Zobrazeno 1 - 10
of 47
pro vyhledávání: '"N. Mode"'
Publikováno v:
BMC Public Health, Vol 16, Iss 1, Pp 1-13 (2016)
Abstract Background Studies uncovering factors beyond socio-economic status (SES) that would explain racial and ethnic disparities in mortality are scarce. Methods Using prospective cohort data from the Third National Health and Nutrition Examination
Externí odkaz:
https://doaj.org/article/b733244ca07445dcb14f51022fac9a10
Akademický článek
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Publikováno v:
Tree-Ring Research. 73:102-112
Since the late 19th Century, geologists and naturalists working in the US Midwest have reported an abundance of tree macrofossils embedded in glacial and lacustrine deposits formed after the Last Glacial Maximum. The most widely-known of these sites
Publikováno v:
Geological Society of America Abstracts with Programs.
Total and direct effects of race on all cause mortality and effects mediated through socio-economic, lifestyle and social support factors, NHANES III. Table S2. Total and direct effects of race on all-cause mortality and effects mediated through heal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::57df33e23eb24a35a4d154a406804342
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Thomas S. Hooyer, William N. Mode
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Boreas. 29:261-271
A sediment core from Lake Yarnyshnoe-3 (69°04'N; 36°04'E), an emerged coastal lake from the tundra of the north-central Kola Peninsula, has been analyzed for fossil pollen and diatoms. The pollen record shows the Younger Dryas event marked by incre
Publikováno v:
Boreas. 26:329-346
Sediment cores recovered from four emerged lakes (54, 41, 22, and 7 m a.s.l.) provide new data on the deglaciation and relative sea-level history of the Murman coast, Kola Peninsula. The transition from marine to lacustrine sediment is identified in
Publikováno v:
Géographie physique et Quaternaire. 39:151-162
The late-glacial and Holocene paleoenvironmental sequence for the Frobisher Bay area is outlined using glacial, sea level, and palynological evidence. A rapid retreat of ice from the late Foxe glacial maximum in the lower part of the bay after 11,000