Fossil calibration dates for molecular phylogenetic analysis of snakes 2: Caenophidia, Colubroidea, Elapoidea, Colubridae

被引:0
|
作者
Head, Jason J. [1 ,2 ]
Mahlow, Kristin [3 ]
Mueller, Johannes [3 ]
机构
[1] Dept Zool, Downing St, Cambridge CB2 3EJ, England
[2] Downing St Univ Cambridge, Univ Museum Zool, Downing St, Cambridge CB2 3EJ, England
[3] Leibniz Inst Evolut & Biodivers Forsch, Museum Naturkunde, Invalidenstr 43, D-10115 Berlin, Germany
基金
美国国家科学基金会;
关键词
Serpentes; fossil; calibration; Caenophidia; Colubroidea; Elapoidea; Colubridae; LATE MIOCENE SNAKES; WESTERN INDIA; EARLY EOCENE; ECOLOGICAL OPPORTUNITY; MAEVARANO FORMATION; SQUAMATE REPTILES; SPECIES RICHNESS; MAHAJANGA BASIN; EARLY OLIGOCENE; CENTRAL-EUROPE;
D O I
暂无
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Caenophidia, the snake clade that includes the highest species richness, morphological diversity, and ecological breadth within Serpentes, has been extensively studied with respect to molecular phylogenetic systematics. The majority of the caenophidian fossil record, though dense, has been taxonomically defined on the basis of general anatomical similarity or shared geographic provenance with extant reference taxa. As a result, historical patterns of diversification within the clade are poorly constrained due to a paucity of reliable fossil calibration dates. Here we provide 10 fossil calibration dates for phylogenetic analysis of caenophidian relationships. Calibration points include apomorphy-based systematic justifications based on cranial and precloacal vertebral elements and precise dates for hard minimum divergence timings. Calibrated nodes are for Caenophidia, Acrochordus, Elapoidea, Colubridae, and constituent sub-clades. Hard minimum divergence timings range from late Cretaceous to Miocene. The spatial and temporal distribution of reliable first occurrence of colubroid taxa suggests late Paleogene intercontinental dispersals between Asia, North America, and Africa, followed by rapid diversification and subsequent dispersals into all non-Polar continents by the early Neogene.
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页数:21
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