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Environmental controls on the stable isotopic composition of Mercenaria mercenaria: Potential application to paleoenvironmental studies

机译:对mercenaria mercenaria稳定同位素组成的环境控制:对古环境研究的潜在应用

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摘要

We have investigated the environmental controls of seasonally resolved records of oxygen and carbon isotopes of modern Mercenaria mercenaria bivalves collected live from five coastal sites along the east coast of North America. Seasonal profiles of δ18O and δ13C obtained by subsampling the incremental growth layers of aragonite were compared with in situ historical records of temperature and salinity. We show that M. mercenaria δ18O profiles track accurately the seasonal variations of water temperature and that variations in growth rates do not affect the shell δ18O values. Growth rates are strongly reduced or interrupted below water temperatures ranging from 8 to 10°C, implying that only bivalves sampled in tropical areas track the full amplitude of seasonal variations. Although further measurements of water δ18O and a better understanding of seasonal variations of the water δ18O-salinity relationships are necessary, Mercenaria mercenaria bivalves appear to precipitate their shell close to isotopic equilibrium. Whereas the amplitude of the seasonal profiles of δ18O reflects variations in water temperature, the annual average δ18O decreases with latitude, reflecting the trend of rainfall and riverwater δ18O with latitude over the Northern American continent.
机译:我们已经调查了从北美沿东海岸的五个沿海地点采集的现代Mercenaria mercenaria bivalves的氧和碳同位素的季节性分解记录的环境控制。通过对文石的增量生长层进行二次采样获得的δ18O和δ13C的季节性分布图与温度和盐度的原位历史记录进行了比较。我们显示,M。mercenariaδ18O轮廓准确地跟踪了水温的季节性变化,并且增长率的变化不会影响壳中的δ18O值。在8至10°C的水温以下,生长速度会大大降低或中断,这意味着只有在热带地区采样的双壳类动物才能追踪季节变化的全部幅度。尽管有必要对水δ18O进行进一步测量并更好地了解水δ18O-盐度关系的季节性变化,但Mercenaria mercenaria bivalves的壳似乎沉淀出接近同位素平衡的位置。 δ18O的季节廓线的振幅反映了水温的变化,而年平均δ18O则随纬度而降低,反映了北美大陆降雨和河流水δ18O随纬度的变化趋势。

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