Problems in Zoogeography of the Lake Trout, Salvelinus namaycush

1964 ◽  
Vol 21 (5) ◽  
pp. 977-994 ◽  
Author(s):  
C. C. Lindsey

Disagreement exists in the literature as to whether lake trout survived Wisconsin glaciation north or south of the ice sheet. Other freshwater fishes whose range in North America equals or exceeds that of lake trout all survived in both northern and southern refugia. Arguments in favour of a southern refugium for lake trout include their wide distribution eastward to Nova Scotia and New England, their presence in some Mississippi headwaters, and possible late-Wisconsin date of a fossil lake trout south of glaciation. Absence from some habitable lakes along the southern margin of glaciation is attributable to northward shift of isotherms during the hypsithermal period. A northern refugium is suggested by occurrence of lake trout in remote parts of Alaska, and the improbability of their having failed to reach and persist in Alaska prior to last glacial advance. They do not now closely approach Bering Strait, and may be held in check by ecological factors which have been operative also during previous glacial and interglacial periods, on the Bering land bridge as well as on the continent. Hucho taimen is a related Asian counterpart whose dispersal may be similarly controlled. Large lampreys may prevent dispersal of lake trout into lower water courses and the sea.

Science ◽  
1965 ◽  
Vol 147 (3662) ◽  
pp. 1107-1114 ◽  
Author(s):  
D. M. Hopkins ◽  
F. S. MacNeil ◽  
R. L. Merklin ◽  
O. M. Petrov

2018 ◽  
Vol 50 (1) ◽  
pp. 113-121 ◽  
Author(s):  
Carolina CORNEJO ◽  
Christoph SCHEIDEGGER

AbstractUsing an ITS mutation rate as calibration reference, a three-locus timetree was generated for the genus Lobaria and its most important clades. The timetree resolved most clades with strong support and gave an estimate of the diversification time for Lobaria during the early Oligocene. A fossil impression from a 12–24 million-year-old Miocene deposit is hypothesized here to belong to an ancestral Lobaria species. Additionally, the age estimate indicates that the paleoclimate and the closing or opening of the Bering Strait played a major role in shaping the current distribution of most Lobaria species. It is hypothesized that the Bering land bridge acted as a major highway during warm-temperate climate periods, but as a barrier during Arctic climate times.


2017 ◽  
Vol 13 (8) ◽  
pp. 991-1005 ◽  
Author(s):  
Martin Jakobsson ◽  
Christof Pearce ◽  
Thomas M. Cronin ◽  
Jan Backman ◽  
Leif G. Anderson ◽  
...  

Abstract. The Bering Strait connects the Arctic and Pacific oceans and separates the North American and Asian landmasses. The presently shallow ( ∼  53 m) strait was exposed during the sea level lowstand of the last glacial period, which permitted human migration across a land bridge today referred to as the Bering Land Bridge. Proxy studies (stable isotope composition of foraminifera, whale migration into the Arctic Ocean, mollusc and insect fossils and paleobotanical data) have suggested a range of ages for the Bering Strait reopening, mainly falling within the Younger Dryas stadial (12.9–11.7 cal ka BP). Here we provide new information on the deglacial and post-glacial evolution of the Arctic–Pacific connection through the Bering Strait based on analyses of geological and geophysical data from Herald Canyon, located north of the Bering Strait on the Chukchi Sea shelf region in the western Arctic Ocean. Our results suggest an initial opening at about 11 cal ka BP in the earliest Holocene, which is later than in several previous studies. Our key evidence is based on a well-dated core from Herald Canyon, in which a shift from a near-shore environment to a Pacific-influenced open marine setting at around 11 cal ka BP is observed. The shift corresponds to meltwater pulse 1b (MWP1b) and is interpreted to signify relatively rapid breaching of the Bering Strait and the submergence of the large Bering Land Bridge. Although the precise rates of sea level rise cannot be quantified, our new results suggest that the late deglacial sea level rise was rapid and occurred after the end of the Younger Dryas stadial.


Taxon ◽  
1968 ◽  
Vol 17 (1) ◽  
pp. 71-72 ◽  
Author(s):  
F. P. Jonker

Antiquity ◽  
2015 ◽  
Vol 89 (345) ◽  
pp. 740-742 ◽  
Author(s):  
Herbert Maschner

This review considers three books on the archaeology of territories situated around the Bering Sea—a region often referred to as Beringia, adopting the term created for the Late Pleistocene landscape that extended from north-east Asia, across the Bering Land Bridge, to approximately the Yukon Territory of Canada. This region is critical to the archaeology of the Arctic for two fundamental reasons. First, it is the gateway to the Americas, and was certainly the route by which the territory was colonised at the end of the last glaciation. Second, it is the place where the entire Aleut-Eskimo (Unangan, Yupik, Alutiiq, Inupiat and Inuit) phenomenon began, and every coastal culture from the far north Pacific, to Chukotka, to north Alaska, and to arctic Canada and Greenland, has its foundation in the cultural developments that occurred around the Bering Sea.


2020 ◽  
Vol 66 (3-4) ◽  
pp. 180-189
Author(s):  
Denise Taimi Karkkainen ◽  
Stephen J. Richards ◽  
Fred Kraus ◽  
Burhan Tjaturadi ◽  
Keliopas Krey ◽  
...  

We describe a new species of gecko in the Lepidodactylus novaeguineae Group from Salawati Island, West Papua Province, Indonesia. The new species can be distinguished from all congeners by a unique combination of aspects of body size, shape, colouration, and scalation. The holotype and only known specimen is a mature male with a snout-vent length of less than 33 mm, suggesting it is the smallest species of Lepidodactylus; however, to confirm that, larger sample sizes of the nominate species and other species are required. The Lepidodactylus novaeguineae Group has a wide distribution across the western, northern, and eastern margins of New Guinea, but it seems to be most often associated with islands (including land-bridge islands) or geological terranes derived from former island arcs.


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