This paper reassesses the areal extent of Mammoth Steppe in Eastern Beringia and discusses some of the ways in which grazing and topography entered into the maintenance of the Mammoth Steppe. Large, generalist grazing mammals, by their grazing style, helped maintain the Mammoth Steppe by removing old-growth and by stimulating grass plants to reproduce vegetatively. These grazers also promoted uniformity in growth-form and uniformity in plant biomass (phytomass) above and below the ground surface. During the late Pleistocene these large, generalist grazers were eliminated from interior Alaska by Paleolndian hunters and their predatory animal companions. The loss of these large, generalist grazers precipitated a change in the structure of the...
Human colonization and subsequent occupation of eastern Beringia, beginning c. 14,500 years ago, is ...
This paper explores paleoenvironmental and paleoecological information that may be obtained from sma...
We explore the relationship between the edaphic potential of soils and the mineral properties of the...
This paper reassesses the areal extent of Mammoth Steppe in Eastern Beringia and discusses some of t...
Abstract The Siberian mammoth steppe ecosystem changed dramatically with the disappearance of large ...
The collapse of the steppe-tundra biome (mammoth steppe) at the end of the Pleistocene is used as an...
The Bering Land Bridge (BLB) connected the two principal arctic biological refugia, Western and East...
During the late Pleistocene (130-12 ka), Beringia, a largely ice-free land located in the Mammoth St...
The Pleistocene mammoth steppe was a vast biome that stretched from northwestern Europe to central C...
There is an abundance of soils and paleosols as well as terraces and terrace fills and erosional for...
ABSTRACT. Late Pleistocene Beringia had herb-dominated vegetation with abundant grasses (Poaceae), a...
The human colonization of Beringia during the Late Glacial (14,500-11,700 years ago) is one of the m...
It has often been said tallgrass prairies are the result of fire and climate. That statement is true...
Plant macrofossils from the Mamontovy Khayata permafrost sequence (71°60N, 129°25E) on the Bykovsky ...
ABSTRACT. While bison were the most abundant large mammals in Eastern Beringia for most of the last ...
Human colonization and subsequent occupation of eastern Beringia, beginning c. 14,500 years ago, is ...
This paper explores paleoenvironmental and paleoecological information that may be obtained from sma...
We explore the relationship between the edaphic potential of soils and the mineral properties of the...
This paper reassesses the areal extent of Mammoth Steppe in Eastern Beringia and discusses some of t...
Abstract The Siberian mammoth steppe ecosystem changed dramatically with the disappearance of large ...
The collapse of the steppe-tundra biome (mammoth steppe) at the end of the Pleistocene is used as an...
The Bering Land Bridge (BLB) connected the two principal arctic biological refugia, Western and East...
During the late Pleistocene (130-12 ka), Beringia, a largely ice-free land located in the Mammoth St...
The Pleistocene mammoth steppe was a vast biome that stretched from northwestern Europe to central C...
There is an abundance of soils and paleosols as well as terraces and terrace fills and erosional for...
ABSTRACT. Late Pleistocene Beringia had herb-dominated vegetation with abundant grasses (Poaceae), a...
The human colonization of Beringia during the Late Glacial (14,500-11,700 years ago) is one of the m...
It has often been said tallgrass prairies are the result of fire and climate. That statement is true...
Plant macrofossils from the Mamontovy Khayata permafrost sequence (71°60N, 129°25E) on the Bykovsky ...
ABSTRACT. While bison were the most abundant large mammals in Eastern Beringia for most of the last ...
Human colonization and subsequent occupation of eastern Beringia, beginning c. 14,500 years ago, is ...
This paper explores paleoenvironmental and paleoecological information that may be obtained from sma...
We explore the relationship between the edaphic potential of soils and the mineral properties of the...