Foraminiferal responses to flood events, human activities and sea-level changes in brackish Lake Jinzai, Shimane Prefecture, southwest Japan, in the last 60 years

  • Nomura Ritsuo
    Foraminiferal Laboratory, Faculty of Education and Research Center for Coastal Lagoon Environments, Shimane University
  • Roser Barry P.
    Interdisciplinary Faculty of Science and Engineering, Shimane University

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  • 島根県神西湖(汽水湖)における過去60年間の洪水,人間活動および海面水位変動に対する有孔虫の応答

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Abstract

We examined the impacts of both sea-level changes and flood events on the foraminiferal assemblages in brackish Lake Jinzai, northeast Shimane Prefecture, southwest Honshu, Japan, over the last 60 years. Sea-level rises that occurred around the coast of Japan in the 1950s and mid-1970s are recognized by increases in the number of foraminiferal individuals per gram of sediment, as represented by the brackish species Ammonia “beccarii” and the coastal species Elphidium excavatum. Sea-level rise after the 1990s was not accompanied by an increase in the number of foraminiferal individuals, indicating that the foraminiferal abundance is not primarily controlled by sea-level changes, but rather by some other factors. Long-term information of annual COD (Chemical Oxygen Demand) changes in brackish water from the 1980s indicates that organic contents are a major factor controlling the foraminiferal abundances. We confirmed that the sea-level rise from the late 1980-90s to the present did not contribute to the foraminiferal abundances, as did those of the 1950 and 1970s.<BR>These foraminiferal species also have responded to flood events in three different ways : (1) A. “beccarii” developed first, and E. excavatum occurred later ; (2) only A. “beccarii” occurred ; and (3) both species developed together. The foraminifera responded to the short-term events by increase of individual numbers, suggesting enhanced productivity. Accordingly, flood events contribute an increased supply of food resources for foraminifera, as provided by higher organic contents or nutrients.

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