Worldwide genotyping in the planktonic foraminifer Globoconella inflata: implications for life history and paleoceanography

• Published in: PloS one 2011-10, Vol.6 (10), p.e26665-e26665
• Main Authors: Morard, Raphaël, Quillévéré, Frédéric, Douady, Christophe J, de Vargas, Colomban, de Garidel-Thoron, Thibault, Escarguel, Gilles
• Format: Article
• Language: English
• Subjects: Antarctic front; Biogeography; Biology; Biometry; Cryptic species; Data analysis; Datasets; Datum (elevation); DNA, Ribosomal Spacer - genetics; Earth Sciences; Environmental science; Environmental Sciences; Evolution; Foraminifera - classification; Foraminifera - genetics; Fossils; Genetic aspects; Genetic diversity; Genetic Variation - genetics; Genotypes; Genotyping; Genotyping Techniques; Globoconella inflata; Hemispheres; Internationality; Life history; Molecular biology; Morphology; Oceans and Seas; Paleoceanography; Paleontology; Phylogenetics; Phylogeny; Phylogeography; Plankton; Plankton - classification; Plankton - genetics; Pleistocene; Pliocene; Polar environments; Ribosomal DNA; Sciences of the Universe; Seasonal variations; Sediments; Software packages; Speciation; Species; Stratigraphy; Studies; Subtropical zones
• ISSN: 1932-6203; 1932-6203
• DOI: 10.1371/journal.pone.0026665

The planktonic foraminiferal morpho-species Globoconella inflata is widely used as a stratigraphic and paleoceanographic index. While G. inflata was until now regarded as a single species, we show that it rather constitutes a complex of two pseudo-cryptic species. Our study is based on SSU and ITS rDNA sequence analyses and genotyping of 497 individuals collected at 49 oceanic stations covering the worldwide range of the morpho-species. Phylogenetic analyses unveil the presence of two divergent genotypes. Type I inhabits transitional and subtropical waters of both hemispheres, while Type II is restricted to the Antarctic subpolar waters. The two genetic species exhibit a strictly allopatric distribution on each side of the Antarctic Subpolar Front. On the other hand, sediment data show that G. inflata was restricted to transitional and subtropical environments since the early Pliocene, and expanded its geographic range to southern subpolar waters ∼700 kyrs ago, during marine isotopic stage 17. This datum may correspond to a peripatric speciation event that led to the partition of an ancestral genotype into two distinct evolutionary units. Biometric measurements performed on individual G. inflata from plankton tows north and south of the Antarctic Subpolar Front indicate that Types I and II display slight but significant differences in shell morphology. These morphological differences may allow recognition of the G. inflata pseudo-cryptic species back into the fossil record, which in turn may contribute to monitor past movements of the Antarctic Subpolar Front during the middle and late Pleistocene.