首页> 外文期刊>Global ecology and biogeography >Do past climate states influence diversity dynamics and the present-day latitudinal diversity gradient?
【24h】

Do past climate states influence diversity dynamics and the present-day latitudinal diversity gradient?

机译:过去的气候状态是否会影响多样性动态和当今的纬度多样性梯度?

获取原文
获取原文并翻译 | 示例
           

摘要

Aim To identify the role of climate variations over geological time in shaping present-day diversity patterns, particularly the latitudinal diversity gradient (LDG; the decrease of taxonomic diversity from low towards high latitudes), using marine bivalves as a model system. Location World-wide. Methods We use the fossil record of extant and extinct bivalve taxa and information on global palaeoclimate states to evaluate how the climate state at the beginning of the evolutionary history of individual families influenced (a) their diversification dynamics through subsequent climate changes and (b) their present-day LDG. For (a), we estimated per-family genus origination and extinction rates during the last cool interval in the late Cenozoic and overall genus origination and extinction rates since the early Palaeozoic. For (b), we compared LDG slopes and oldest fossil occurrences of extant families with palaeoclimate data. We also tested whether such dynamics vary with life habits. Results Families that originated in warm intervals tend to have higher extinction rates in the (cool) late Cenozoic and occasionally in other cool intervals. However, in contrast to the results of Romdal et al. (Global Ecology and Biogeography, 2013, 22, 344-350), present-day LDG slopes do not vary with the climate state at the time of family origination, regardless of the palaeoclimatic scheme used. Infaunal living families have marginally higher origination rates in the late Cenozoic, but their LDG slopes do not differ significantly from the epifaunal families. In contrast, feeding habit appears to affect family LDG slopes, but not late Cenozoic diversification rates. Main conclusion For marine bivalves, ancestral climate state appears to influence subsequent diversification dynamics with clades originating in warm intervals showing higher extinction rates during intervals of global cooling, but ancestral climate has no detectable influence on present-day LDGs.
机译:目的以海洋双壳类为模型系统,确定地质时期的气候变化在塑造当今多样性格局(尤其是纬度多样性梯度(LDG;从低纬度到高纬度的分类学多样性的减少))中的作用。全球分布。方法我们使用现存和灭绝的双壳类生物群的化石记录以及全球古气候状态的信息来评估单个家庭进化史开始时的气候状态如何影响(a)通过随后的气候变化以及(b)他们的多样化动态。今天的LDG。对于(a),我们估计了新生代末次凉爽时期每个家庭的属起源和灭绝率,以及古生代以来的总体属起源和灭绝率。对于(b),我们将LDG斜率和现存家族中最古老的化石发生与古气候数据进行了比较。我们还测试了这种动力是否随生活习惯而变化。结果起源于温暖时期的家庭在(新生代)晚(新生代)灭绝率较高,有时在其他寒冷时期也有更高的灭绝率。但是,与Romdal等人的结果相反。 (全球生态与生物地理,2013,22,344-350),无论采用何种古气候方案,当今的LDG斜率都不会随着家庭起源时的气候状态而变化。在新生代晚期,非软体动物生活家庭的起源率略高,但他们的LDG斜率与附生动物家庭没有显着差异。相反,进食习惯似乎影响家庭LDG坡度,但不影响新生代晚期的多样化速度。主要结论对于海洋双壳类动物,祖先的气候状态似乎影响随后的多样化动态,进化枝起源于温暖的时间间隔,在全球降温期间灭绝率更高,但祖先的气候对当今的LDGs没有可检测的影响。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号