Synchronous diversification of Sulawesi’s iconic artiodactyls driven by recent geological events
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Frantz, Laurent A. F.; Rudzinski, Anna; Nugraha, Abang Mansyursyah Surya; Evin, Allowen; Burton, James; Hulme-Beaman, Ardern; Linderholm, Anna; Barnett, Ross; Vega, Rodrigo; Irving-Pease, Evan K.; Haile, James; Allen, Richard; Leus, Kristin; Shephard, Jill; Hillyer, Mia; Gillemot, Sarah; van den Hurk, Jeroen; Ogle, Sharron; Atofanei, Cristina; Thomas, Mark G.; Johansson, Friederike; Mustari, Abdul Haris; Williams, John; Mohamad, Kusdiantoro; Damayanti, Chandramaya Siska; Wiryadi, Ita Djuwita; Obbles, Dagmar; Mona, Stephano; Day, Hally; Yasin, Muhammad; Meker, Stefan; McGuire, Jimmy A.; Evans, Ben J.; von Rintelen, Thomas; Ho, Simon Y. W.; Searle, J. B.; Kitchener, Andrew C.; Macdonald, Alastair A.; Shaw, Darren J.; Hall, Robert; Galbusera, Peter; Larson, Greger
The high degree of endemism on Sulawesi has previously been suggested to have vicariant origins, dating back to 40 Ma. Recent studies, however, suggest that much of Sulawesi's fauna assembled over the last 15 Myr. Here, we test the hypothesis that more recent uplift of previously submerged portions of land on Sulawesi promoted diversification and that much of its faunal assemblage is much younger than the island itself. To do so, we combined palaeogeographical reconstructions with genetic and morphometric datasets derived from Sulawesi's three largest mammals: the babirusa, anoa and Sulawesi warty pig. Our results indicate that although these species most likely colonized the area that is now Sulawesi at different times (14 Ma to 2–3 Ma), they experienced an almost synchronous expansion from the central part of the island. Geological reconstructions indicate that this area was above sea level for most of the last 4 Myr, unlike most parts of the island. We conclude that emergence of land on Sulawesi (approx. 1–2 Myr) may have allowed species to expand synchronously. Altogether, our results indicate that the establishment of the highly endemic faunal assemblage on Sulawesi was driven by geological events over the last few million years.
L.A.F.F., J.H., A.L., A.H.-B. and G.L. were supported by a European Research Council grant (ERC-2013-StG-337574-UNDEAD) and Natural Environmental Research Council grants (NE/K005243/1 and NE/K003259/1). L.A.F.F. was supported by a Junior Research Fellowship (Wolfson College, University of Oxford) and a Wellcome Trust grant (210119/Z/18/Z). P.G., S.G., J.v.d.H., C.A. and D.O. were supported by Flemish government structural funding. A.R. was supported by a Marie Curie Initial Training Network (BEAN—Bridging the European and Anatolian Neolithic, GA no. 289966) awarded to M.G.T. M.G.T. is supported by a Wellcome Trust Senior Research Fellowship (GA no. 100719/Z/12/Z). B.J.E. was supported by the Natural Science and Engineering Research Council of Canada. This work received additional support from the University of Edinburgh Development Trust, the Roslin Institute, the Balloch Trust and the Stichting Dierentuin Helpen (Consortium of Dutch Zoos). Additional support was also provided by the Rufford Small Grant, Royal Geographical Society, London, the Royal Zoological Society of Scotland and the University of Edinburgh Birrell-Gray Travel Award.
The Royal Society
biogeography; evolution; geology; Wallacea
Previously Published As
Proc. R. Soc. B (2018) 285: 20172566