| 安徽蚌埠晚更新世的Palaeoloxodon naumanni (Makiyama)及其古环境意义 |
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| 引用本文：王强,田国强,金权.1996.安徽蚌埠晚更新世的Palaeoloxodon naumanni (Makiyama)及其古环境意义[J].地球学报,17(z1):200-206. |
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| 中文摘要:安徽省蚌埠及所辖怀远、固镇、五河三县境内，由于开挖怀（远）-洪（泽湖）新河，相继发现了诺氏古菱齿象Palaeoloxodon naumanni的一个头骨和9个门齿化石，铀系测年表明，它们分别是末次间冰期中72ka B.P.末次冰期中相当间冰阶的63ka和40ka B.P.的生物遗骸，反映晚更新世期间这一地区有3次较暖的生态环境；流水对化石的搬运作用明显，蚌埠以西以重量大的下颚骨为主，蚌埠以北、以东以易搬运的门齿为主，甚至在盛冰期砂层上、下部分别见驼鸟Struthio蛋和古菱齿象化石。 |
| 中文关键词:安徽蚌埠 晚更新世 诺氏古菱齿象 |
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| Late Pleistocene Palaeoloxodon naumanni (Makiyama) in the Bengbu Area, Anhui and Its Palaeoenvironmental Significance |
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| Abstract:Following the excavating of the channel from Huaiyun county, Anhui to Hongzehu Lake, Jiangsu, a total of nine incisors and one skull of Palaeologxodom naumanni (Makiyama) (Fig.2, Plate1) have been found in the course of 80km in length.
In Japan the 14C dating data show that P. naumanni was living in the duration of 16.2-32.0 ka B.P (requeted from Zhou Mingzhen et al.; 1974). Based on te stratigraphic correlation it can be seen that the horizons yielding these fossils had been determined late Late Pleistocene in geological time either in the Huaibei (north side of Huaihe River) Plain of Anhui province or in the north part of Peixian county of Jiangsu province (Fig.3). The U-Series dating data for six specimens represent that two dating data were unavailable, because the specimens dated 190km and that dated 72ka only have a distance of 7m. As the weathering, the enamel on the fossil surface had being denuded out and the ground wa-ter and surrounding sediment all could affect the fossils, so the specimens dated 190ka and 290ka respectively might had being polluted. The specimens dated 72ka B.P. belong to the Late Interglacial stage in time, the specimen dated 63ka B.P. belongs to the duration of warm-temperature phase with 65.0-53.5ka B.P., which was determined in the Bo-hai Sea based on transgressional layer and sporo-pollen analyese. The specimen dated 40ka B.P. belongs to another warm-temperature phase (the duration of 40-30ka B.P.), which was also determined based on same analyses in sea region and on coastal plain.It appears that P. naumanni occurred generally in warm-temperature and wet climatic stage.
However, thses follils might be transported by flowing water or runoff. At Fuyang and Mengcheng counties located at the west side of Bengbu sity, a total of 19 specimens of lower jaw or skull of P. naumanni have been found and in the studied area the incisors are dominant. At Maotang village of Huaiyuan county, the fossil of P. naumanni occurred at the depth 9m and two eggs of Struthio at the depth of 6m (5th volumn from the left in Fig.3). The latter only occurred at the Maximum Glacial Stage (25-15ka B.P.). By the way, the low sea-level at that time caused the riverine hearward-eroding and palaeoland-form had rolling ground, the stratigraphic hiatus also ocurred then (Fig.3). This means that these fossils were not in situ and the western region from the Bengbu city might be the main haunt of P. naumanni at that time. |
| keywords:Bengbu area Anhui province Late Pleistoncene Palaeoloxodon naumanni |
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