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首页> 外文期刊>Lethaia: An International Journal of Palaeontology and Stratigraphy >Intraspecific variation of hatchling size in late cretaceous ammonoids from hokkaido, japan: Implication for planktic duration at early ontogenetic stage
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Intraspecific variation of hatchling size in late cretaceous ammonoids from hokkaido, japan: Implication for planktic duration at early ontogenetic stage

机译:人工孵化的大小的种内变异从北海道白垩纪菊石,日本:含义为planktic时间早个体发育的阶段

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摘要

Intraspecific variations of the early shell dimensions (ammonitella and protoconch diameters) of two Late Cretaceous (earliest Campanian) ammonoid species (Gaudryceras tenuiliratum and Hypophylloceras subramosum) from the Haboro and Ikushumbetsu areas, Hokkaido, Japan, show no significant difference between these areas that are approximately 110km apart. The geographic distributions of G. tenuiliratum and H. subramosum are supposed to be mainly controlled by the flotation and transportation during the embryonic stage within floating egg masses and/or post-embryonic stage because of their small hatchling sizes (1.18-1.46mm in diameter for G. tenuiliratum, and 0.91-1.13mm in diameter for H. subramosum), suggesting these two ammonite species at the embryonic and/or post-embryonic stages were transported at least 110km. Postulating that the velocity of palaeocurrent around the Haboro and Ikushumbetsu areas during the Cretaceous Period was 0.25m/s, similar to those in the modern ocean current flowing off the eastern Pacific coast of Hokkaido, the egg masses and/or hatchlings of G. tenuiliratum and H. subramosum were buoyant and transported more than 5days. The preliminary comparison of hatchling size through time suggests that the hatching sizes of H. subramosum in Hokkaido increased slightly from the Middle Turonian until the earliest Campanian (during about 7Myr). □ammonoid, hatchling, paleoecology, variation, Cretaceous.
机译:种内变异早期的外壳维度(ammonitella和胎壳直径)两晚白垩世(最早的坎帕阶)菊石(Gaudryceras tenuiliratum和从Haboro Hypophylloceras subramosum)北海道Ikushumbetsu领域,日本,没有这些领域之间的显著差异相距约110公里。分布g . tenuiliratum和H。subramosum应该是主要的控制浮选和运输期间在浮动的卵子质量和/或胚胎阶段因为他们的小post-embryonic阶段人工孵化的大小(直径1.18 - -1.46毫米的G。tenuiliratum, 0.91 - -1.13毫米直径,H。subramosum),表明这两个亚扪人在胚胎和/或post-embryonic物种阶段是运输至少110公里。假定古水流的速度在Haboro Ikushumbetsu区域中白垩纪是0.25 m / s,类似这些在现代海洋的流动的电流东太平洋海岸的北海道,卵子质量和/或g . tenuiliratum和H的幼仔。subramosum活跃、运输均超过5天。大小通过时间表明,孵化大小的h . subramosum在北海道增加从中间土仑阶到最早的坎帕阶(7最高产量研究期间)。□菊石,人工孵化、古生态学变化,白垩纪。

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