Abstract

Carex subgenus Psyllophorae is an engaging study group due to its early diversification compared to most Carex lineages, and its remarkable disjunct distribution in four continents corresponding to three independent sections: sect. Psyllophorae in Western Palearctic, sect. Schoenoxiphium in Afrotropical region, and sect. Junciformes in South America (SA) and SW Pacific. The latter section is mainly distributed in Patagonia and the Andes, where it is one of the few Carex groups with a significant in situ diversification. We assess the role of historical geo-climatic events in the evolutionary history of the group, particularly intercontinental colonization events and diversification processes, with an emphasis on SA. We performed an integrative study using phylogenetic (four DNA regions), divergence times, diversification rates, biogeographic reconstruction, and bioclimatic niche evolution analyses. The crown age of subg. Psyllophorae (early Miocene) supports this lineage as one of the oldest within Carex. The diversification rate probably decreased over time in the whole subgenus. Geography seems to have played a primary role in the diversification of subg. Psyllophorae. Inferred divergence times imply a diversification scenario away from primary Gondwanan vicariance hypotheses and suggest long-distance dispersal-mediated allopatric diversification. Section Junciformes remained in Northern Patagonia since its divergence until Plio-Pleistocene glaciations. Andean orogeny appears to have acted as a northward corridor, which contrasts with the general pattern of North-to-South migration for temperate-adapted organisms. A striking niche conservatism characterizes the evolution of this section. Colonization of the SW Pacific took place on a single long-distance dispersal event from SA. The little ecological changes involved in the trans-Pacific disjunction imply the preadaptation of the group prior to the colonization of the SW Pacific. The high species number of the section results from simple accumulation of morphological changes (disparification), rather than shifts in ecological niche related to increased diversification rates (radiation).

Highlights

  • The Neotropic is one of the most biodiverse regions, containing seven of the 36 currently recognized biodiversity hotspots of Earth (Koenig, 2016), and is considered an evolutionary hub for research about the origin of biological diversity (Rull, 2008)

  • The present study provides new insights into the biogeographic and diversification patterns of the Southern Hemisphere and in particular Patagonia, one of the least studied areas of South America (SA)

  • The early diversification of the latter section involved the differentiation of a group of species mostly restricted to a single landmass (SA), with its diversity centre in N Patagonia and a single direct long-distance dispersal (LDD) to SW Pacific

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Summary

Introduction

The Neotropic is one of the most biodiverse regions, containing seven of the 36 currently recognized biodiversity hotspots of Earth (Koenig, 2016), and is considered an evolutionary hub for research about the origin of biological diversity (Rull, 2008). This involves taxa distributed at medium and high latitudes of both the hemispheres It has mainly been explained through long-distance dispersal (LDD) likely by birds and dated back to cold periods of the Plio-Pleistocene (Simpson et al, 2005, 2017; Spalik et al, 2010; Villaverde et al, 2017a). Another less explored pattern is the trans-Caribbean disjunction. Recent molecular dating studies have confirmed that LDD explains some of the Gondwanan distribution patterns better than vicariance-like scenarios, especially in plants (McGlone et al, 2001; Sanmartín and Ronquist, 2004). Just a few groups of ancient (Cretaceous) origin seem to have Gondwanan distributions explained by tectonic vicariance, such as Araucariaceae (Biffin et al, 2010; Kranitz et al, 2014)

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