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来自施蒂里亚盆地斯洛文尼亚部分的早中新世深水十足目甲壳动物群落及其古环境和古生物地理学意义。

AN EARLY MIOCENE DEEP-WATER DECAPOD CRUSTACEAN FAUNULE FROM THE SLOVENIAN PART OF THE STYRIAN BASIN, AND ITS PALAEOENVIRONMENTAL AND PALAEOBIOGEOGRAPHICAL SIGNIFICANCE.

作者信息

Gašparič Rok, Hyžný Matúš

机构信息

Oertijdmuseum De Groene Poort, Bosscheweg 80, NL-5283 WB Boxtel, The Netherlands;

Geological-Paleontological Department, Natural History Museum, Burgring 7, A-1010 Vienna, Austria;

出版信息

Pap Palaeontol. 2015 May 1;1(2):141-166. doi: 10.1002/spp2.1006.

Abstract

A new decapod crustacean faunule is described from the early Miocene of the Slovenian part of the Styrian Basin. The Ivnik Beds exposed at the Činžat locality contain seven species: (Axiidea: Callianassidae), Lepidophthalmus paratethyensis sp. nov. (Axiidea: Callianassidae), (Gebiidea: Laomediidae), (Brachyura: Chasmocarcinidae), (Brachyura: Goneplacidae), sp. nov. (Brachyura: Mathildellidae) and sp. nov. (Brachyura: Retroplumidae). Numerous specimens of well-preserved permitted its redescription and re-assignment of its familial placement to Chasmocarcinidae. sp. nov. constitutes the first fossil occurrence of the genus known to date. The decapod association, as well as other faunal elements, suggests low-energy deep-water depositional environment with epibathyal water depth of more than 125 m. The studied locality is situated in the Ribnica-Selnica graben filled with sediments once deposited in the Central Paratethys sea. Based on the affinities of decapod genera of the Central Paratethys and the Proto-Mediterranean, we conclude that the exchange of decapod faunas between these regions was probably regulated by an anti-estuarine circulation permitting an easier incursion of species from the Proto-Mediterranean into the Paratethys and simultaneous hindering the Paratethyan endemics () from entering the Mediterranean.

摘要

本文描述了施蒂里亚盆地斯洛文尼亚部分中新世早期的一个新的十足目甲壳动物群落。在钦扎特地区暴露的伊夫尼克层含有7个物种:(异尾下目:美人虾科),副特提斯刺铠虾,新种(异尾下目:美人虾科),(蝉蟹下目:老蝉蟹科),(短尾下目:裂面蟹科),(短尾下目:藻虾科),新种(短尾下目:马蒂尔德蟹科)和新种(短尾下目:反美螯蟹科)。大量保存完好的标本使得对其重新描述并将其科的归属重新确定为裂面蟹科成为可能。新种是该属迄今为止已知的首次化石记录。十足目动物群落以及其他动物区系元素表明,该地区为低能深水沉积环境,水深超过125米,属于上半深海。研究地点位于里布尼察-塞尔尼察地堑,该地堑曾沉积有中央特提斯海的沉积物。基于中央特提斯和原始地中海十足目属的亲缘关系,我们得出结论,这些地区之间十足目动物群的交换可能受反河口环流的调节,这种环流使得物种更容易从原始地中海侵入特提斯海,同时阻碍特提斯海特有物种()进入地中海。

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