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首页> 外文期刊>Paleobiology >Taphonomic bias and time-averaging in tropical molluscan death assemblages: differential shell half-lives in Great Barrier Reef sediment
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Taphonomic bias and time-averaging in tropical molluscan death assemblages: differential shell half-lives in Great Barrier Reef sediment

机译:热带软体动物死亡组合中的音速偏差和时间平均:大堡礁沉积物的壳半衰期不同

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摘要

Radiocarbon-calibrated amino acid racemization ages of 428 individually dated shells representing four molluscan taxa are used to quantify time-averaging and shell half-lives with increasing burial depth in the shallow-water carbonate lagoon of Rib Reef, central Great Barrier Reef, Australia. The top 20 cm of sediment contains a distinct, essentially modern assemblage. Shells recovered at depths from 25 to 125 cm are age-homogeneous and significantly older than the surface layer. Taxon age distributions within sedimentary layers indicate that the top 125 cm of lagoonal sediment is thoroughly mixed on a sub-century scale. The age distributions and shell half-lives of four taxa (Ethalia, Natica, Tellina, and Turbo) are found to be largely distinct. Shell half-lives do not coincide with any single morphological characteristic thought to infer greater durability, but they are strongly related to a combined durability score based on shell density, thickness, and shape. These results illustrate the importance of bioturbation in tropical sedimentary environments, indicate that age estimates in this depositional setting are sensitive to taxon choice, and quantify a taxon-dependent bias in shell longevity and death assemblage formation.
机译:放射性碳校准的氨基酸外消旋年龄为428个代表四个软体动物类群的单独的壳,用于量化平均时间和壳半衰期,其随埋葬深度的增加而增加 < / sup>在澳大利亚大堡礁中部Rib Reef的浅水碳酸盐泻湖中。沉积物的顶部20厘米包含 独特的,实质上是现代的组合。在25至125厘米深度处恢复的壳 是年龄均一的,并且显着比表层老。 沉积层内的分类年龄分布表明,泻湖沉积物的顶部125 cm在一个世纪以下的时间里被彻底混合。发现四个类群(Ethalia,Natica, Tellina和Turbo)的年龄 分布和壳半衰期截然不同。 Shell 半衰期与任何可以推断出更高耐久性的形态学特征 不符,但它们与基于组合耐久性得分的 密切相关壳密度,厚度, 和形状。这些结果说明了生物扰动 在热带沉积环境中的重要性,表明该沉积环境中的年龄估计 对分类群选择敏感, 并量化了壳寿命和死亡的分类群依赖性偏见 组装形成。

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  • 来源
    《Paleobiology》 |2009年第4期|565-586|共22页
  • 作者单位

    School of Marine and Tropical Biology, James Cook University, Townsville, Queensland 4811, Australia;

    Australian Nuclear Science and Technology Organisation, PMB 1, Menai, New South Wales 2234, Australia qhx@ansto.gov.au;

    Department of Geology, Northern Arizona University, Flagstaff, Arizona 86011-4099 Darrell.Kaufman@nau.edu;

    School of Earth and Environmental Sciences, James Cook University, Townsville, Queensland 4811, Australia Raphael.Wust@jcu.edu.au;

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