Phylogeography of Hepialus humuli (L.) (Lepidoptera: Hepialidae) in Europe: short distance vs. large scale postglacial expansions from multiple Alpine refugia and taxonomic implications

2014 ◽  
Vol 45 (3) ◽  
pp. 209-250 ◽  
Author(s):  
Thomas J. Simonsen ◽  
Peter Huemer

We explore the phylogeography of the common ghost moth, Hepialus humuli (Linnaeus) in Europe based on 1451 bp Cytochromeoxydase Subunit 1 (COI) mtDNA and 617 bp Ribosomal protein Subunit 5 (RpS5) ntDNA with special focus on populations in the Alps and surrounding regions, as well as northern Europe. While RpS5 fails to recover any phylogeographic signal, COI reveals a remarkable pattern with central European populations separated in four well-defined groups. The most divergent group is restricted to northern Italy and southern Austria and geographically isolated from the others; one group is found only in the central-northern region south of Lake Constance (Liechtenstein, western Austria) and co-occurs with the two other groups, from north-eastern Alps and north-western Alps respectively. We conclude that the southern and central groups are relicts from a previous Pleistocene glacial maximum, whereas the two latter groups were isolated during the last glacial maximum in a western and an eastern refugium respectively, the exact extends of these refugia are uncertain. The central group has subsequently interbred with the two other northern groups and probably only exists today as ancient mtDNA haplotypes. The north-western and north-eastern groups have spread considerably and overlap over a large part of their range in the Alps and surrounding areas. Following the last glacial maximum, the north-western group spread into western Europe as far as Normandy, but the English Channel has apparently acted as a dispersal barrier. The north-eastern group spread into eastern and northern Europe, including Scandinavia, and possibly into the Balkans as well. The British Isles as well as the North Atlantic islands groups, the Faroese and Shetlands were colonised from southern Scandinavia or northern Germany, likely via Doggerland. Despite the deep divergence in mtDNA between the populations in Italy and southern Austria, and the remaining populations, there are no consistent morphological differences, and we conclude that there is no evidence that the southern populations should be considered a separate species. Although the populations in the Shetland and Faroese islands are phenotypically distinct from most other populations, we find no genetic or genitalia morphological differences between these populations and the rest. We therefore conclude that they display what can be termed cryptic genetic homogeneity. As the phenotypic variation is not unique to these populations either, we synonymise the North Atlantic subspecies H. humuli thulensis Newman syn.n. with H. humuli humuli.

2020 ◽  
Author(s):  
Laurie Menviel ◽  
Paul Spence ◽  
Luke Skinner ◽  
Kazuyo Tachikawa ◽  
Tobias Friedrich ◽  
...  

<p>While paleoproxy records and modelling studies consistently suggest that North Atlantic  Deep Water (NADW) was shallower at the Last Glacial Maximum (LGM) than during pre-industrial times, its strength is still subject to debate partly due to different signals across the North Atlantic. Here, using a series of LGM experiments performed with a carbon isotopes enabled Earth system model, we show that proxy records are consistent with a shallower and weaker NADW. A significant equatorward advance of sea-ice over the Labrador Sea and the Nordic Seas shifts the NADW convection sites to the south of the Norwegian Sea. While the deep western boundary current in the Northwest Atlantic weakens with NADW, a change in density gradients strengthens the deep southward flow in the Northeast Atlantic. A shoaling and weakening of NADW further allow penetration of Antarctic Bottom Water in the North Atlantic despite its transport being reduced. This resultant globally weaker oceanic circulation leads to an increase in deep ocean carbon of ~500 GtC, thus significantly contributing to the lower LGM atmospheric CO<sub>2</sub> concentration.</p><p> </p>


1996 ◽  
Vol 62 ◽  
pp. 1-17 ◽  
Author(s):  
Ruth Charles

This paper critically examines the known radiocarbon evidence for the human recolonisation of a part of north-western Europe, the north-western Ardennes. Two sites in this region, the Trou de Blaireaux at Vaucelles and the Grotte de Sy Verlaine, have been suggested as two of the earliest human occupation sites after the Last Glacial Maximum in northern Europe. The dating evidence from these two sites, alongside other late Magdalenian sites in the immediate area, is reviewed and found to be highly problematic. More recent radiocarbon work using AMS is described and the results discussed. On this basis it is suggested that there is no direct evidence for human presence in this region prior to the start of the Böiling Interstadial phase of the Lateglacial, c. 13,000 BP.


2001 ◽  
Vol 28 (8) ◽  
pp. 1571-1574 ◽  
Author(s):  
Chris D. Hewitt ◽  
Anthony J. Broccoli ◽  
John F. B. Mitchell ◽  
Ronald J. Stouffer

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