Record Details

Environmental control of living symbiotic and asymbiotic foraminifera of the California Current

ScholarsArchive at Oregon State University

Field Value
Title Environmental control of living symbiotic and asymbiotic foraminifera of the California Current
Names Ortiz, Joseph D. (creator)
Mix, Alan C. (creator)
Collier, Robert W. (creator)
Date Issued 1995-12 (iso8601)
Note Copyright 1995 by the American Geophysical Union
Abstract Plankton tows from the northern California Current constrain biological and physical
influences on living planktonic foraminifera. In this region, the dominant factors controlling the
size and distribution of symbiotic and asymbiotic species are light and food. Food decreases offshore.
Light, needed for symbiont photosynthesis, increases offshore as water turbidity lessens.
Asymbiotic foraminifera (e.g., right-coiling Neogloboquadrina pachyderma, Globigerina
quinqueloba, and Globigerina bulloides), which survive by grazing, dominate the coastal fauna.
The most abundant of these species, right-coiling Neogloboquadrina pachyderma, did not change
in size in response to increasing food. Species that benefit from symbiont photosynthesis
(Orbulina universa, Neogloboquadrina dutertrei, Globigerinoides ruber, and Globigerinita glutinata)
dominate the offshore fauna. Individuals of these species are rare and have smaller shells in turbid
waters where light is limited. G. ruber, which is near its thermal tolerance limit of ≈14°C, is the
only species to demonstrate a clear temperature response. Although temperature may control a
foramimferal species distribution near the limits of its thermal tolerance, food and light appear to
provide the primary control under more favorable thermal conditions. We infer that gradients in
food and light can result in quantifiable sedimentary patterns related to oceanic productivity
through changes in plankton biomass and turbidity.
Genre Article
Identifier J. D. Ortiz, Alan C. Mix, and R. W. Collier. "Environmental control of living symbiotic and asymbiotic foraminifera of the California Current." Paleoceanography 10.6 (1995): 987-1009. Print.

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