Abstract

After evolving in Africa at the close of the Miocene, mammoths (Mammuthus sp.) spread through much of the northern hemisphere, diversifying morphologically as they entered various habitats. Paleontologically, these morphs are conventionally recognized as species. In Pleistocene North America alone, several mammoth species have been recognized, inhabiting environments as different as cold tundra-steppe in the north and the arid grasslands or temperate savanna-parklands of the south. Yet mammoth phylogeographic studies have overwhelmingly focused on permafrost-preserved remains of only one of these species, Mammuthus primigenius (woolly mammoth). Here we challenge this bias by performing a geographically and taxonomically wide survey of mammoth genetic diversity across North America. Using a targeted enrichment technique, we sequenced 67 complete mitochondrial genomes from non-primigenius specimens representing M. columbi (Columbian mammoth), M. jeffersonii (Jeffersonian mammoth), and M. exilis (pygmy mammoth), including specimens from contexts not generally associated with good DNA preservation. While we uncovered clear phylogeographic structure in mammoth matrilines, their phylogeny as recovered from mitochondrial DNA is not compatible with existing systematic interpretations of their paleontological record. Instead, our results strongly suggest that various nominal mammoth species interbred, perhaps extensively. We hypothesize that at least two distinct stages of interbreeding between conventional paleontological species are likely responsible for this pattern – one between Siberian woolly mammoths and resident American populations that introduced woolly mammoth phenotypes to the continent, and another between ecomorphologically distinct populations of woolly and Columbian mammoths in North America south of the ice.

Highlights

  • The conventional dual-source view of New World mammoth evolution (Harington, 1984; Agenbroad, 2005; Fisher, 2009; Saunders et al, 2010) holds that the Late Pleistocene diversity originated from two distinct, differently adapted ancestral lineages

  • Assuming that Columbian mammoths descended from an early Irvingtonian immigrant to North America (Agenbroad, 2005; Lister and Bahn, 2007), putatively M. trogontherii according to the single-source hypothesis (Lister and Sher, 2015), and that the pattern of diversity points to a North American origin of Clade I, we find that the most parsimonious reconciliation of the genetic evidence with the paleontological record requires the conclusion that the mitochondrial to most recent common ancestry (tMRCAs) is much more ancient than a tips-only calibration scheme would estimate

  • By confirming that Columbian mammoths most likely descended from the same matrilines that were previously observed in woolly mammoths, we provide evidence supporting an ancient chronology for both this and our previous concept of mammoth mitogenomic phylogeny

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Summary

Introduction

The conventional dual-source view of New World mammoth evolution (Harington, 1984; Agenbroad, 2005; Fisher, 2009; Saunders et al, 2010) holds that the Late Pleistocene diversity originated from two distinct, differently adapted ancestral lineages (or species). During the early Irvingtonian North American Land Mammal Age (NALMA), 1.8–0.24 Ma, the primitive species Mammuthus meridionalis (southern mammoth) entered North America over the Bering Land Bridge. From this source arose the Columbian mammoth, Mammuthus columbi, a widespread species adapted to mid-continental parklands and grasslands, together with perhaps one or two other more specialized taxa (Mammuthus exilis, Channel Islands pygmy mammoth, and the eastern woodlands Mammuthus jeffersonii, Jefferson’s mammoth). In western Beringia (Chukotka), a different primitive species, cold-adapted Mammuthus trogontherii (steppe mammoth), evolved into the woolly mammoth (Mammuthus primigenius), which first entered northwestern North America during the early Rancholabrean NALMA, 0.125–0.011 Ma. Thereafter, woolly mammoths progressively moved southward along steppe habitats bordering the Laurentide ice sheet, eventually reaching the present-day Great Lakes region and Atlantic Coast. Despite their success in expanding into almost every habitable region within Late Pleistocene North America, all mammoth species were extinct by the start of the Holocene or shortly thereafter (Haile et al, 2009)

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