We find three coral boulders (approx. 5 m across) resting on the Holocene coral terrace on the Jiupeng coast of southeastern Taiwan. Three exotic corals on the outer part of the boulders are dated at ca. 5000 yr BP which is similar to that of in situ corals composing the Holocene terrace. We interpret that these boulders were broken off from the coral terrace and were transported by tsunami waves, although the timing of the paleotsunami is not determined at this stage.
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机译：我们在台湾东南部九鹏海岸的全新世珊瑚阶地上发现了三个珊瑚石（宽约5 m）。巨石外部的三个外来珊瑚的日期大约为。 5000 yr BP，类似于组成全新世阶地的原位珊瑚。我们解释说，这些巨石是从珊瑚阶地上折断的，并通过海啸波进行了运输，尽管目前还不确定古海啸的发生时间。
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