Worthy Trevor H, Tennyson Alan J D, Archer Michael, Musser Anne M, Hand Suzanne J, Jones Craig, Douglas Barry J, McNamara James A, Beck Robin M D
School of Earth and Environmental Sciences, Darling Building DP 418, Adelaide University, North Terrace, Adelaide 5005, South Australia, Australia.
Proc Natl Acad Sci U S A. 2006 Dec 19;103(51):19419-23. doi: 10.1073/pnas.0605684103. Epub 2006 Dec 11.
New Zealand (NZ) has long been upheld as the archetypical example of a land where the biota evolved without nonvolant terrestrial mammals. Their absence before human arrival is mysterious, because NZ was still attached to East Antarctica in the Early Cretaceous when a variety of terrestrial mammals occupied the adjacent Australian portion of Gondwana. Here we report discovery of a nonvolant mammal from Miocene (19-16 Ma) sediments of the Manuherikia Group near St Bathans (SB) in Central Otago, South Island, NZ. A partial relatively plesiomorphic femur and two autapomorphically specialized partial mandibles represent at least one mouse-sized mammal of unknown relationships. The material implies the existence of one or more ghost lineages, at least one of which (based on the relatively plesiomorphic partial femur) spanned the Middle Miocene to at least the Early Cretaceous, probably before the time of divergence of marsupials and placentals > 125 Ma. Its presence in NZ in the Middle Miocene and apparent absence from Australia and other adjacent landmasses at this time appear to reflect a Gondwanan vicariant event and imply persistence of emergent land during the Oligocene marine transgression of NZ. Nonvolant terrestrial mammals disappeared from NZ some time since the Middle Miocene, possibly because of late Neogene climatic cooling.
长期以来,新西兰一直被视为生物群在没有非飞行陆地哺乳动物的情况下进化的典型例子。在人类到达之前它们的缺失是个谜,因为在早白垩世时新西兰仍与东南极洲相连,当时各种陆地哺乳动物占据了冈瓦纳大陆相邻的澳大利亚部分。在此,我们报告在新西兰南岛奥塔哥中部圣巴坦斯(SB)附近的马努赫里基亚群中新世(1900 - 1600万年前)沉积物中发现了一种非飞行哺乳动物。一块部分相对原始的股骨和两块具有自近裔特化特征的部分下颌骨代表了至少一种关系未知的小鼠大小的哺乳动物。这些材料意味着存在一个或多个幽灵谱系,其中至少一个(基于相对原始的部分股骨)从中中新世跨越到至少早白垩世,可能早于有袋类和胎盘类在1.25亿年前分化的时间。它在中新世中期出现在新西兰,而此时在澳大利亚和其他相邻陆块显然不存在,这似乎反映了冈瓦纳大陆的替代事件,并意味着在新西兰渐新世海侵期间出现的陆地持续存在。自中新世中期以来的某个时候,非飞行陆地哺乳动物从新西兰消失了,可能是由于晚新近纪的气候变冷。