Villafaña Jaime A, Rivadeneira Marcelo M, Pimiento Catalina, Kriwet Jürgen
Vienna Doctoral School of Ecology and Evolution, Vienna, Austria; Centro de Investigación en Recursos Naturales y Sustentabilidad, Universidad Bernardo O'Higgins, Avenida Viel 1497, 8370993 Santiago, Chile.
Laboratorio de Paleobiología, Centro de Estudios Avanzados en Zonas Áridas (CEAZA), Avenida Bernardo Ossandón 877, 1781681, Coquimbo, Chile; Departamento de Biología Marina, Facultad de Ciencias del Mar, Universidad Católica del Norte, Larrondo 1281, Coquimbo, Chile; Departamento de Biología, Universidad de La Serena, Avenida Raul Bitrán 1305, La Serena, Chile.
Paleobiology. 2023 May;49(2):329-341. doi: 10.1017/pab.2022.40. Epub 2023 Feb 8.
Despite the rich fossil record of Neogene chondrichthyans (chimaeras, sharks, rays, and skates) from Europe, little is known about the macroevolutionary processes that generated their current diversity and geographical distribution. We compiled 4368 Neogene occurrences comprising 102 genera, 41 families, and 12 orders from four European regions (Atlantic, Mediterranean, North Sea, and Paratethys) and evaluated their diversification trajectories and paleobiogeographic patterns. In all regions analyzed, we found that generic richness increased during the early Miocene, then decreased sharply during the middle Miocene in the Paratethys, and moderately during the late Miocene and Pliocene in the Mediterranean and North Seas. Origination rates display the most significant pulses in the early Miocene in all regions. Extinction rate pulses varied across regions, with the Paratethys displaying the most significant pulses during the late Miocene and the Mediterranean and North Seas during the late Miocene and early Pliocene. Overall, up to 27% and 56% of the European Neogene genera are now globally and regionally extinct, respectively. The observed pulses of origination and extinction in the different regions coincide with warming and cooling events that occurred during the Neogene globally and regionally. Our study reveals complex diversity dynamics of Neogene chondrichthyans from Europe and their distinct biogeographic composition despite the multiple marine passages that connected the different marine regions during this time.
尽管欧洲新近纪软骨鱼类(银鲛、鲨鱼、鳐鱼和魟)拥有丰富的化石记录,但对于产生其当前多样性和地理分布的宏观进化过程却知之甚少。我们汇总了来自欧洲四个地区(大西洋、地中海、北海和副特提斯海)的4368个新近纪化石记录,涵盖102个属、41个科和12个目,并评估了它们的多样化轨迹和古生物地理模式。在所有分析的地区中,我们发现属的丰富度在中新世早期增加,然后在副特提斯海的中新世中期急剧下降,而在地中海和北海的中新世晚期和上新世则适度下降。在所有地区,起源率在中新世早期显示出最显著的峰值。灭绝率峰值在不同地区有所不同,副特提斯海在中新世晚期显示出最显著的峰值,而地中海和北海在中新世晚期和上新世早期显示出最显著的峰值。总体而言,欧洲新近纪属中分别有高达27%和56%现已在全球和区域灭绝。在不同地区观察到的起源和灭绝峰值与新近纪全球和区域发生的变暖和变冷事件相吻合。我们的研究揭示了欧洲新近纪软骨鱼类复杂的多样性动态及其独特的生物地理组成,尽管在此期间不同海洋区域之间有多个海洋通道相连。