沃克沙生物群:了解志留纪早期生活的绝佳窗口

Geology Today Pub Date : 2023-09-27 DOI:10.1111/gto.12447
Kenneth C. Gass, Simon J. Braddy
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引用次数: 0

摘要

Waukesha生物群(Brandon Bridge Formation Lagerstätte)是志留纪早期(437 Ma)美国威斯康辛州的浅海化石。它们在细层状白云质泥岩中的特殊保存是由潮汐影响的条件和/或微生物埋藏介导的。贝类生物矿化动物很少见,但软体生物很常见。节肢动物占主导地位,包括三叶虫、叶隆虫、介形虫、一种袋形目动物、一种synziphosurine和各种神秘的类群。动物群还包括进化上的“遗留物”,如古Scolecids和lobopodian。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Waukesha Biota: a wonderful window into early Silurian life

The Waukesha Biota (Brandon Bridge Formation Lagerstätte) is a diverse assemblage of early Silurian (437 Ma) shallow marine fossils from Wisconsin, USA. Their exceptional preservation, in finely laminated dolomitic mudstones, was mediated by tidally-influenced conditions and/or microbial entombment. Shelly biomineralized animals are rare, but soft-bodied organisms are common. Arthropods dominate, including trilobites, phyllocarids, ostracodes, a thylacocephalan, a synziphosurine and various enigmatic groups. The fauna also includes evolutionary ‘holdovers’, such as palaeoscolecids and a lobopodian.

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