泰国南部“Turritella”Duplicata (Linnaeus, 1758) (cerithi总科,turritellae)的生物学和年代学观察

Pub Date : 2016-12-01 DOI:10.4002/040.059.0206
R. Waite, W. Allmon
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引用次数: 12

摘要

重复Turritella duplicata (Linnaeus, 1758)是一种海洋悬浮食性腹足类动物,分布在东南亚和印度-西太平洋的浅海和潮滩环境中。这是在泰国南部甲米地区诺帕拉塔拉国家公园的一个潮滩上进行的研究。重复Turritella duplicata主要分布在潮间带下游,共采集和测量了90个标本。他们在平面上的地理位置被绘制出来,揭示了人口分布的分区,平行和垂直于海岸线。壳的大小分布表明,该种群完全由成年虫组成。对三个贝壳进行的δ18O年代学研究表明,与季节变化相关的水参数变化高达1.5‰,表明其寿命约为3年,生长速度受季节控制。幼鱼的缺失和观察到的种群分布,再加上化石数据表明,繁殖发生在早春,种群代表大约一岁或更大的三个队列。不能排除在其他季节迁徙到更深的水域的可能性。较小的个体优先在内潮滩发现,2岁以上的个体优先在外潮滩定居。所分析的贝壳的碳同位素组成部分地跟踪了这些生命阶段,表明代谢的“生命效应”正在影响贝壳的δ13C。
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Observations on the Biology and Sclerochronology of “Turritella” Duplicata (Linnaeus, 1758) (Cerithioidea, Turritellidae) from Southern Thailand
ABSTRACT Turritella duplicata (Linnaeus, 1758) is a marine suspension-feeding gastropod found in shallow-marine and tidal flat environments throughout Southeast Asia and the Indo-West Pacific. It was studied on a tidal flat in the national park of Nopparat Thara in the district of Krabi, southern Thailand. Turritella duplicata was found primarily in the lower intertidal zone, and 90 specimens were gathered and measured. Their geographical positions on the flat were mapped, revealing zonations in population distribution, both parallel and perpendicular to the shore-line. The size distribution of the shells indicates that the population consists exclusively of adults. δ18O sclerochronology performed on three shells shows variations of up to 1.5‰ associated with seasonal changes in water parameters, suggesting longevity of about three years and seasonally controlled growth rates. The absence of juveniles and observed population distribution coupled with the sclerochronological data suggest that reproduction occurs in early spring, and that the population represents three cohorts approximately one year in age and older. Migration to deeper water during other seasons cannot be ruled out. Smaller individuals were preferentially found on the inner tidal flat, and individuals older than two years preferentially colonised the outer tidal flat. The carbon isotopic composition of the analysed shells partially tracks these life stages, suggesting that metabolic “vital effects” are influencing the δ13C of the shells.
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