Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Thane W. Anderson"'
Autor:
Thane W. Anderson, C. F. M. Lewis
Publikováno v:
Journal of Paleolimnology. 47:513-530
Piston cores from deep-water bottom deposits in Lake Ontario contain shallow-water sediments such as, shell-rich sand and silt, marl, gyttja, and formerly exposed shore deposits including woody detritus, peat, sand and gravel, that are indicative of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::08d10f3aff99bc0d43499a3659e8cb50
https://doi.org/10.1007/s10933-011-9551-8
https://doi.org/10.1007/s10933-011-9551-8
Publikováno v:
Géographie physique et Quaternaire. 36:197-208
Overburden removal for quarrying operations at the Milford Gypsum Quarry, East Milford, Nova Scotia, exposed 2 m of compacted and distorted peat and organic clays with abundant plant remains, associated with inorganic and laminated clays and sands. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::53ad987f2e9785d7a4bb8a51b75f548e
https://doi.org/10.7202/032477ar
https://doi.org/10.7202/032477ar
Publikováno v:
Géographie physique et Quaternaire. 47:111-118
A partial skeleton of an adult male walrus (Odobenus rosmarus) was excavated from a raised beach on the Labrador coast, near the present community of Forteau. Bone collagen from the specimen has been radiocarbon dated at about 11 500 yr BP. Fossil po
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1c1de5ce476425ee17699f5ed7ca4ac6
https://doi.org/10.7202/032935ar
https://doi.org/10.7202/032935ar
Publikováno v:
Journal of Paleolimnology. 39:491-509
Swan Lake is a small kettle lake located on the Oak Ridges Moraine; a moraine that is recognized as an important source of ground water for the nearby and rapidly expanding Greater Toronto Area. A paleolimnological reconstruction using pollen and dia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::087ecf6b51492fd3a32acc85ac98abd4
https://doi.org/10.1007/s10933-007-9126-x
https://doi.org/10.1007/s10933-007-9126-x
Publikováno v:
Journal of Paleolimnology. 39:361-380
Lake Simcoe is a large lake 45 km across and in places over 30 m deep, located between Lake Huron and Lake Ontario, in the glaciated terrain of southern Ontario, Canada. Seismostratigraphic analysis of high-resolution seismic reflection profiles, tog
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4c9a99ea42a1906baebc25ac3903615a
https://doi.org/10.1007/s10933-007-9111-4
https://doi.org/10.1007/s10933-007-9111-4
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 246:75-100
An examination of post-Younger Dryas (YD) pollen stratigraphies in the Gulf of St. Lawrence and St. Lawrence estuary region reveals features in the pollen records that represent breaks in the normal vegetation succession, widespread vegetation suppre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0522d90b2dadbdf29b6a3495456c071e
https://doi.org/10.1016/j.palaeo.2006.10.028
https://doi.org/10.1016/j.palaeo.2006.10.028
Publikováno v:
Journal of Paleolimnology. 14:297-309
Excavation below the Lake Algonquin gravel beach bar near Clarksburg, Ontario, exposed mollusc-bearing clay over a lens of plant debris. This is the northernmost and most deeply buried Lake Algonquin fossil site found thus far in Ontario. It is the f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::07481db2e9472f5083070702b1fc9437
https://doi.org/10.1007/bf00682430
https://doi.org/10.1007/bf00682430
Autor:
David K. Rea, David M. Dobson, Alison J. Smith, Thane W. Anderson, C. F. Michael Lewis, David L. Dettman, Theodore C. Moore, Larry A. Mayer
Publikováno v:
Geology. 22:1059
The oxygen isotope record of ostracode and clam shells recovered from Great Lakes cores of known age allows definition of times when meltwaters from the Laurentide ice sheet were important components of lake water in the several lake basins since 12
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6184910faee0f3c332ff0b56c3ba1aed
https://doi.org/10.1130/0091-7613(1994)022<1059:glpcio>2.3.co
https://doi.org/10.1130/0091-7613(1994)022<1059:glpcio>2.3.co
Publikováno v:
Quaternary Research. 23:205-226
The Gage Street site in Kitchener, Ontario, is a peat/marl sequence representing continuous lacustrine sedimentation from the time of deglaciation (ca. 13,000 yr B.P.) through 6900 yr B.P. Insect, pollen, and plant macrofossil remains isolated from t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dd2e9803a5f966daee0b58cf861ba3ff
https://doi.org/10.1016/0033-5894(85)90029-8
https://doi.org/10.1016/0033-5894(85)90029-8
Publikováno v:
Quaternary Research. 5:49-87
Molluscs, ostracodes, diatoms, pollen, plant macrofossils, peat, and wood have been found in glacial Lake Algonquin sediments, and estuarine-alluvial sediments of the same age, in southern Ontario. Molluscs and ostracodes are particularly abundant an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b93a5c446f43cb2439a296e3d47bc69c
https://doi.org/10.1016/0033-5894(75)90048-4
https://doi.org/10.1016/0033-5894(75)90048-4