首页> 外文期刊>Proceedings of the Yorkshire Geological Society >Biogeography and Mass Extinction: Extirpation and re-invasion of Normalograptus species (Graptolithina) in the Late Ordovician Palaeotropics
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Biogeography and Mass Extinction: Extirpation and re-invasion of Normalograptus species (Graptolithina) in the Late Ordovician Palaeotropics

机译:生物地理学和大规模灭绝:奥陶纪晚古生代正本草(Graptolithina)的灭绝和再入侵

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摘要

Normalograptids constitute a distinctive but not easily identified group of derived axonophorans. A new study of Normalograptus morphology indicates that many Late Ordovician taxa previously identified as Normalograptus are actually referable to Syracograptus and related climacograptoids. These re-identifications have led to the recognition of a complex biogeographic history among normalograptids and their descendants, including an interesting pattern that had previously been overlooked - a late Katian disappearance of Normalograptus from the palaeotropics. Normalograptid palaeogeographic distribution in the Ordovician appears to comprise 5 main phases: (1) evolutionary origin probably in relatively high palaeolatitudes in the early to mid Darriwilian; (2) spread to global distribution in later Darriwilian time; (3) retreat from most low palaeolatitude regions during the early Katian, with perhaps a slightly delayed retreat from Laurentia; (4) a complete extirpation from the low palaeolatitudes by the mid Katian (Ea4); (5) reinvasion of the low palaeolatitudes that accompanies the remarkable ecological and evolutionary replacement of the Diplograptina by species of Normalograptus and their descendants during the latest Katian-early Hirnantian. We propose two sets of hypotheses to explain Late Ordovician Normalograptus distribution. First, given the low species diversity of Normalograptus, we suggest as a null hypothesis that the disappearance of normalograptids from low palaeolatitudes during the late Sandbian and early Katian as simply a stochastic outcome a small clade simply went extinct by chance alone. The alternative is that the loss of Normalograptus species reflects some form of extinction for cause. either: (1) competitive exclusion; or (2) an inability to adapt to changing environmental conditions. In the case of the competitive exclusion hypothesis, the most likely competitors are species of the Diplograptina.
机译:正常脂蛋白构成了独特的但不易识别的衍生轴突基团。一项对正长齿形形态的新研究表明,许多以前被确定为正长齿形的奥陶纪晚期分类群实际上可用于锡拉长齿形棘齿类和相关的云形类。这些重新识别导致人们认识到正角石t及其后代之间复杂的生物地理历史,包括一个以前被忽略的有趣模式-太古堡中正角石og的晚期卡蒂安消失。奥陶纪的正牙形古地理分布似乎包括5个主要阶段:(1)演化起源可能在达里维利亚初中中期相对较高的古纬度; (2)在后来的达里维尔时代传播到全球; (3)在卡蒂安早期从大多数低古纬度地区撤退,也许从劳伦蒂亚撤退的时间略有延迟; (4)凯迪中期中期(Ea4)完全从古隆起灭绝; (5)在最近的凯迪安-赫南提斯早期,由普通og草及其后代显着改变了古隆起的生态和进化替代了低古高原。我们提出了两组假设来解释晚奥陶纪正齿分布。首先,鉴于正态石rap的物种多样性低,我们作为零假设提出,在桑德比亚晚期和卡蒂安早期,低纬度古正齿石的消失只是一个随机的结果,一个小进化枝只是偶然地灭绝了。另一种选择是,正常og物种的消失反映了某种原因的灭绝。 (1)竞争排斥;或(2)无法适应不断变化的环境条件。在竞争排斥假设的情况下,最有可能的竞争者是Diplograptina的物种。

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