阿尔科伊最上中新世的Korynochoerus古choerus。。

Q4 Earth and Planetary Sciences Spanish Journal of Paleontology Pub Date : 2022-09-02 DOI:10.7203/sjp.25152

J. van der Made, Margarita Belinchón García

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引用次数: 3

摘要

Alcoy（西班牙阿利坎特）的褐煤矿是一个典型的大型哺乳动物产地，在1845年之前就已经为人所知。这个地方被severa置于上中新世！作者，但它被其他人放在上新世。动物群包括一个suid，它有助于确定当地的年代。在人们所知的很长一段时间里，它被确定为soemmeringi水藻。Korynochoerus paleochoerus和Sus arvernensi。它也可能代表Korynochoerus provincia/is。我们所研究的材料属于Korynochoerus paleochoerus。对Alcoy的年代测定有四个重要的物种：K.pa/aeochoerus、Dicerorhinus schleiermacheri。Hip·parion gromovae和Hipparion crassum。前三个物种被认为最后一次出现在MN 13中，最后一个物种则被认为第一次出现在MN 13中。Alcoy位于MN 13-上中新世。

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Korynochoerus palaeochoerus from the uppermost Miocene of Alcoy..

The lignite mine of Alcoy (Alicante, Spain) is a classic macro mammal locality that was already known before 1845. This locality was placed in the Upper Miocene by severa! authors, but it was placed in the Pliocene by others. The fauna includes a suid, that helps to date the locality. During the long period that the suid was known it has been determined as Hyotherium soemmeringi. Korynochoerus palaeochoerus and Sus arvernensi. It also might represent Korynochoerus provincia/is. The material studied by us belongs to Korynochoerus palaeochoerus. There are four species of importance for dating Alcoy: K. pa/aeochoerus, Dicerorhinus schleiermacheri. Hip· parion gromovae and Hipparion crassum. The first three species are thought to have their last occurrence in MN 13, the last species is thought to have its first occurrence in MN 13. Alcoy is placed in MN 13 -the Upper Miocene.

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来源期刊

Spanish Journal of Paleontology Earth and Planetary Sciences-Paleontology

CiteScore

1.00

自引率

0.00%

发文量

389

期刊介绍： The journal is international and publishes original manuscripts in Spanish and, preferentially, British spelling English on all aspects of broad interest in palaeontology. Particularly, the SJP aims to communicate and promote palaeontological research to the global scientific community. Moreover, articles on new discoveries and approaches are especially welcome. Finally, studies of present-day material can be included if they have significant palaeontological relevance.