Relationship between depth, sediment, latitude, and the structure of benthic infaunal assemblages on the mainland shelf of southern California

Citation
M. Bergen et al., Relationship between depth, sediment, latitude, and the structure of benthic infaunal assemblages on the mainland shelf of southern California, MARINE BIOL, 138(3), 2001, pp. 637-647
Citations number
53
Categorie Soggetti
Aquatic Sciences
Journal title
MARINE BIOLOGY
ISSN journal
00253162 → ACNP
Volume
138
Issue
3
Year of publication
2001
Pages
637 - 647
Database
ISI
SICI code
0025-3162(200103)138:3<637:RBDSLA>2.0.ZU;2-#
Abstract
A regional benthic survey was conducted in 1994, and the data were used to assess the relationship among three habitat factors (depth, sediment grain size, and latitude) and the distribution of benthic infaunal assemblages on the southern California coastal shelf. Benthic samples were collected with a 0.1 m(2) Van Veen grab from 251 sites on the continental shelf (10-200 m deep) from Point Conception, California, to the United States-Mexico inter national border. The relationship between habitat and assemblages was inves tigated by conducting a Q-mode cluster analysis to define groups of station s with similar species composition and then examining whether differences w ere present in physical habitat attributes among those groups of stations. Analysis of data from 175 uncontaminated sites yielded four habitat-related benthic infaunal assemblages along the southern California coastal shelf: a shallow-water assemblage from 10-32m, a mid-depth assemblage between 32 a nd 115 m, and two deep-water (115-200 m) assemblages, one in fine and one i n coarse sediments. These empirically defined points in the depth and sedim ent grain size gradients can be used to define reference habitats for the d evelopment of biocriteria. Benthic abundance and diversity were greatest in the mid-depth assemblage, conforming to predictions for benthic assemblage s in regions of upwelling. Within the 500 km of coastline examined, latitud e was not an important factor in defining assemblages.