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Deep-water zooplankton of the Guaymas basin hydrothermal vent field

Publication ,  Journal Article
Wiebe, PH; Copley, N; Van Dover, C; Tamse, A; Manrique, F
Published in: Deep Sea Research Part A, Oceanographic Research Papers
January 1, 1988

Zooplankton from the Guaymas Basin deep-sea vent field were collected with a 1 m2 MOCNESS to examine the distribution of total standing stock, taxonomic composition, size-frequency distribution of zooplankton, and the species composition of calanoid copepods. Low altitude (∼ 100 m above the bottom) horizontal tows along and across the axis of the basin's southern trough, and oblique tows from the bottom of the basin (∼ 2000 m) to the surface were made. Total biomass in near-bottom samples (range: 13-46 cc/1000 m3) was only about a factor of 10 lower than in the upper 100 m. However, there was little or no evidence for enrichment of biomass in the ∼ 100 m zone above the vent site relative to biomass at the same depth horizon over non-vent areas. Total numbers of individuals ranged between 2600 and 4800/1000 m3. Calanoid copepods consistently ranked first in abundance of counts of the taxa, followed by cyclopoid copepods, ostracods, chaetognaths, and amphipods. Other less abundant taxa, but in some cases important contributors to total biomass, were coelenterates (siphonophores, medusae), decapod shrimp, and polychaetes. Size-frequency analysis of individuals from each taxon indicated that the biomass and abundance spectra do not fit the theoretically expected spectra based on weight-dependent metabolism and growth. The pyramid of biomass was substantially different from the pyramid of numbers in this deep-sea community. Of the 67 species of copepods identified in two samples taken on low altitude tows, only 15 co-occurred in both samples. Many of the species in this relatively diverse community remain to be described. Larval and post-larval forms of benthic clams, gastropods, polychaetes, and crustaceans associated with the vents were collected 100-200 m above the southern trough, indicating the post-larvae may play an active role in dispersal of hydrothermal vent species. © 1988.

Duke Scholars

Published In

Deep Sea Research Part A, Oceanographic Research Papers

DOI

ISSN

0198-0149

Publication Date

January 1, 1988

Volume

35

Issue

6

Start / End Page

985 / 1013
 

Citation

APA
Chicago
ICMJE
MLA
NLM
Wiebe, P. H., Copley, N., Van Dover, C., Tamse, A., & Manrique, F. (1988). Deep-water zooplankton of the Guaymas basin hydrothermal vent field. Deep Sea Research Part A, Oceanographic Research Papers, 35(6), 985–1013. https://doi.org/10.1016/0198-0149(88)90072-6
Wiebe, P. H., N. Copley, C. Van Dover, A. Tamse, and F. Manrique. “Deep-water zooplankton of the Guaymas basin hydrothermal vent field.” Deep Sea Research Part A, Oceanographic Research Papers 35, no. 6 (January 1, 1988): 985–1013. https://doi.org/10.1016/0198-0149(88)90072-6.
Wiebe PH, Copley N, Van Dover C, Tamse A, Manrique F. Deep-water zooplankton of the Guaymas basin hydrothermal vent field. Deep Sea Research Part A, Oceanographic Research Papers. 1988 Jan 1;35(6):985–1013.
Wiebe, P. H., et al. “Deep-water zooplankton of the Guaymas basin hydrothermal vent field.” Deep Sea Research Part A, Oceanographic Research Papers, vol. 35, no. 6, Jan. 1988, pp. 985–1013. Scopus, doi:10.1016/0198-0149(88)90072-6.
Wiebe PH, Copley N, Van Dover C, Tamse A, Manrique F. Deep-water zooplankton of the Guaymas basin hydrothermal vent field. Deep Sea Research Part A, Oceanographic Research Papers. 1988 Jan 1;35(6):985–1013.

Published In

Deep Sea Research Part A, Oceanographic Research Papers

DOI

ISSN

0198-0149

Publication Date

January 1, 1988

Volume

35

Issue

6

Start / End Page

985 / 1013