Control of deep-sea benthic community structure by oxygen and organic-matter gradients in the eastern Pacific Ocean
Document Type
Article
Date of Original Version
1-1-1991
Abstract
At boundaries of oxygen minimum zones (OMZs), bathyal faunas experience steep gradients in oxygen and organic-matter availability. This study compares changes in microbial, meiofaunal, macrofaunal and megafaunal benthic assemblages along these gradients on Volcano 7, a 2.3-km high seamount in the E tropical Pacific. Faunal tolerance to dysaerobic (low oxygen) conditions varies with organism size; microbial and meiofaunal abundances are less affected than macro- and megafaunal abundances. At the exceedingly low concentrations (<0.1 ml/l) encountered on the upper summit of Volcano 7, oxygen appears to exert primary control over abundance, composition and diversity of macrofauna, overriding other factors such as food availability and sediment grain size. When oxygen concentration is sufficient, food availability in sediments is highly correlated with meiofaunal and macrofaunal abundance. -from Authors
Publication Title, e.g., Journal
Journal of Marine Research
Volume
49
Issue
4
Citation/Publisher Attribution
Levin, L. A., C. L. Huggett, and K. F. Wishner. "Control of deep-sea benthic community structure by oxygen and organic-matter gradients in the eastern Pacific Ocean." Journal of Marine Research 49, 4 (1991). doi: 10.1357/002224091784995756.