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Ichnological analysis of the Pleistocene Dwarka Formation, Gulf of Kachchh: tracemaker behaviors and reworked traces

机译:卡契海湾更新世德瓦卡组的技术分析:示踪剂行为和返工痕迹

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Complex interaction among trace fossils are important in understanding organisms niche preference for foraging in ancient rock records. There exist well-recorded examples of compound trace fossils. However, such compound traces rarely exhibit exploitation of burrow wall and fill sediments for feeding. In recent sediments, several examples are well documented for feeding on burrow wall and burrow fills because of nutrient enrichments in them. Such type of complex interactions occur in the shallow marine Pleistocene age sequences exposed in island in Gulf of Kachchh, India. These deposits are known as ‘Shankhodhar Sand Clay Member’ of Dwarka Formation. Trace fossils recorded are Chondrites , Chomatichnus , Gyrolithes , Ophiomorpha, Rhizocorallium , Schaubcylindrichnus , Sinusichnus , Spongeliomorpha , Taenidium and display three Ichnoassemblages. Three types of complex interactions are suggested: (1) Burrow architecture modification, (2) feeding on burrow walls and burrow fills and (3) acute angle branching. Thus, the trace fossil association indicates selective preference of trace maker for their foraging activities in shallow marine Shankhodhar Sand Clay Member of Pleistocene age.
机译:痕迹化石之间复杂的相互作用对于理解生物在古岩石记录中觅食的生态位偏好至关重要。有记录良好的复合痕迹化石实例。然而,这种复合痕迹很少显示出对洞穴壁的利用并填充了沉积物用于喂养。在最近的沉积物中,由于其中的养分含量丰富,因此有很多实例可以用来进食洞穴壁和洞穴填充物。这种复杂的相互作用类型发生在印度卡奇赫湾的岛屿中暴露的浅海更新世年龄序列中。这些矿床被称为Dwarka组的“ Shankhodhar砂土成员”。记录的痕迹化石是蛇纹石,蛇纹石,陀螺,蛇形纲,根茎线虫,剑齿龙,剑形目,,形变体,Ta钛和显示三个鱼类组合。建议了三种类型的复杂相互作用:(1)挖洞结构的修改;(2)挖洞壁和挖洞的填充物;(3)锐角分支。因此,痕迹化石协会表明在更新世时代浅海海洋Shankhodhar沙土成员中,痕迹制造者对其觅食活动的选择性偏爱。

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