151 Environmental Geoscience (Posters)
BENTHIC FORAMINIFERA IN LONG ISLAND SOUND: INDICATORS OF ENVIRONMENTAL CHANGES
Paper number: 151-29
Program: Technical Sessions
Time: 8:00 AM – 12:00 PM
Authors
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Shaleen BowmanN/A
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Ellen ThomasWesleyan Univ, Middletown, CT
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Johan C. VarekampWesleyan Univ, Middletown, CT
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Ellen L. MecrayU. S. Geol Survey, Woods Hole, MA
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Joel MooreU. S. Geol Survey, Woods Hole, MA
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Marilyn Buchholtz ten BrinkU. S. Geol Survey, Woods Hole, MA
Abstract
Assemblages vary by water depth and by sub-basin. A core taken to the east of the Connecticut River contains assemblages with open marine shelf species (e.g., Eponides repandus). The relative abundance of the herbivorous species E. excavatum is highest (>90%) in cores at water depths <10 m, and increased throughout LIS from ~1850 AD on, possibly in response to anthropogenic eutrophication. The increase in relative abundance of Ammonia beccarii is a post-1960s phenomenon, and is most pronounced at sites at water depths <10 m and in western LIS. A core collected near the mouth of the Connecticut River shows a high relative abundance of A. beccarii in post-1960 samples, despite its location in eastern LIS, possibly as a result of high nutrient influx from the river. In the Gulf of Mexico and Chesapeake Bay, recent increases in relative abundance of A. beccarii have been linked to increased hypoxia/anoxia, but our data, the species’ biogeography and laboratory behavior suggest that in LIS regional warming may also be important.