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首页> 外文期刊>Pacific Science: A Quarterly Devoted to the Biological and Physical Sciences of the Pacific Region >Systematic review of Late Pleistocene turtles (Reptilia : Chelonii) from the Ryukyu Archipelago, Japan, with special reference to paleogeographical implications
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Systematic review of Late Pleistocene turtles (Reptilia : Chelonii) from the Ryukyu Archipelago, Japan, with special reference to paleogeographical implications

机译:来自日本琉球群岛的晚更新世海龟(Reptilia:Chelonii)的系统综述,特别涉及古地理学意义

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摘要

The Quaternary terrestrial turtle fauna of the Ryukyu Archipelago was reviewed on the basis of recently excavated fossils, as well as literature information. As a result, five extinct species (four geoemydids [Cuora sp., Geoemyda amamiensis, Mauremys sp., and another species with undetermined generic and specific status] and one testudinid [Manouria oyamai]) were recognized from Late Pleistocene cave and fissure deposits. Two of the three turtles currently occurring in this archipelago (C. flavomarginata and G. japonica) were also recognized from comparable deposits on islands, including those where they do not occur at present. These records indicate that the terrestrial turtles of the Ryukyus were much more diverse during the Late Pleistocene than at present, and that extinction has occurred during the last few tens of thousands of years not only for those five fossil species but also for some island populations of the extant species. Distributions of three of the extinct species (G. amamiensis, Cuora sp., and the geoemydid [genus and species undetermined]), confined to the central Ryukyus, are concordant with the currently prevailing hypothesis of Ryukyu paleogeography, which assumes a relatively long isolation of this region and much more recent insularization of the southern Ryukyus. In contrast, distributions of the remaining two extinct species (Man. oyamai and Matt. sp.) must be explained by some ad hoc scenario or, other-wise, drastic modification of the current hypothesis.
机译:根据最近发掘的化石以及文献资料,对琉球群岛第四纪陆生海龟区系进行了审查。结果,从晚更新世洞穴和裂隙沉积物中识别出了五个灭绝的物种(四个土生类(Cuora sp。,Ageomeyda amamiensis,Mauremys sp。,以及另一个具有不确定的一般和特定状态的物种)和一个睾丸类[Manyama Oyamai]。当前在该群岛中出现的三只海龟中的两只(C. flavomarginata和G. japonica)也可以从岛上可比的沉积物中识别出来,包括目前尚不存在的那些。这些记录表明,在晚更新世期间,琉球的陆龟比现在更加多样化,而且在过去的几万年中不仅灭绝了这五种化石物种,而且还造成了一些岛上物种的灭绝。现存物种。仅限于琉球中部的三种灭绝物种(G. amamiensis,Cuora sp。和geoemydid [属和未定物种])的分布与琉球古地理学目前流行的假设相符,该假设假设一个相对较长的孤立期该地区以及最近的南琉球岛孤立化。相反,必须通过一些特殊情况或对当前假说的剧烈修改来解释其余两个已灭绝物种的分布(Manyama oyamai和Matt。sp。)。

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