Goodfriend GA, Gould SJ
G. A. Goodfriend, Geophysical Laboratory, Carnegie Institution of Washington, 5251 Broad Branch Road, NW, Washington, DC 20015, USA. S. J. Gould, Museum of Comparative Zoology, Harvard University, Cambridge, MA 02138, USA.
Science. 1996 Dec 13;274(5294):1894-7. doi: 10.1126/science.274.5294.1894.
The late Quaternary fossil record of the Bahamian land snail Cerion on Great Inagua documents two transitions apparently resulting from hybridization. In the first, a localized modern population represents the hybrid descendants of a 13,000-year-old fossil form from the same area, introgressed with the modern form now characteristic of the adjacent regions. In the second case, a chronocline spanning 15,000 to 20,000 years and expressing the transition of an extinct fossil form to the modern form found on the south coast was documented by morphometry of fossils dated by amino acid racemization and radiocarbon. Hybrid intermediates persisted for many thousands of years.
大伊纳瓜岛巴哈马陆地蜗牛Cerion的晚第四纪化石记录表明,有两次过渡显然是由杂交导致的。第一次,一个局部现代种群是来自同一地区的具有13000年历史的化石形态的杂交后代,它与现在相邻地区特有的现代形态发生了基因渗入。在第二种情况下,通过氨基酸消旋和放射性碳测定年代的化石形态测量法记录了一条跨越15000至20000年的时间渐变群,它显示了一种已灭绝的化石形态向在南海岸发现的现代形态的转变。杂交中间体持续存在了数千年。