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全新世期间西北太平洋小齿鲸类的隐性种群更替

Hidden population turnover of small odontocetes in the northwestern North Pacific during the Holocene.

作者信息

Kishida Takushi, Sawada Kyohei, Namigata Sakiko, Takabatake Takamune, Suzuki Miwa, Takezoe Nanami, Yamamoto Takumi, Nakanishi Toshimichi, Kitagawa Hiroyuki

机构信息

College of Bioresource Sciences, Nihon University, Kameino 1866, Fujisawa, Kanagawa 252-0880, Japan.

Museum of Natural and Environmental History Shizuoka, Shizuoka 422-8017, Japan.

出版信息

Biol Lett. 2025 Jan;21(1):20240525. doi: 10.1098/rsbl.2024.0525. Epub 2025 Jan 8.

Abstract

Despite numerous studies on the rise and fall of terrestrial megafauna in the late Quaternary, knowledge about marine megafauna from this period remains limited. In this study, we performed radiocarbon dating and partial mitochondrial DNA sequencing from the skeletal remains of three species of small odontocetes (Pacific white-sided dolphins, Dall's porpoises and harbour porpoises) excavated from prehistoric archaeological sites around the Japanese shore dating back to 8500-1000 years ago (ya). Pacific white-sided dolphins that habituated the eastern coast of Hokkaido around 2000 ya belonged to different maternal groups than those from over 5000 ya and today. Furthermore, the species composition excavated from eastern Hokkaido sites varies between 5000 and 2000 ya. These findings suggest two significant population turnovers of small odontocetes on the east coast of Hokkaido, a transitional zone between the coastal area of East Asia and the offshore North Pacific. Notably, the first turnover, occurring between 5000 and 2000 ya, represents the oldest evidence of local population turnovers of marine megafauna during the late Quaternary.

摘要

尽管对第四纪晚期陆地巨型动物的兴衰进行了大量研究,但关于这一时期海洋巨型动物的知识仍然有限。在本研究中,我们对从日本海岸周围可追溯到8500 - 1000年前(ya)的史前考古遗址挖掘出的三种小型齿鲸(太平洋白侧海豚、白腰鼠海豚和港湾鼠海豚)的骨骼遗骸进行了放射性碳年代测定和部分线粒体DNA测序。约2000 ya时栖息在北海道东海岸的太平洋白侧海豚与5000 ya以上及现今的海豚属于不同的母系群体。此外,从北海道东部遗址挖掘出的物种组成在5000 ya至2000 ya之间有所不同。这些发现表明,在北海道东海岸这个东亚沿海地区与北太平洋近海的过渡地带,小型齿鲸出现了两次重大的种群更替。值得注意的是,第一次更替发生在5000 ya至2000 ya之间,是第四纪晚期海洋巨型动物局部种群更替的最古老证据。

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