Birbal Sahni Institute of Palaeobotany, Lucknow, India.
J Biosci. 2012 Sep;37(4):769-76. doi: 10.1007/s12038-012-9233-3.
Cocos sahnii Kaul, a fossil palm fruit, is validated and described from the Fuller's earth deposits of Kapurdi village of Rajasthan considered as Early Eocene in age. The fossil best resembles the genus Cocos, particularly Cocos nucifera L., which is now a common coastal element thriving in highly moist conditions. The recovery of this coconut-like fruit, along with earlier described evergreen taxa from the same formation, suggests the existence of typical tropical, warm and humid coastal conditions during the depositional period. The present arid to semi-arid climatic conditions occurring in Rajasthan indicate drastic climate change in the region during the Cenozoic. The possible time for the onset of aridity in the region which caused the total eradication of semi-evergreen to evergreen forests is discussed, as well as the palaeobiogeography of coconuts.
卡乌尔氏椰子化石,一种古棕榈科果实,产自拉贾斯坦邦卡普尔迪村的白垩纪地层,被确认为始新世早期。该化石最接近椰子属,尤其是现在常见于沿海地区的椰子椰属,这种椰子属在高湿度条件下茁壮成长。这种椰子状果实的发现,以及同一地层中更早描述的常绿分类群,表明在沉积时期存在典型的热带、温暖和潮湿的沿海条件。拉贾斯坦邦目前的干旱到半干旱气候条件表明,该地区在新生代发生了剧烈的气候变化。讨论了导致半常绿到常绿森林完全消失的干旱的开始时间,以及椰子的古生物地理学。