FN Archimer Export Format
PT J
TI Limited dispersal and in situ diversification drive the evolutionary history of Rasborinae fishes in Sundaland
BT 
AF Sholihah, Arni
   Delrieu‐Trottin, Erwan
   Sukmono, Tedjo
   Dahruddin, Hadi
   Pouzadoux, Juliette
   Tilak, Marie‐Ka
   Fitriana, Yuli
   Agnèse, Jean‐François
   Condamine, Fabien L.
   Wowor, Daisy
   Rüber, Lukas
   Hubert, Nicolas
AS 1:1,2;2:1,3;3:4;4:5;5:1,6;6:1;7:5;8:1;9:1;10:5;11:7,8;12:1;
FF 1:;2:;3:;4:;5:PDG-RBE-IHPE;6:;7:;8:;9:;10:;11:;12:;
C1 UMR 5554 ISEM (IRD, UM, CNRS, EPHE) Université de Montpellier Montpellier, France
   School of Life Sciences and Technology Institut Teknologi Bandung Bandung ,Indonesia
   Museum für Naturkunde Leibniz‐Institut für Evolutions und Biodiversitätsforschung an der Humboldt‐Universität zu Berlin Berlin, Germany
   Department of Biology Universitas Jambi Jambi, Indonesia
   Division of Zoology Research Center for Biology Indonesian Institute of Sciences (LIPI) Cibinong ,Indonesia
   UMR 5244 IHPE (CNRS, IFREMER, UM, UPVD) Université de Montpellier Montpellier, France
   Naturhistorisches Museum Bern Bern ,Switzerland
   Aquatic Ecology and Evolution Institute of Ecology and Evolution University of Bern Bern,Switzerland
C2 IRD, FRANCE
   INST TEKNOL BANDUNG, INDONESIA
   LEIBNIZ INST EVOL BIODIVERS SCI, GERMANY
   UNIV JAMBI, INDONESIA
   LIPI, INDONESIA
   IFREMER, FRANCE
   NATURHISTORISCHES MUSEUM, SWITZERLAND
   UNIV BERN, SWITZERLAND
SI MONTPELLIER
SE PDG-RBE-IHPE
UM IHPE
IN WOS Ifremer UMR
   copubli-france
   copubli-p187
   copubli-europe
   copubli-int-hors-europe
   copubli-sud
IF 4.81
TC 9
UR https://archimer.ifremer.fr/doc/00700/81221/93577.pdf
LA English
DT Article
DE ;ancestral areas estimation;cryptic diversity;dispersal pathways;diversification models;historical biogeography;mitogenomes;phylogenetic reconstructions;Pleistocene climatic fluctuations;sea levels
AB Aim Sea-level changes have long been put forward to explain the colonization of Southeast Asian islands by freshwater aquatic organisms. We examined the relative impact of Sundaland geology since the Oligocene and of Pleistocene Eustatic Fluctuations on the mitochondrial lineage diversification of a species-rich subfamily of freshwater fishes widely distributed in Southeast Asia. We specifically tested if the expansion of exposed lands and increased island connectivity during Pleistocene low sea levels (the paleoriver hypothesis) induced bursts of diversification. Location Sundaland. Taxon Rasborinae (Actinopterygii, Cypriniformes, Danionidae). Methods We aggregated 1,017 cytochrome oxidase I sequences and 79 mitogenomes to delineate Molecular Operational Taxonomic Units (MOTUs) and further reconstruct a time-calibrated phylogeny of Rasborinae. Ancestral area estimations were conducted using both island and paleoriver partitioning to examine the impact of island connectivity during Pleistocene sea-level changes on dispersal. Temporal trends of diversification are explored through statistical selection of best-fit models. Results The origin of Sundaland mitochondrial lineages is dated at c. 33 Ma and four major clades are identified, which diversified between c. 31 and 22 Ma. The Island of Borneo and North Sunda paleoriver are identified as the source of Sundaland Rasborinae. Geographical patterns of lineage divergence indicate that most divergence events occurred within islands and diversification under constant birth rate models are the most likely for all clades. Conclusions The geographical and historical context of diversification of mitochondrial lineages in Rasborinae provides little support for the paleoriver hypothesis. The onset of isolation of Borneo from mainland Asia triggered the initial diversification of the group (c. 31–22 Ma). The late colonization of Java and Sumatra occurred through several independent dispersal events, poorly explained by Pleistocene sea-level changes and frequently followed by in situ diversification. 
PY 2021
PD SEP
SO Journal Of Biogeography
SN 0305-0270
PU Wiley
VL 48
IS 9
UT 000662971800001
BP 2153
EP 2173
DI 10.1111/jbi.14141
ID 81221
ER

EF