Last edited by Grogore
Tuesday, July 21, 2020 | History

2 edition of Late-glacial and postglacial vegetation change in southwestern New York State. found in the catalog.

Late-glacial and postglacial vegetation change in southwestern New York State.

Norton G. Miller

Late-glacial and postglacial vegetation change in southwestern New York State.

by Norton G. Miller

  • 157 Want to read
  • 38 Currently reading

Published by University of the State of New York, State Education Dept. in Albany .
Written in English

    Subjects:
  • Paleobotany -- New York (State),
  • Pollen, Fossil.,
  • Glacial epoch -- New York (State)

  • Edition Notes

    SeriesBulletin -- 420
    ContributionsNew York State Museum and Science Service.
    The Physical Object
    Paginationvii, 102 p.
    Number of Pages102
    ID Numbers
    Open LibraryOL22335825M

    See what's new with book lending at the Internet Archive Late-glacial and pre-boreal pollen and diatom diagrams from Skurup, So Ann-Marie Robertsson Not in Library. Not in Library. Late-glacial and postglacial vegetation change in southwestern New . State University, where he also received graduate training in geology. Reflecting his personal roots, Norton's Ph.D. dissertation focused on late glacial and postglacial vegetation change in southwestern New York which ultimately became a NY State Museum Bulletin (NYSM Bulletin , ). Norton spent his early career at the.

    Rhodora publishes work relating to the botany of North America and covers topics such as systematics, floristics, ecology, evolution, and population genetics.   The topic of his dissertation, completed in , was glacial and postglacial vegetation change in southwestern New York State, also published as a New York State Museum Bulletin. Dr.

      His early studies aimed to reconstruct post-Pleistocene vegetation in western New York State based on pollen profiles from four peatlands, and formed the core of his doctoral dissertation at Michigan State University, completed in under the direction of Dr. A. T. Cross: Late-glacial and postglacial vegetation change in southwestern New. Abstract. A cool period from about to 10 BP (11 to ka) is recognized in pollen records from the southern Great Lakes area by the return of Picea and Abies dominance and by the persistence of herbs. The area of cooling appears centred on the Upper Great Lakes.


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Late-glacial and postglacial vegetation change in southwestern New York State by Norton G. Miller Download PDF EPUB FB2

Comment on ''Evidence for large-scale subglacial meltwater flood events in southern Ontario and northern New York State,"Geol Nieuwolt, S.

Tropical Climatology, Wiley, London, pp. Sarvis, A.P. Postglacial Water Levels in the Great Lakes Region in Relation to Holocene Climate Change: Thecamoebian and Palynological Evidence, Tiffin, S.H. Dinocyst biochronology and palynofacies – inferred systems tract character of Miocene sequences from the New Jersey Mid-Atlantic Transect (ODP Legs A and AX), A younger glacial Lake Iroquois in the Lake Ontario basin, Ontario and New York: re-examination of pollen stratigraphy and radiocarbon dating C.F.M.

Lewis, a T.W. Anderson * b a Geological Survey of Canada, Natural Resources Canada, 1 Challenger Drive, P.O. BoxDartmouth, NS B2Y 4A2, : C.F.M. Lewis, T.W. Anderson. Stable oxygen isotope contents of marl deposits and molluscs from lakes and ponds in northern New York State (U.S.A.) and southwestern Ontario (Canada) are remarkably uniform for carbonates formed between ab yr B.P.

and yr B.P. This suggests relatively stable climatic conditions with slowly increasing temperatures. late quaternary paleogeographic changes in the coastal environments of delaware, middle atlantic bight, related to archaeologic settings part v.

late‐glacial and early postglacial environments. new data and models for 8, years of archaic societies and their environments in the upper susquehanna valley of new york state.

bruce. Articles: Deer, Toads, Dogs, And Frogs: A New Interpretation of the Faunal Remains from the Engelbert Site, Tioga County, New York (April M. Beisaw, p. ); New York State's Garnetiferous Gneiss Bannerstones: The Form and Function of Flight (Ralph C.

Rataul, p. ); Paul Radin and the Historical Origins of Debates on Indigenous Knowledge. Gordon RB. The primeval forest types of southwestern New York. Catterraugus County. New York State Mus Bull Albany: Univ State New York. Gordon RB. The natural vegetation of Ohio in pioneer days.

Bull Ohio Biol Surv New Ser 3(2):xi, Gordon RB. Personal recollections of the Ohio Natural Vegetation Survey. Norwegian late glacial. Following the Danish example, late‐glacial pollen diagrams from Norway have been interpreted as pioneer vegetation developing into more or less open birch forest in the interstadial (Allerød), which was then destroyed completely or partially during the cold Younger Dryas interval (6).A synthesis delimited vegetation regions and the ecotones between them.

Use of paleoclimatic data as analogs for understanding future global changes. In J. Eddy and H. Oeschger (eds.) Global Changes in the Perspective of the Past.

Wiley and Sons Ltd., London, pp. Webb, T. III. Postglacial magnitudes and rates of vegetation change in eastern North America: implications for the future. "Late-glacial and Holocene vegetation and climate variability, including major droughts, in the Sky Lakes region of southeastern New York State." Palaeogeography, Palaeoclimatology, Palaeoecology [ / ].

The sensitivity of global climate to colder North Atlantic sea surface temperatures is in vestigated with the use of the GISS general circulation model. North Atlantic ocean temperatu B.P., resembling those prevalent during the Younger Dryas, were incorporated into the model of the present climate and also into an experiment using orbital parameters and land ice.

Late-glacial and Postglacial Vegetation Change in Southwestern New York State. New York State Museum and Science Service BulletinAlbany. Robinson, Francis “Jess” W., IV The Initiation and Maintenance of the Early Woodland Interaction Sphere (ca.3, B.P.): The View from Six Northeastern Mortuary Sites.

About Cookies, including instructions on how to turn off cookies if you wish to do so. By continuing to browse this site you agree to us using cookies as described in About Cookies. Remove maintenance message. Vegetation established earlier in the southern ranges, following the same general trend as the Laurentian Ice Sheet recession.

However, local factors such as ice retreat, response to global-scale climate changes, and paraglacial processes acted in synergy to increase the resilience and to influence the occurrence of alpine landscapes.

Access to society journal content varies across our titles. If you have access to a journal via a society or association membership, please browse to your society journal, select. The aim of this research is to determine the response of the vegetation in coastal Maritime Canada to the Younger Dryas cooling event (°10 —10 1 4 C yr BP) that interrupted the warming trend following the last glaciation.

Detailed paleoecological studies were carried out on the organic, pollen, and plant macrofossil content of sediment cores recovered from six small lakes in New. Miller, N.G. Late-glacial and postglacial vegetation change in southeastern New York State.

Bulletin of the New York State Museum Science Service. Late-glacial and postglacial vegetation change in southwestern New York State. New York State Museum and Science Service Bulletin Albany, NY, USA: The State Education Department. Mott RJ, Farley-Gill LD. A late-Quaternary pollen profile from Woodstock.

Ontario. Canadian Journal of Botany – Pennington W. This site uses cookies to deliver our services, improve performance, for analytics, and (if not signed in) for advertising.

By using LibraryThing you acknowledge that. Changes by a factor of 5 or more for all except rate pollen types from one level to the next were considered significant indication of changes in the pollen input to the lake, reflecting changes in the pollen productivity of the surrounding vegetation.

Miller, N. G. Late-glacial and postglacial vegetation change in southwestern New York State. – BulletinNew York State Mu - seum and Science Service, The State Education Dept, New York.

Mott, R. J. Palynological studies of lake sediment profiles from southwestern New Brunswick. – Can. J. Earth Sci. –intervention of William P. Letchworth, a prominent western New York State figure and at that time vice-president of the State Board of Charities, the State of New York assumed the support of the institution.

The old facilities continued in use until when the school came under.New radiocarbon dates from the Allegheny Valley. Ann. Meeting Eastern States Archaeological Federation. MILLER, N. G. Late&acial and postglacial vegetation change in southwestern New York state.