> An ellipsoidal chamber which is composed of a very thin organic layer a'/> Probable insect cocoon or pupation chamber in a channel‐fill sandstone bed of the Lower Cretaceous Jinju Formation, South Korea
首页> 外文期刊>Lethaia: An International Journal of Palaeontology and Stratigraphy >Probable insect cocoon or pupation chamber in a channel‐fill sandstone bed of the Lower Cretaceous Jinju Formation, South Korea
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Probable insect cocoon or pupation chamber in a channel‐fill sandstone bed of the Lower Cretaceous Jinju Formation, South Korea

机译:可能的昆虫茧或蛹室在南韩国下白垩纪金济山丛林灌注砂岩床中

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摘要

> An ellipsoidal chamber which is composed of a very thin organic layer and emplaced in an enlargement continuing upwards into a vertical burrow is found in thin sections of a fluvial channel‐fill sandstone bed of the Lower Cretaceous Jinju Formation in South Korea. Micromorphological analysis demonstrates that the ellipsoidal chamber is attributable to Fictovichnus . It can be interpreted as a free‐standing wall of a wasp cocoon attributable to Fictovichnus sciuttoi or Fictovichnus aragon , or an organic lining of chafer beetle or weevil pupation chamber attributable to Fictovichnus gobiensis . The analysis further shows that the vertical burrow and enlargement appear to reflect chafer and weevil larval behaviour, but the arrangement of the chamber within the enlargement appears to be the same as a wasp cocoon inside a cell. Such uncertainties of ichnotaxonomic assignment and putative producer suggest that the Jinju specimen may reflect an aberrant pupation behaviour of coleopterans or hymenopterans. This Early Cretaceous specimen may be the earliest record of an insect pupation structure probably associated with a burrow. Its atypical morphologies and very rare occurrence in a channel sandstone bed without other evidence of pedogenesis suggest that the Jinju specimen was constructed in incipiently and briefly exposed sediment, unlike typical insect nesting structures constructed in soil.
机译: > 椭圆形腔室由非常薄的有机层组成并在扩大到垂直洞穴中的扩大中被施加到垂直洞穴中,在韩国下白垩纪金济州的河流灌注砂岩床的薄片中发现。微观分析表明椭圆形腔室可归因于 fictovichnus 。它可以被解释为一种归属于WASP茧的独立墙 Fictovichnus sciuttoi 或者 fictovichnus aragon 或归因于 Fictovichnus gobiensis 。该分析进一步表明,垂直挖洞和放大似乎反映了褶皱和象鼻虫幼虫行为,但是腔室内的腔室的布置似乎与细胞内的黄蜂茧相同。米诺莫明的转让和推定制片人的这种不确定性表明,金州标本可能反映鞘翅目性植物或血管内单人的异常蛹行为。这种早期的白垩纪标本可能是可能与洞穴相关的昆虫蛹结构的最早记录。其非典型形态和在通道砂岩床上非常罕见,没有其他基础证据表明,金州标本在初始和短暂的暴露沉积物中构建,与土壤中构建的典型昆虫嵌套结构不同。

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