Phylogeographic analysis of the red seaweed Palmaria palmata reveals a Pleistocene marine glacial refugium in the English Channel

• Published in: Molecular Ecology
• Main Authors: Provan, Jim, Wattier, Remi, A, Maggs, Christine, A
• Other Authors: Queen's University Belfast (QUB), Biogéosciences UMR 6282 (BGS), Université de Bourgogne (UB)-Centre National de la Recherche Scientifique (CNRS)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2005
• Subjects: cox 2-3 glacial refugia ITS Palmaria palmata phylogeography plastid; cox 2-3; glacial refugia; ITS; Palmaria palmata; phylogeography; plastid; [SDV]Life Sciences [q-bio]; Hurd; Iceland; North Atlantic
• Online Access: https://u-bourgogne.hal.science/hal-04345183; https://u-bourgogne.hal.science/hal-04345183/document; https://u-bourgogne.hal.science/hal-04345183/file/P12-Provan-Palpal-ME-2005.pdf; https://doi.org/10.1111/j.1365-294x.2005.02447.x

Phylogeography has provided a new approach to the analysis of the postglacial history of a wide range of taxa but, to date, little is known about the effect of glacial periods on the marine biota of Europe. We have utilized a combination of nuclear, plastid and mitochondrial genetic markers to study the biogeographic history of the red seaweed Palmaria palmata in the North Atlantic. Analysis of the nuclear rDNA operon (ITS1-5.8S-ITS2), the plastid 16S-trn I-trn A-23S-5S, rbc L-rbc S and rpl 12-rps 31-rpl 9 regions and the mitochondrial cox 2-3 spacer has revealed the existence of a previously unidentified marine refugium in the English Channel, along with possible secondary refugia off the southwest coast of Ireland and in northeast North America and/or Iceland. Coalescent and mismatch analyses date the expansion of European populations from approximately 128 000 BP and suggest a continued period of exponential growth since then. Consequently, we postulate that the penultimate (Saale) glacial maximum was the main event in shaping the biogeographic history of European P. palmata populations which persisted throughout the last (Weichselian) glacial maximum (c. 20 000 BP) in the Hurd Deep, an enigmatic trench in the English Channel.