Late Miocene transformation of Mediterranean Sea biodiversity

Konstantina Agiadi, Niklas Hohmann, Elsa Gliozzi, Danae Thivaiou, Francesca Bosellini, Marco Taviani, Giovanni Bianucci, Alberto Collareta, Laurent Londeix, Costanza Faranda, Francesca Bulian, Efterpi Koskeridou, Francesca Lozar, Alan Maria Mancini, Stefano Dominici, Pierre Moissette, Ildefonso Bajo Campos, Enrico Borghi, George Iliopoulos, Assimina Antonarakou, George Kontakiotis, Evangelia Besiou, Stergios D. Zarkogiannis, Mathias Harzhauser, Francisco Javier Sierro, Marta Coll, Iuliana Vasiliev, Angelo Camerlenghi, Daniel Garcia-Castellanos
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Abstract

Understanding deep-time marine biodiversity change under the combined effects of climate and connectivity changes is fundamental for predicting the impacts of modern climate change in semi-enclosed seas. We quantify the Late Miocene-Early Pliocene (11.63-3.6 Ma) taxonomic diversity of the Mediterranean Sea for calcareous nannoplankton, dinocysts, foraminifera, ostracods, corals, molluscs, bryozoans, echinoids, fishes, and marine mammals. During this time, marine biota was affected by global climate cooling and the restriction of the Mediterranean's connection to the Atlantic Ocean that peaked with the Messinian Salinity Crisis. Although the net change in species richness from the Tortonian to the Zanclean varies by group, species turnover is greater than 30% in all cases. The results show clear perturbation already in the pre-evaporitic Messinian (7.25-5.97 Ma), with patterns differing among groups and sub-basins.
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中新世晚期地中海生物多样性的转变
了解气候和连通性变化共同作用下的深时海洋生物多样性变化,对于预测现代气候变化对半封闭海域的影响至关重要。我们对地中海晚中新世-早上新世(11.63-3.6 Ma)的钙质浮游动物、恐龙囊虫、有孔虫、桡足类动物、珊瑚、软体动物、浮游动物、回声类动物、鱼类和海洋哺乳动物的分类多样性进行了量化。在此期间,海洋生物区系受到全球气候变冷和地中海与大西洋连接受限的影响,这种影响在梅西尼亚盐度危机中达到顶峰。虽然从托尔托尼到赞克利时期物种丰富度的净变化因群而异,但在所有情况下,物种更替率都超过了 30%。结果表明,在前蒸发期的梅西尼亚(7.25-5.97 Ma)就已经出现了明显的扰动,各组和各亚盆地的模式也不尽相同。
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