MEPS

Marine Ecology Progress Series

MEPS is a leading hybrid research journal on all aspects of marine, coastal and estuarine ecology. Priority is given to outstanding research that advances our ecological understanding.

Online: ISSN 1616-1599

Print: ISSN 0171-8630

DOI: https://doi.org/10.3354/meps

Impact Factor2.1 (JCR 2025 release)

Article Acceptance Rate52.2% (2024)

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Volume contents
Mar Ecol Prog Ser 249:223-236 (2003)

Onshore offshore variations in copepod community structure off the Oregon coast during the summer upwelling season

ABSTRACT: During the summer of 1994, 1996, and 1997, we conducted hydrographic and plankton surveys of the upper 70 m in the nearshore, the continental shelf, and off shelf oceanic waters off Oregon, USA. Copepod densities and biomass were estimated along4 transects from each cruise. The on shelf copepod biomass was 2.8 times greater than off shelf biomass. Nonmetric multidimensional scaling identified an on shelf and an off shelf copepod community. The change in community composition usually occurred ator slightly offshore of the continental shelf break, defined here as 180 m water depth. Indicator-species analysis identified the subarctic neritic species, Calanus marshallae, Pseudocalanus mimus, and Acartia longiremis, as goodindicators of continental shelf waters. ŒWarm water¹ species Mesocalanus tenuicornis, Calocalanus styliremis, Clausocalanus spp., and Ctenocalanus vanus were indicators of off shelf waters. The copepod communities off the coastof Oregon during the summer upwelling season reflect the origins of the dominating currents within each habitat. The coastal copepod community is subarctic neritic in origin, consistent with southward coastal flows. The offshore copepod community is amixture of species with origins in the Transition Zone as well as species that are typical of the coastal region of the California Current off central and southern California. We speculate that the central and southern California Current species arepresent in offshore waters of Oregon in summer because they are transported north with the Davidson Current in winter but, with the initiation of the upwelling season in spring, they are transported into offshore waters where they establish viablepopulations.

KEYWORDS

Cheryl A. Morgan (Corresponding Author)

  • Cooperative Institute for Marine Resources Studies, Oregon State University, Hatfield Marine Science Center, 2030 S. Marine Science Dr., Newport, Oregon 97365, USA
cheryl.morgan@noaa.gov

William T. Peterson (Co-author)

  • National Marine Fisheries Service, Northwest Fisheries Science Center, Hatfield Marine Science Center, 2030 S. Marine Science Dr., Newport, Oregon 97365, USA

Robert L. Emmett (Co-author)

  • National Marine Fisheries Service, Northwest Fisheries Science Center, Hatfield Marine Science Center, 2030 S. Marine Science Dr., Newport, Oregon 97365, USA