DISTRIBUTION OF ZOOPLANKTON ASSOCIATED WITH THE ENDEAVOR RIDGE HYDROTHERMAL PLUME

Citation
Bj. Burd et Re. Thomson, DISTRIBUTION OF ZOOPLANKTON ASSOCIATED WITH THE ENDEAVOR RIDGE HYDROTHERMAL PLUME, Journal of plankton research, 17(5), 1995, pp. 965-997
Citations number
35
Categorie Soggetti
Marine & Freshwater Biology
ISSN journal
01427873
Volume
17
Issue
5
Year of publication
1995
Pages
965 - 997
Database
ISI
SICI code
0142-7873(1995)17:5<965:DOZAWT>2.0.ZU;2-1
Abstract
Enhanced zooplankton biomass was found in shallow (<900 m) and deep (> 900 m) net samples collected over the Endeavour Ridge hydrothermal plu me in 1991 and 1992. This enhanced biomass was manifest in considerabl y higher abundance values for most species in proximity to the vent fi eld compared with abundance values from net samples collected 10-50 km off-axis. The species most enriched in abundance by the hydrothermal plume were those normally found in the mid-depth scattering layer at 4 00-900 m depth. These mid-depth animals were also the dominant fauna i n the deep scattering layers that overlie the hydrothermal plume at de pths of 1200-1900 m near the main vent field. The abundance and biomas s dominants were species with Pronounced ontogenetic migration pattern s, and their associated predators. The abundance of many typically dee p species was also enhanced over the main vent field. Faunal compositi ons of net samples were compared using a similarity measure and averag e linkage rule. Deep fauna in proximity to the vent field but not asso ciated with scattering layers (Group 1), were similar to deep fauna 10 -50 km off-axis. The fauna of the deep scattering layer over the vent field (Group 2) was most similar to surface and mid-depth scattering l ayer fauna found within a 50 km radius of the vent field. Statistical tests of linkages obtained using a bootstrap method indicate that the abundance and taxonomic composition of the two faunal groups were sign ificantly distinct in 1992, but not in 1991. We conclude that there wa s considerable infiltration of shallow fauna into the deep scattering layers within 2-3 km of the main vent field, less extensive infiltrati on 10-15 km to the north and south of the vent field in 1991, and insi gnificant infiltration at stations 50 km to the west of the vent field in 1992. A bootstrap analysis comparing the faunal composition of net s towed above 900 m depth showed that shallow fauna were not significa ntly distinct between the two sampling years or up to 50 km away from the vent field.