Time-calibrated molecular phylogeny of pteropods

PLoS One. 2017 Jun 12;12(6):e0177325. doi: 10.1371/journal.pone.0177325. eCollection 2017.

Abstract

Pteropods are a widespread group of holoplanktonic gastropod molluscs and are uniquely suitable for study of long-term evolutionary processes in the open ocean because they are the only living metazoan plankton with a good fossil record. Pteropods have been proposed as bioindicators to monitor the impacts of ocean acidification and in consequence have attracted considerable research interest, however, a robust evolutionary framework for the group is still lacking. Here we reconstruct their phylogenetic relationships and examine the evolutionary history of pteropods based on combined analyses of Cytochrome Oxidase I, 28S, and 18S ribosomal rRNA sequences and a molecular clock calibrated using fossils and the estimated timing of the formation of the Isthmus of Panama. Euthecosomes with uncoiled shells were monophyletic with Creseis as the earliest diverging lineage, estimated at 41-38 million years ago (mya). The coiled euthecosomes (Limacina, Heliconoides, Thielea) were not monophyletic contrary to the accepted morphology-based taxonomy; however, due to their high rate heterogeneity no firm conclusions can be drawn. We found strong support for monophyly of most euthecosome genera, but Clio appeared as a polyphyletic group, and Diacavolinia grouped within Cavolinia, making the latter genus paraphyletic. The highest evolutionary rates were observed in Heliconoides inflatus and Limacina bulimoides for both 28S and 18S partitions. Using a fossil-calibrated phylogeny that sets the first occurrence of coiled euthecosomes at 79-66 mya, we estimate that uncoiled euthecosomes evolved 51-42 mya and that most extant uncoiled genera originated 40-15 mya. These findings are congruent with a molecular clock analysis using the Isthmus of Panama formation as an independent calibration. Although not all phylogenetic relationships could be resolved based on three molecular markers, this study provides a useful resource to study pteropod diversity and provides general insight into the processes that generate and maintain their diversity in the open ocean.

MeSH terms

  • Animals
  • Computational Biology / methods
  • DNA Barcoding, Taxonomic
  • Evolution, Molecular*
  • Fossils
  • Gastropoda / classification*
  • Gastropoda / genetics*
  • Genes, Mitochondrial
  • Geography
  • Panama
  • Phylogeny*
  • Sequence Analysis, DNA

Grants and funding

This work was supported by a Netherlands Organisation for Scientific Research (NWO) cruise participation grant, Veni and Vidi grants 863.08.024 and 016.161351 (http://www.nwo.nl), respectively, to K.T.C.A. Peijnenburg. M. Hughes was supported by the Natural History Museum of London / Imperial College Biosystematics Mres programme and John Templeton Foundation grant 43915 (https://www.templeton.org). S.L. Bush was funded by the Smithsonian Women’s Committee grants and Smithsonian research funds to K.J. Osborn, and the Monterey Bay Aquarium. The David and Lucile Packard Foundation provided funding for numerous cruises to the Monterey Bay Aquarium Research Institute in which K.J. Osborn and S.L. Bush participated. Plankton collections for this study were (partially) supported by National Science Foundation (USA) grants OCE-1230900 to the UNOLS Training Program and OCE-1029478 and OCE-1338959 (https://www.nsf.gov) to E. Goetze, National Ocean and Atmospheric Administration’s Northeast Fisheries Science Center to NOAA/National Marine Fisheries Service and M. Vecchione, and the UK Natural Environmental Research Council National Capability funding to Plymouth Marine Laboratory and the National Oceanography Centre, Southampton. Funding for SEAMAP surveys was provided by NOAA. This is contribution number 308 of the Atlantic Meridional Transect Programme. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.