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保存在脊椎动物粪化石中的介壳虫幼虫(法国勒凯斯诺伊,始新世早期):古生态学见解

Scale insect larvae preserved in vertebrate coprolites (Le Quesnoy, France, Lower Eocene): paleoecological insights.

作者信息

Robin Ninon, Foldi Imre, Godinot Marc, Petit Gilles

机构信息

Muséum National d'Histoire Naturelle, CNRS, UPMC, Sorbonne Université, UMR 7207 CR2P, 8 rue Buffon, CP 38, 75005, Paris, France.

Muséum National d'Histoire Naturelle, UMR 7205, CP50, Entomologie, Paris, France.

出版信息

Naturwissenschaften. 2016 Oct;103(9-10):85. doi: 10.1007/s00114-016-1412-x. Epub 2016 Sep 29.

Abstract

Coprolites of terrestrial vertebrates from the Sparnacian Le Quesnoy locality (Ypresian, Eocene, MP7, 53 Ma; Oise, France) were examined for possible parasitic helminth eggs. The extraction of the coprolite components was performed by a weak acetolyse and a slide mounting in glycerin. This long examination did not reveal paleoparasite remains, which may be explained through several arguments. However, some pollen grains, some enigmatic components, and two well-preserved first-instar cochineal nymphs (Hemiptera: Sternorrhyncha: Coccoidea) were evidenced in coprolites. Identified as Coccidae, these larvae are the earliest stage of the scale insect development ever reported as fossil, revealing the specific environment of preservation that fossilized scats may provide. These observations, combined to the coprolites morphotype, enable to ascribe the fossil scats producer to a small herbivorous mammal present in the deposit (early perissodactyls or Plesiadapidae). Regarding the ecology of extant representatives of Coccidae, this mammal was a likely foliage consumer, and the abundant Juglandaceae and/or Tiliaceae from Le Quesnoy might have lived parasitized by scale insects. These Early Eocene parasites had an already well-established dissemination strategy, with prevalent minute first-instar larvae. The herein performed extraction technique appears well-suited for the study of carbonate coprolites and could certainly be useful for evidencing other kind of microorganisms (including internal parasites).

摘要

对来自法国瓦兹省勒凯斯努瓦地区(始新世伊普雷斯期,MP7,5300万年前)斯帕尔纳阶的陆生脊椎动物粪便化石进行了检查,以寻找可能存在的寄生蠕虫卵。通过轻度乙酸分解法和甘油载玻片固定法对粪便化石成分进行提取。长期的检查未发现古寄生虫遗迹,对此可通过多种观点来解释。然而,在粪便化石中发现了一些花粉粒、一些神秘成分以及两只保存完好的一龄胭脂虫若虫(半翅目:胸喙亚目:蚧总科)。这些幼虫被鉴定为蚧科,是有化石记录以来介壳虫发育的最早阶段,揭示了粪便化石可能提供的特定保存环境。这些观察结果,结合粪便化石的形态类型,使得能够将化石粪便的产生者归为该沉积层中存在的一种小型食草哺乳动物(早期奇蹄目动物或近猴科动物)。关于现存蚧科动物的生态,这种哺乳动物可能以树叶为食,而勒凯斯努瓦地区丰富的胡桃科和/或椴科植物可能曾受到介壳虫的寄生。这些始新世早期的寄生虫已经有了完善的传播策略,其主要是微小的一龄幼虫。本文所采用的提取技术似乎非常适合研究碳酸盐粪便化石,并且肯定有助于发现其他种类的微生物(包括体内寄生虫)。

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