Snails versus hermit crabs : a new interpretation on shell-peeling predation in fossil gastropod assemblages
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概要
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We propose two new methods, an "endobiont method" and a "model method," to quantitatively evaluate shell-peeling predation against snails and hermit crabs in fossil gastropod assemblages. The endobiont method, based on the frequency of peeled and pagurized shells, provides the minimum and maximum estimates of predation against hermit crabs. The model method, based on the frequency distribution of shell repairs per shell in peeled and unpeeled shells, estimates directly the frequencies of predation against hermit crabs and snails. Our two methods were applied to a deep-water gastropod assemblage from the Pliocene Shinzato Formation, Okinawa, Japan. Results show that peeling predation, irrespective of the high frequency of repaired breaks (thought to be an indication of high predatory attacks on snails in previous studies), is mostly attributable to hermit crabs rather than to snails in elongate shells, whereas it is the reverse in spherical shells. The results suggest that the frequency of repaired breaks is strongly controlled by the abundance of elongate shells in fossil gastropod assemblages, and that the increasing evidence of peeling predation, irrespective of predation pressure, is also caused by the increase of elongate shells (e.g., caenogastropods) in gastropod assemblages since the mid-Mesozoic. The new methods could be used for the real understanding of the history of this unique biological interaction through geologic times.
- 日本古生物学会の論文
- 2004-06-30
著者
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Kase Tomoki
Department of Geology, National Science Museum
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Kase Tomoki
Department Of Geology And Paleontology National Museum Of Nature And Science
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Kase Tomoki
Department Of Geology National Science Museum
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ISHIKAWA Makiko
Department of Radiology, Fulisawa Municipal Hospital.
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Tsutsui Hidekazu
Laboratory For Cell Function Dynamics Institute For Physical And Chemical Research (riken)
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TOJO BUNJI
Department of Earth and Planetary Science, Nagoya University
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Tojo B
Department Of Earth And Planetary Science Nagoya University
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Ishikawa Makiko
Department Of Geology National Science Museum
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