4.2 Article

A new species of Kolpochoerus (Mammalia: Suidae) from the Pliocene of Central Afar, Ethiopia: Its Taxonomy and Phylogenetic Relationships

Journal

JOURNAL OF MAMMALIAN EVOLUTION
Volume 20, Issue 2, Pages 115-127

Publisher

SPRINGER
DOI: 10.1007/s10914-012-9207-0

Keywords

Suinae; Kolpochoerus; Taxonomy; Phylogeny; Phyletic evolution; Woranso-Mille; Gona; Pliocene; Ethiopia

Funding

  1. National Science Foundation [BCS-0234320, BCS-0542037]
  2. Leakey Foundation
  3. National Geographic Society
  4. Wenner-Gren Foundation
  5. Direct For Social, Behav & Economic Scie
  6. Division Of Behavioral and Cognitive Sci [1125157] Funding Source: National Science Foundation
  7. Division Of Behavioral and Cognitive Sci
  8. Direct For Social, Behav & Economic Scie [1125345, 1124705] Funding Source: National Science Foundation

Ask authors/readers for more resources

Kolpochoerus (Mammalia: Suidae) is a suine genus represented by a number of species from Plio-Pleistocene sites in Africa. While the general trends in Kolpochoerus evolution are broadly known, gaps in the fossil record preclude an understanding of the details of its evolutionary tempo and mode. Here, we describe a new species, Kolpochoerus millensis, based on new fossil material from the Woranso-Mille and Gona sites in the Central Afar region of Ethiopia and dated to 3.5-3.8 million years ago (Ma). Third molars of K. millensis are metrically and morphologically intermediate between the early Pliocene K. deheinzelini and earliest late Pliocene K. afarensis. It appears that K. deheinzelini, K. millensis, and K. afarensis are temporally disjunct and phenetically distinguishable parts of a single evolving lineage. The recognition of these chronospecies provides additional evidence for anagenetic evolution. It demonstrates clearly the presence of transitional forms in the fossil record. The extensive and well-dated Kolpochoerus fossil record serves as one of the best documented examples of the occurrence of phyletic evolution. Moreover, K. millensis is one of the best biochronological markers in eastern Africa for the time between 3.5 and 3.8 Ma.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.2
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available