 20 g wet wt) were found at MAP or GME. Concurrent photographic records indicate higher f aunal densities than do net catches. Faunal differences between statio ns were examined, and a weak relationship between surface productivity and megafaunal abundance was established. Data are inadequate to dete ct a similar relationship with biomass. Biomass values at PAP of 16-39 times those of MAP and GME appear to be explained by the deposition o f phytodetritus at PAP but not at MAP or, probably, at GME. Among inve rtebrates, detritivores form the dominant feeding guild at all localit ies, but carnivores are important at MAP and GME. Phytodetritus appear s to support the abundant surface-grazing holothurians at PAP.