The current phylogenetic hypothesis for the evolution and biogeography of fiddler crabs relies on the assumption that complex behavioral traits are assumed to also be evolutionary derived. Indo-west Pacific fiddler crabs have simpler reproductive social behavior and are more marine and were thought to be ancestral to the more behaviorally complex and more terrestrial American species. It was also hypothesized that the evolution of more complex social and reproductive behavior was associated with the colonization of the higher intertidal zones. Our phylogenetic analysis, based upon a set of independent molecular characters, however, demonstrates how widely entrenched ideas about evolution and biogeography led to a reasonable, but apparently incorrect, conclusion about the evolutionary trends within this pantropical group of crustaceans. Species bearing the set of "derived traits" are phylogenetically ancestral, suggesting an alternative evolutionary scenario: the evolution of reproductive behavioral complexity in fiddler crabs may have arisen multiple times during their evolution. The evolution of behavioral complexity may have arisen by coopting of a series of other adaptations for high intertidal living and antipredator escape. A calibration of rates of molecular evolution from populations on either side of the Isthmus of Panama suggest a sequence divergence rate for 16S rRNA of 0.9% per million years. The divergence between the ancestral clade and derived forms is estimated to be approximately 22 million years ago, whereas the divergence between the American and Indo-west Pacific is estimated to be approximately 17 million years ago.

译文

当前有关招潮蟹进化和生物地理学的系统发育假说依赖于这样的假设,即复杂的行为特征被认为也是进化衍生的。印度西太平洋招潮蟹的繁殖社会行为更简单,更海洋,被认为是行为更复杂,更陆生的美洲物种的祖先。还假设更复杂的社会和生殖行为的演变与潮间带较高的定殖有关。然而,我们基于一组独立的分子特征进行的系统发育分析表明,关于进化和生物地理学的根深蒂固的思想如何导致对这一泛型甲壳类动物的进化趋势得出合理但显然不正确的结论。具有一系列 “衍生特征” 的物种是系统发育的祖先,这表明了另一种进化方案: 招潮蟹的生殖行为复杂性的进化可能在进化过程中出现了多次。行为复杂性的演变可能是通过对潮间带生活和反捕食者逃逸的一系列其他适应进行合作而引起的。对巴拿马地峡两侧种群分子进化速率的校准表明,16S rRNA的序列发散速率为每百万年0.9%。祖先进化枝和衍生形式之间的差异估计约为2200万年前,而美洲和印度西太平洋之间的差异估计约为1700万年前。

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