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Pre-Wisconsinan mammals from Jamaica and models of late Quaternary extinction in the Greater Antilles
The purpose of this paper is : 1) to present radiometric dates for the first pre-Wisconsinan land mammal locality recognized in the West Indies, and 2) to assess the significance of this new information for existing models of Quaternary extinctions

The Wisconsinan glacier complex in Glaciations quaternaires dans l'Hémisphère Nord.

Chronology of late Wisconsinan glaciation in middle North America
We propose a chronology of late Wisconsinan glacial fluctuations in middle North America, from Alberta to Wisconsin, based on radiocarbon dates derived solely from wood. Previous chronologies of the southwestern margin of the North American
into the Lake Michigan basin about 11,700 BP, and an advance into the Lake Superior basin about 9 900 BP. In addition, the beginning of late Wisconsinan glaciation, before 20,000 BP, is fairly well documented. None of the fluctuations in the western part

Plant and insect remains from the Wisconsinan interstadial/stadial transition at Wedron, North-Central Illinois

Objective reconstructions of the Late Wisconsinan Laurentide ice-sheet and the significance of deformable beds

Evidence for Wisconsinan Glaciations in the Verrill Canyon area, Scotian Slope

Source and origin of Roxana silt and middle Wisconsinan midcontinent glacial activity

Plant and insect fossils from the Mayo Indian village Section (central Yukon) : new data on middle Wisconsinan environments and glaciation

The middle wisconsinan history of the Laurentide ice-sheet in La calotte glaciaire laurentidienne = The Laurentide ice sheet.

Multiple paleosols in pre-wisconsinan drift, northwestern Montana and southwestern Alberta

The anomalous Roxana Silt and mid-wisconsinan events in and near southern Michigan

Probable late Wisconsinan ice margin on the upper continental slope off St. Pierre Bank, eastern Canada

The early wisconsinan history of the Laurentide ice-sheet in La calotte glaciaire laurentidienne = The Laurentide ice sheet.

This paper discusses paleoceanographic and sedimentary environments in Hudson Strait interpreted from foraminiferal and seismic evidence. The changing environments and their chronology provide further evidence on dynamics of the Late Wisconsinan

BELOW THEM. THE DEVELOPMENT OF SUCH EXTENSIVE PERIGLACIAL LANDFORMS IN AN AREA FAR SOUTH OF THE WISCONSINAN ICE BORDER WAS ENABLED BY THE FAVORABLE LITHOLOGY, ATTITUDE, AND ASPECT OF THESE LEDGES. (A.).

Characteristics and significance of pre-Wisconsinan saprolites in the northern Appalachians in Weathered mantles (saprolites) over basement rocks of High Latitudes = Les manteaux d'altération sur les socles des Hautes Latitudes.

., but a lack of age control makes this assignment uncertain. A curve based on a late Wisconsinan, high relative sea-level stand of + 32 m at 13,000 yr B.P., a low stand of 47 m at 10,500 yr B.P., and younger radiocarbon dates related to sea-level rise indicates

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