TY - JOUR
T1 - Late Miocene transformation of Mediterranean Sea biodiversity
AU - Agiadi, Konstantina
AU - Hohmann, Niklas
AU - Gliozzi, Elsa
AU - Thivaiou, Danae
AU - Bosellini, Francesca R.
AU - Taviani, Marco
AU - Bianucci, Giovanni
AU - Collareta, Alberto
AU - Londeix, Laurent
AU - Faranda, Costanza
AU - Bulian, Francesca
AU - Koskeridou, Efterpi
AU - Lozar, Francesca
AU - Mancini, Alan Maria
AU - Dominici, Stefano
AU - Moissette, Pierre
AU - Campos, Ildefonso Bajo
AU - Borghi, Enrico
AU - Iliopoulos, George
AU - Antonarakou, Assimina
AU - Kontakiotis, George
AU - Besiou, Evangelia
AU - Zarkogiannis, Stergios D.
AU - Harzhauser, Mathias
AU - Sierro, Francisco Javier
AU - Coll, Marta
AU - Vasiliev, Iuliana
AU - Camerlenghi, Angelo
AU - García-Castellanos, Daniel
N1 - Publisher Copyright:
© 2024 The Authors.
PY - 2024/9/25
Y1 - 2024/9/25
N2 - 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 to 3.6 million years (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, reflecting a high degree of reorganization of the marine ecosystem after the crisis. The results show a clear perturbation already in the pre-evaporitic Messinian (7.25 to 5.97 Ma), with patterns differing among groups and subbasins.
AB - 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 to 3.6 million years (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, reflecting a high degree of reorganization of the marine ecosystem after the crisis. The results show a clear perturbation already in the pre-evaporitic Messinian (7.25 to 5.97 Ma), with patterns differing among groups and subbasins.
UR - http://www.scopus.com/inward/record.url?scp=85204941860&partnerID=8YFLogxK
U2 - 10.1126/sciadv.adp1134
DO - 10.1126/sciadv.adp1134
M3 - Article
C2 - 39321301
AN - SCOPUS:85204941860
SN - 2375-2548
VL - 10
JO - Science advances
JF - Science advances
IS - 39
M1 - eadp1134
ER -