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评估三叶虫中的幼态异时性:以来自辛辛那提地区(上奥陶统)辛辛那提统的小型三叶虫柔曲隐头虫微小亚种为例。

Evaluating paedomorphic heterochrony in trilobites: the case of the diminutive trilobite Flexicalymene retrorsa minuens from the Cincinnatian Series (Upper Ordovician), Cincinnati region.

作者信息

Hunda Brenda R, Hughes Nigel C

机构信息

Cincinnati Museum Center, 1301 Western Avenue, Cincinnati, OH 45203, USA.

出版信息

Evol Dev. 2007 Sep-Oct;9(5):483-98. doi: 10.1111/j.1525-142X.2007.00186.x.

DOI:10.1111/j.1525-142X.2007.00186.x
PMID:17845519
Abstract

Flexicalymene retrorsa minuens from the uppermost 3 m of the Waynesville Formation of the Cincinnatian Series (Upper Ordovician) of North America lived approximately 445 Ma and exhibited marked reduction in maximum size relative to its stratigraphically subjacent sister subspecies, Flexicalymene retrorsa retrorsa. Phylogenetic analysis is consistent with the notion that F. retrorsa retrorsa was the ancestor of F. retrorsa minuens. F. retrorsa minuens has been claimed to differ from F. retrorsa retrorsa"in size alone," and thus presents a plausible example of global paedomorphic evolution in trilobites. Despite strong similarity in the overall form of the two subspecies, F. retrorsa minuens is neither a dwarf nor a simple progenetic descendant of F. retrorsa retrorsa. More complex patterns of global heterochronic paedomorphosis, such as a neotonic decrease in the rate of progress along a common ontogenetic trajectory with respect to size, coupled with growth cessation at a small size, "sequential" progenesis, or non-uniform changes in the rate of progress along a shared ontogenetic trajectory with respect to size, can also be rejected. Rather, differences between these subspecies are more consistent with localized changes in rates of character development than with a global heterochronic modification of the ancestral ontogeny. The evolution of F. retrorsa minuens from F. retrorsa retrorsa was largely dominated by modifications of the development of characters already evident in the ancestral ontogeny, not by the origin of novel structures. Factors promoting size reduction in F. retrorsa minuens appear to have been specific to this subspecies, because other co-occurring taxa, including other trilobite species, do not show marked differences in mean size.

摘要

北美辛辛那提统(上奥陶统)韦恩斯维尔组最上部3米处的后弯小卷曲三叶虫生活在约4.45亿年前,与地层位置更低的姊妹亚种后弯卷曲三叶虫相比,其最大体型显著减小。系统发育分析与后弯卷曲三叶虫是后弯小卷曲三叶虫祖先的观点一致。后弯小卷曲三叶虫据称与后弯卷曲三叶虫“仅在体型上”存在差异,因此是三叶虫全球幼态发育演化的一个合理例证。尽管这两个亚种的整体形态极为相似,但后弯小卷曲三叶虫既不是侏儒形态,也不是后弯卷曲三叶虫简单的幼态后代。更复杂的全球异时幼态发育模式,比如沿着共同个体发育轨迹在体型方面的新态速率降低,再加上小体型时生长停止、“连续”幼态发生,或者沿着共享个体发育轨迹在体型方面的发育速率发生非均匀变化,也都可以被排除。相反,这些亚种之间的差异更符合性状发育速率的局部变化,而非祖先个体发育的全球异时性改变。后弯小卷曲三叶虫从后弯卷曲三叶虫的演化主要由祖先个体发育中已明显存在的性状发育变化主导,而非新结构的起源。促进后弯小卷曲三叶虫体型减小的因素似乎是该亚种所特有的,因为其他共生类群,包括其他三叶虫物种,在平均体型上并未表现出明显差异。

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