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古生物学和现代生物学数据的结合表明,由于环境变化的影响,长尾鲨形目鲨鱼的多样化过程可能出现了延迟爆发。

Combining palaeontological and neontological data shows a delayed diversification burst of carcharhiniform sharks likely mediated by environmental change.

机构信息

Institut des Sciences de l'Evolution de Montpellier, CNRS, IRD, EPHE, Université de Montpellier, 34095, Montpellier, France.

出版信息

Sci Rep. 2022 Dec 19;12(1):21906. doi: 10.1038/s41598-022-26010-7.

DOI:10.1038/s41598-022-26010-7
PMID:36535995
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9763247/
Abstract

Estimating deep-time species-level diversification processes remains challenging. Both the fossil record and molecular phylogenies allow the estimation of speciation and extinction rates, but each type of data may still provide an incomplete picture of diversification dynamics. Here, we combine species-level palaeontological (fossil occurrences) and neontological (molecular phylogenies) data to estimate deep-time diversity dynamics through process-based birth-death models for Carcharhiniformes, the most speciose shark order today. Despite their abundant fossil record dating back to the Middle Jurassic, only a small fraction of extant carcharhiniform species is recorded as fossils, which impedes relying only on the fossil record to study their recent diversification. Combining fossil and phylogenetic data, we recover a complex evolutionary history for carcharhiniforms, exemplified by several variations in diversification rates with an early low diversity period followed by a Cenozoic radiation. We further reveal a burst of diversification in the last 30 million years, which is partially recorded with fossil data only. We also find that reef expansion and temperature change can explain variations in speciation and extinction through time. These results pinpoint the primordial importance of these environmental variables in the evolution of marine clades. Our study also highlights the benefit of combining the fossil record with phylogenetic data to address macroevolutionary questions.

摘要

估算深层物种级别的多样化过程仍然具有挑战性。化石记录和分子系统发育都可以估计物种形成和灭绝率,但每种类型的数据可能仍然提供了多样化动态的不完整图景。在这里,我们结合了物种水平的古生物学(化石出现)和新生学(分子系统发育)数据,通过基于过程的出生-死亡模型来估算当今最具物种多样性的鲨鱼目——角鲨目的深层时间多样性动态。尽管它们的化石记录可以追溯到中侏罗世,但现存的角鲨目物种只有一小部分被记录为化石,这阻碍了仅依靠化石记录来研究它们最近的多样化。结合化石和系统发育数据,我们为角鲨目恢复了一个复杂的进化历史,其多样化率的几次变化就是例证,早期的多样性较低,然后是新生代辐射。我们进一步揭示了过去 3000 万年的多样化爆发,其中只有部分是仅用化石数据记录的。我们还发现,珊瑚礁扩张和温度变化可以通过时间来解释物种形成和灭绝的变化。这些结果突显了这些环境变量在海洋类群进化中的原始重要性。我们的研究还强调了将化石记录与系统发育数据相结合来解决宏观进化问题的好处。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/29a2d4f8417b/41598_2022_26010_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/7c8e59266024/41598_2022_26010_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/10816a90d13b/41598_2022_26010_Fig2_HTML.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/6b487ac575ab/41598_2022_26010_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/a9efbd8c042b/41598_2022_26010_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/daceb06d9c5d/41598_2022_26010_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/29a2d4f8417b/41598_2022_26010_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/7c8e59266024/41598_2022_26010_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/10816a90d13b/41598_2022_26010_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/984d604bf7ea/41598_2022_26010_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/de0b1a0fc45d/41598_2022_26010_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/6b487ac575ab/41598_2022_26010_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/a9efbd8c042b/41598_2022_26010_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/daceb06d9c5d/41598_2022_26010_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/61e3/9763247/29a2d4f8417b/41598_2022_26010_Fig8_HTML.jpg

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