Winkler Alisa J
Shuler Museum of Paleontology, Department of Geological Sciences, Southern Methodist University, Dallas, Texas 75275, USA.
J Hum Evol. 2002 Jan-Feb;42(1-2):237-56. doi: 10.1006/jhev.2001.0501.
A minimum of 28 genera of rodents and one genus of lagomorph were recovered from the Tugen Hills, Baringo District, Kenya, from localities dating from over 15.5 to about 4.4 Ma. The middle Miocene (sites dated between 15.8 and 15.3 Ma) rodent fauna recovered primarily from the Kipsaramon site complex, Muruyur Formation, includes a mixture of characteristically early Miocene taxa, and more derived forms. Composition of the African rodent fauna changes dramatically with the introduction of myocricetodontines, democricetodontines, and dendromurines, immigrants primarily from southern Asia. In the Tugen Hills, these taxa are first found in the Kabasero localities, Ngorora Formation, at sites dating from 12.5-12.33 Ma. A second major change in the African rodent fauna reflects the introduction of murines, immigrants from southern Asia. In the Tugen Hills murines are first encountered at Kapcheberek, Lukeino Formation, dated to 5.9-5.7 Ma. One rodent genus from the Lukeino Formation (Arvicanthis), and two from the Tabarin locality, Chemeron Formation (Heliosciurus, Paraxerus; 4.5-4.4 Ma), represent the earliest records of these extant African genera. A cricetomyine from the Ngorora Formation (12.5 Ma) is likely the earliest report of this exclusively African group. One of the earliest African records of porcupines (Hystricide) is from the Lukeino Formation. Lagomorphs are poorly represented, but include one of the earliest African occurrences of the family Leporidae from the Mpesida Beds (bracketed by dates of 7-6.2 Ma), and possibly a new genus of leporid from the Kapcheberek locality. Analysis of the Tugen Hills small mammals in association with other African records suggests several episodes of dispersal between Africa and Eurasia during the middle and late Miocene. Rodents from Kipsaramon are indicative of forests in conjunction with more open habitats. Those from the Kapcheberek locality are suggestive of a savanna habitat. The rodents from the Tabarin locality suggest a woodland environment.
在肯尼亚巴林戈区的图根山,从距今1550多万年至约440万年前的不同地点,发现了至少28个啮齿动物属和1个兔形目动物属。从中新世中期(年代测定在1580万至1530万年前)主要从穆鲁尤尔组的基普萨拉蒙遗址群发现的啮齿动物群,包括典型的中新世早期类群和更多衍生形态的混合。随着主要来自亚洲南部的鼠形仓鼠亚科、民主仓鼠亚科和非洲林鼠亚科动物的迁入,非洲啮齿动物群的组成发生了巨大变化。在图根山,这些类群最早发现于恩戈罗拉组的卡巴塞罗地点,年代为1250万至1233万年前。非洲啮齿动物群的第二个主要变化反映了来自亚洲南部的鼠科动物的迁入。在图根山,鼠科动物最早在卡普切贝雷克被发现,属于卢凯诺组,年代为590万至570万年前。卢凯诺组的一个啮齿动物属(非洲沼鼠属)以及切梅龙组塔巴林地点的两个属(非洲太阳松鼠属、非洲长尾松鼠属;450万至440万年前),代表了这些现存非洲属的最早记录。恩戈罗拉组(1250万年前)的一种仓鼠亚科动物可能是这个仅存于非洲的类群的最早记录。豪猪(豪猪科)最早的非洲记录之一来自卢凯诺组。兔形目动物的代表性较差,但包括来自姆佩西达层(年代在700万至620万年前)的兔科动物在非洲的最早出现之一,以及可能来自卡普切贝雷克地点的一个新的兔科属。结合其他非洲记录对图根山小型哺乳动物的分析表明,在中新世中期和晚期,非洲和欧亚大陆之间有几次扩散事件。基普萨拉蒙的啮齿动物表明当时是森林与更开阔栖息地并存的环境。卡普切贝雷克地点的啮齿动物表明是稀树草原栖息地。塔巴林地点的啮齿动物表明是林地环境。