Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Mark Demitroff"'
Autor:
Tomasz Karasiewicz, Piotr Moska, Mark Demitroff, Magdalena Fiłoc, Joanna Rychel, Mirosława Kupryjanowicz, Barbara Woronko, Aleksander Adamczyk
Publikováno v:
Quaternary International. 617:80-100
In Eastern Europe Marine Isotope Stage (MIS) 3 represents a period characterised by severe climate change of very rapid onset, which is recorded in the regional sedimentary record. Hitherto this work, the geomorphic impact of these abrupt changes to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::92fbb5777688dc94497ca46afd935464
https://doi.org/10.1016/j.quaint.2021.08.012
https://doi.org/10.1016/j.quaint.2021.08.012
Autor:
Stephen A. Wolfe, Barbara Woronko, Mark Demitroff, Dorota Chmielowska, Michael Dominic Cicali
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::29698d2367701daf94410f5dcc3be9e1
https://doi.org/10.1130/abs/2019am-336443
https://doi.org/10.1130/abs/2019am-336443
Autor:
Mark Demitroff
Publikováno v:
Permafrost and Periglacial Processes. 27:123-137
The Pleistocene environment of the New Jersey Pine Barrens has been interpreted as either cool and moist, with boreal forest, or cold and dry, with semi-desert conditions. The presence of ventifacts is often cited as perfunctory evidence for strong P
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a7e4be88390245185171a9f9988f87ac
https://doi.org/10.1002/ppp.1860
https://doi.org/10.1002/ppp.1860
Publikováno v:
Permafrost and Periglacial Processes. 20:285-294
Sand-wedge casts, soil wedges and other non-diastrophic, post-depositional sedimentary structures suggest that Late-Pleistocene permafrost and deep seasonal frost on the Mid-Atlantic Coastal Plain extended at least as far south as southern Delaware,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::600353780d48f47d982f4b91d7d06520
https://doi.org/10.1002/ppp.659
https://doi.org/10.1002/ppp.659
Publikováno v:
Permafrost and Periglacial Processes. 18:49-59
Frost fissures, filled with wind-abraded sand and mineral soil, and numerous small-scale non-diastrophic deformations, occur in the near-surface sediments of the Pine Barrens of southern New Jersey. The fissures are the result of thermal-contraction
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::82c9cb7ee80dc06b34274bf2208fef55
https://doi.org/10.1002/ppp.572
https://doi.org/10.1002/ppp.572
Publikováno v:
Permafrost and Periglacial Processes. 16:173-186
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5c8e3955f01aa88bd2c1a351dcb1f135
https://doi.org/10.1002/ppp.520
https://doi.org/10.1002/ppp.520
Publikováno v:
Permafrost and Periglacial Processes. 14:259-274
Relict sand wedges, up to 2.5 m deep and 0.4 m wide, are present in the Pine Barrens of southern New Jersey. They indicate the previous existence of permafrost. The wedges are composed predominantly of sand that shows evidence of wind transport and a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d11cd604564aa22b43c6a18e13afe2a0
https://doi.org/10.1002/ppp.456
https://doi.org/10.1002/ppp.456
Autor:
Hugh M. French, Mark Demitroff
Publikováno v:
Permafrost and Periglacial Processes. 12:337-350
The ‘frost-thaw’ or thermokarst-lake-basin hypothesis, first invoked by P. E. Wolfe in 1953 to explain the enclosed depressions and shallow basins (‘spungs’) of southern New Jersey, is re-examined. The most probable explanation is that they f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88a423ff744ef8c19890c6da88b3ac77
https://doi.org/10.1002/ppp.401
https://doi.org/10.1002/ppp.401
Publikováno v:
Proceedings of the National Academy of Sciences. 110
One or more bolide impacts are hypothesized to have triggered the Younger Dryas cooling at ∼12.9 ka. In support of this hypothesis, varying peak abundances of magnetic grains with iridium and magnetic microspherules have been reported at the Younge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3a3419e8fc15cfdd4f04e8e8d62d81a3
https://doi.org/10.1073/pnas.1304059110
https://doi.org/10.1073/pnas.1304059110
Autor:
Edward K. Vogel, Malcolm A. LeCompte, C. B. Mooney, Alfred W. Seidel, Barrett N. Rock, Dale Batchelor, Mark Demitroff
Publikováno v:
Proceedings of the National Academy of Sciences. 110
In PNAS, M. Boslough (1) raises issues about carbon spherules and nanodiamonds unrelated to our magnetic spherule focused research (2). Boslough should instead address the questions he raises to the appropriate investigators.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::41921d73a051bdb93b61891915958b1c
https://doi.org/10.1073/pnas.1300425110
https://doi.org/10.1073/pnas.1300425110