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北半球最古老的须鲸。

The oldest mysticete in the Northern Hemisphere.

机构信息

Department of Life Science and Institute of Ecology and Evolutionary Biology, National Taiwan University, Taipei 10617, Taiwan; Department of Geology, National Museum of Nature and Science, Tsukuba 305-0005, Japan.

Burke Museum of Natural History and Culture, University of Washington, Seattle, WA 98105, USA.

出版信息

Curr Biol. 2024 Apr 22;34(8):1794-1800.e3. doi: 10.1016/j.cub.2024.03.011. Epub 2024 Mar 28.

Abstract

Extant baleen whales (Mysticeti) uniquely use keratinous baleen for filter-feeding and lack dentition, but the fossil record clearly shows that "toothed" baleen whales first appeared in the Late Eocene. Globally, only two Eocene mysticetes have been found, and both are from the Southern Hemisphere: Mystacodon selenensis from Peru, 36.4 mega-annum (Ma) ago and Llanocetus denticrenatus from Antarctica, 34.2 Ma ago. Based on a partial skull from the lower part of the Lincoln Creek Formation in Washington State, USA, we describe the Northern Hemisphere's geochronologically earliest mysticete, Fucaia humilis sp. nov. Geology, biostratigraphy, and magnetostratigraphy places Fucaia humilis sp. nov. in the latest Eocene (ca. 34.5 Ma ago, near the Eocene/Oligocene transition at 33.9 Ma ago), approximately coeval with the oldest record of fossil kelps, also in the northeastern Pacific. This observation leads to our hypothesis that the origin and development of a relatively stable, nutrient-rich kelp ecosystem in the latest Eocene may have fostered the radiation of small-sized toothed mysticetes (Family Aetiocetidae) in the North Pacific basin, a stark contrast to the larger Llanocetidae (whether Mystacodon belongs to llanocetids or another independent clade remains unresolved) with the latest Eocene onset of the Antarctic Circumpolar Current in the Southern Hemisphere. Our discovery suggests that disparate mechanisms and ecological scenarios may have nurtured contrasting early mysticete evolutionary histories in the Northern and Southern hemispheres.

摘要

现存的须鲸类(长须鲸)是唯一使用角蛋白须鲸来滤食的动物,没有牙齿,但化石记录清楚地表明,“有齿”的须鲸类最早出现在始新世晚期。在全球范围内,只发现了两种始新世的须鲸,而且都来自南半球:秘鲁的 Mystacodon selenensis,距今 3640 万年前,以及来自南极洲的 Llanocetus denticrenatus,距今 3420 万年前。基于来自美国华盛顿州林肯溪组下部的部分头骨,我们描述了北半球地质年代最早的须鲸类,Fucaia humilis sp. nov. 地质学、生物地层学和磁地层学将 Fucaia humilis sp. nov. 置于始新世晚期(约 3450 万年前,在 3390 万年前的始新世/渐新世过渡附近),与东北太平洋最早的化石巨藻记录大致相同。这一观察结果使我们假设,在始新世晚期,一个相对稳定、营养丰富的巨藻生态系统的起源和发展可能促进了北太平洋盆地中小型有齿须鲸类(Aetiocetidae 科)的辐射,这与在南半球始新世晚期出现的南极环极流形成鲜明对比的是体型较大的 Lanocetidae(Mystacodon 是否属于 llanocetids 或另一个独立的分支尚未解决)。我们的发现表明,在北半球和南半球,不同的机制和生态场景可能孕育了截然不同的早期须鲸进化历史。

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