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西大西洋的蜘蛛蟹,特别提及化石及一些现代的蜘蛛蟹科。

Spider crabs of the Western Atlantic with special reference to fossil and some modern Mithracidae.

作者信息

Klompmaker Adiël A, Portell Roger W, Klier Aaron T, Prueter Vanessa, Tucker Alyssa L

机构信息

Florida Museum of Natural History, University of Florida , Gainesville, FL , United States of America ; Department of Geological Sciences, University of Florida , Gainesville, FL , United States of America.

Florida Museum of Natural History, University of Florida , Gainesville, FL , United States of America.

出版信息

PeerJ. 2015 Oct 1;3:e1301. doi: 10.7717/peerj.1301. eCollection 2015.

Abstract

Spider crabs (Majoidea) are well-known from modern oceans and are also common in the western part of the Atlantic Ocean. When spider crabs appeared in the Western Atlantic in deep time, and when they became diverse, hinges on their fossil record. By reviewing their fossil record, we show that (1) spider crabs first appeared in the Western Atlantic in the Late Cretaceous, (2) they became common since the Miocene, and (3) most species and genera are found in the Caribbean region from the Miocene onwards. Furthermore, taxonomic work on some modern and fossil Mithracidae, a family that might have originated in the Western Atlantic, was conducted. Specifically, Maguimithrax gen. nov. is erected to accommodate the extant species Damithrax spinosissimus, while Damithrax cf. pleuracanthus is recognized for the first time from the fossil record (late Pliocene-early Pleistocene, Florida, USA). Furthermore, two new species are described from the lower Miocene coral-associated limestones of Jamaica (Mithrax arawakum sp. nov. and Nemausa windsorae sp. nov.). Spurred by a recent revision of the subfamily, two known species from the same deposits are refigured and transferred to new genera: Mithrax donovani to Nemausa, and Mithrax unguis to Damithrax. The diverse assemblage of decapods from these coral-associated limestones underlines the importance of reefs for the abundance and diversity of decapods in deep time. Finally, we quantitatively show that these crabs possess allometric growth in that length/width ratios drop as specimens grow, a factor that is not always taken into account while describing and comparing among taxa.

摘要

蜘蛛蟹(蜘蛛蟹总科)在现代海洋中广为人知,在大西洋西部也很常见。蜘蛛蟹在地质历史时期出现在西大西洋的时间以及它们何时开始多样化,取决于它们的化石记录。通过回顾它们的化石记录,我们发现:(1)蜘蛛蟹最早在晚白垩世出现在西大西洋;(2)自中新世以来它们变得常见;(3)从中新世开始,大多数物种和属都发现于加勒比地区。此外,还对一些现代和化石的坚壳蟹科进行了分类学研究,该科可能起源于西大西洋。具体而言,建立了新属马圭坚壳蟹属以容纳现存物种多刺坚壳蟹,同时首次从化石记录(上新世晚期 - 更新世早期,美国佛罗里达)中识别出似肋刺坚壳蟹。此外,从牙买加下中新世与珊瑚相关的石灰岩中描述了两个新物种(阿拉瓦克坚壳蟹新种和温莎内马坚壳蟹新种)。受该亚科近期修订的推动,对来自同一沉积物的两个已知物种进行了重新描述并转移到新属:多诺万坚壳蟹转移到内马坚壳蟹属,爪坚壳蟹转移到坚壳蟹属。这些与珊瑚相关的石灰岩中十足目动物的多样组合突出了地质历史时期珊瑚礁对于十足目动物丰富度和多样性的重要性。最后,我们定量表明这些螃蟹具有异速生长,即随着标本生长,长度/宽度比会下降,而在描述和比较分类单元时,这一因素并不总是被考虑在内。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/de2c/4636416/9e4b05de2785/peerj-03-1301-g001.jpg

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