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首页> 外文期刊>Paleobiology >Ion microprobe-measured stable isotope evidence for ammonite habitat and life mode during early ontogeny
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Ion microprobe-measured stable isotope evidence for ammonite habitat and life mode during early ontogeny

机译:离子微探测器测量的稳定同位素证据在早期组织发生期间的氨栖息地和生命模式

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摘要

Ammonites have disparate adult morphologies indicative of diverse ecological niches, but ammonite hatchlings are small (similar to 1 mm diameter), which raises questions about the similarity of egg incubation and hatchling life mode in ammonites. Modern Nautilus is sometimes used as a model organism for understanding ammonites, but despite their outward similarities, the groups are only distantly related. Trends in ammonite diversity and extinction vulnerability in the fossil record contrast starkly with those of nautilids, and embryonic shells from Late Cretaceous ammonites are two orders of magnitude smaller than nautilid embryonic shells. To investigate possible environmental changes experienced by ammonite hatchlings, we used secondary ion mass spectrometry to analyze the oxygen and carbon isotope composition of the embryonic shells and early postembryonic whorls of five juveniles of Hoploscaphites comprimus obtained from a single concretion in the Fox Hills Formation of South Dakota. Co-occurring bivalves and diagenetic calcite were also analyzed to provide a benthic baseline for comparison. The oxygen isotope ratios of embryonic shells are more like those of benthic bivalves, suggesting that ammonite eggs were laid on the bottom. Ammonite shell immediately after hatching has more negative delta O-18, suggesting movement to more shallow water that is potentially warmer and/or fresher. After approximately one whorl of postembryonic growth, the values of delta O-18 become more positive in three of the five individuals, suggesting that these animals transitioned to a more demersal mode of life. Two other individuals transition to even lower delta O-18 values that could suggest movement to nearshore brackish water. These data suggest that ammonites, like many modern coleoids, may have spawned at different times of the year. Because scaphites were one of the short-term Cretaceous-Paleogene extinction survivors, it is possible that this characteristic allowed them to
机译:氨气具有不同的成年形态,指示各种生态核桃,但含有幼龟小(类似于1毫米的直径),这提出了关于蛋孵育和孵化寿命模式在氨基中的相似性的问题。现代鹦鹉螺有时被用作理解氨化的模型生物体,但尽管他们的外在相似之处,但这些群体只是远方相关。在化石记录中含有多样性和消灭脆弱性的趋势与晚白垩世氨基中的胚胎记录对比度呈现出对比度的趋向性,以及胚胎胚胎的胚胎壳比鹦鹉苷胚胎壳小的两个数量级。为了探讨氨孵化器所经历的可能的环境变化,我们使用二次离子质谱法分析胚胎壳的氧气和碳同位素组成和从南部狐狸山的狐狸山的单一混凝土中获得的五个幼儿的早期嗜睡液。达科他州。还分析了共同发生的双抗体和成岩方解石以提供底线基线进行比较。胚胎壳的氧同位素比更像是底栖母壳的脂肪植物,表明氨铁蛋白被铺设在底部。孵化后立即具有更多负ΔO-18,表明移动到更浅的水,这是可能加热的浅水和/或更柔软的水。经过大约一个后后期生长的螺旋,Delta O-18的价值在五个人中的三个中变得更加积极,这表明这些动物转变为更偏见的生活方式。另外两位个人转变为甚至更低的Delta O-18值,可以建议将移动到近岸咸水。这些数据表明,如许多现代鞘翅目一样,可能在今年的不同时间生成。因为替代者是短期白垩纪 - 古代族消灭幸存者之一,所以这一特征可以允许它们

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