Evidence map›Paper›PMID 29141036›Full record

ArticlePloS one2017

The disjunct pattern of the Neotropical harvestman Discocyrtus dilatatus (Gonyleptidae) explained by climate-driven range shifts in the Quaternary: Paleodistributional and molecular evidence.

Julia Vergara, Luis E Acosta, Raúl E González-Ittig, Luis M Vaschetto, Cristina N Gardenal

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Article in PloS one, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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3 · Its place in the literature

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4 · The record

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5 · Who and what money

Authors and funding

5 authors.

Julia VergaraInstituto de Diversidad y Ecología Animal (IDEA), CONICET-Universidad Nacional de Córdoba, Argentina.
Luis E AcostaInstituto de Diversidad y Ecología Animal (IDEA), CONICET-Universidad Nacional de Córdoba, Argentina.ORCID http://orcid.org/0000-0003-3107-1349
Raúl E González-IttigInstituto de Diversidad y Ecología Animal (IDEA), CONICET-Universidad Nacional de Córdoba, Argentina.
Luis M VaschettoInstituto de Diversidad y Ecología Animal (IDEA), CONICET-Universidad Nacional de Córdoba, Argentina.
Cristina N GardenalInstituto de Diversidad y Ecología Animal (IDEA), CONICET-Universidad Nacional de Córdoba, Argentina.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The disjunct distribution of the harvestman Discocyrtus dilatatus (Opiliones, Gonyleptidae) is used as a case study to test the hypothesis of a trans-Chaco Pleistocene paleobridge during range expansion stages. This would have temporarily connected humid regions ('Mesopotamia' in northeastern Argentina, and the 'Yungas' in the northwest, NWA) in the subtropical and temperate South American lowlands. The present study combines two independent approaches: paleodistributional reconstruction, using the Species Distribution Modeling method MaxEnt and projection onto Quaternary paleoclimates (6 kya, 21 kya, 130 kya), and phylogeographic analyses based on the cytochrome oxidase subunit I molecular marker. Models predict a maximal shrinkage during the warm Last Interglacial (130 kya), and the rise of the hypothesized paleobridge in the Last Glacial Maximum (21 kya), revealing that cold-dry stages (not warm-humid ones, as supposed) enabled the range expansion of this species. The disjunction was formed in the mid-Holocene (6 kya) and is intensified under current conditions. The median-joining network shows that NWA haplotypes are peripherally related to different Mesopotamian lineages; haplotypes from Santa Fe and Córdoba Provinces consistently occupy central positions in the network. According to the dated phylogeny, Mesopotamia-NWA expansion events would have occurred in the last glacial period, in many cases closely associated to the Last Glacial Maximum, with most divergence events occurring shortly thereafter. Only two (out of nine) NWA haplotypes are shared with Mesopotamian localities. A single, presumably relictual NWA haplotype was found to have diverged much earlier, suggesting an ancient expansion event not recoverable by the paleodistributional models. Different measures of sequence statistics, genetic diversity, population structure and history of demographic changes are provided. This research offers the first available evidence for the historical origin of NWA disjunct populations of a Mesopotamian harvestman.

Indexed as

Climate ChangeAnimalsArachnidaModels, TheoreticalPaleontologyPhylogeny

Identifiers

PMID29141036
PMCPMC5687770

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