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  • 1
    Monograph available for loan
    Monograph available for loan
    The blue planet : An introduction to earth system science (1994)
    New York [u.a.] : John Wiley
    Details Availability
    Call number: PIK N 322-97-0340
    Type of Medium: Monograph available for loan
    Pages: 493 p.
    ISBN: 0471540218
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Dangerous earth : an introduction to geologic hazards (1997)
    New York [u.a.] : Wiley
    Details Availability
    Call number: M 99.0459
    Type of Medium: Monograph available for loan
    Pages: XV, 300 S.
    ISBN: 0471135658
    Classification:
    B.2.5.
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    The dynamic earth : an introduction to physical geology (1992)
    New York [u.a.] : Wiley & Sons
    Details Availability
    Call number: M 94.0154 ; M 94.0597 ; AWI G1-92-0462
    Type of Medium: Monograph available for loan
    Pages: xiv, 570 S.
    Edition: 2nd ed.
    ISBN: 0471531316
    Classification:
    A.2.1.
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: GFZ Library
    Branch Library: AWI Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    The quaternary period in the United States (2003)
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Details Availability
    Call number: AWI G7 04-0015
    In: Developments in quaternary science, Volume 1
    Type of Medium: Monograph available for loan
    Pages: ix, 584 Seiten , Illustrationen
    Edition: First edition
    ISBN: 0444514716
    Series Statement: Developments in quaternary science 1
    URL: https://www.gbv.de/dms/goettingen/372523765.pdf
    Language: English
    Note: Contents Foreword / Jim Rose Preface / Alan R. Gillespie, Stephen C. Porter and Brian F. Atwater The southern Laurentide Ice Sheet / David M. Mickelson and Patrick M. Colgan The Cordilleran Ice Sheet / Derek B. Booth, Kathy Goetz Troost, John J. Clague and Richard B. Waitt Controls, history, outbursts, and impact of large late-Quaternary proglacial lakes in North America / James T. Teller Pleistocene glaciations of the Rocky Mountains / Kenneth L. Pierce Quaternary alpine glaciation in Alaska, the Pacific Northwest, Sierra Nevada, and Hawaii / Darrell S. Kaufman, Stephen C. Porter and Alan R. Gillespie Coupling ice-sheet and climate models for simulation of former ice sheets / Shawn J. Marshall, David Pollard, Steven Hostetler and Peter U. Clark Permafrost process research in the United States since 1960 / Bernard Hallet, Jaakko Putkonen, Ronald S. Sletten and Noel Potter Jr. Quaternary sea-level history of the United States / Daniel R. Muhs, John F. Wehmiller, Kathleen R. Simmons, and Linda L. York Western lakes / Larry Benson Isotopic records from ground-water and cave speleothem calcite in North America / Jay Quade Rivers and riverine landscapes / David R. Montgomery and Ellen E. Wohl Landscape evolution models / Frank J. Pazzaglia Eolian sediments / Alan J. Busacca, James E. Beget, Helaine W. Markewich, Daniel R. Muhs, Nicholas Lancaster and Mark R. Sweeney Soils and the Quaternary climate system / Milan J. Pavich and Oliver A. Chadwick Earthquake recurrence inferred from paleoseismology / Brian F. Atwater, Martitia P. Tuttle, Eugene S. Schweig, Charles M. Rubin, David K. Yamaguchi and Eileen Hemphill-Haley Quaternary volcanism in the United States / William E. Scott Late-Quaternary vegetation history of the eastern United States / Eric C. Grimm and George L. Jacobson Jr. Quaternary vegetation and climate change in the western United States: Developments, perspectives, and prospects / Robert S. Thompson, Sarah L. Shafer, Laura E. Strickland, Peter K. Van de Water and Katherine H. Anderson Results and paleoclimate implications of 35 years of paleoecological research in Alaska / Patricia M. Anderson, Mary E. Edwards and Linda B. Brubaker Quaternary history from the U.S. tropics / Sara Hotchkiss Climatically forced vegetation dynamics in eastern North America during the late Quaternary Period / Thompson Webb III, Bryan Shuman and John W. Williams Holocene fire activity as a record of past environmental change / Cathy Whitlock and Patrick J. Bartlein Interannual to decadal climate and streamflow variability estimated from tree rings / David W. Stahle, Falko K. Fye and Matthew D. Therrell Quaternary Coleoptera of the United States and Canada / Allan C. Ashworth Vertebrate paleontology / S. David Webb, Russell W. Graham, Anthony D. Barnosky, Christopher J. Bell, Richard Franz, Elizabeth A. Hadly, Ernest L. Lundelius Jr., H. Gregory McDonald, Robert A. Martin, Holmes A. Semken Jr. and David W. Steadman Peopling of North America / David J. Meltzer Modeling paleoclimates / Patrick J. Bartlein and Steven W. Hostetle
    Location: AWI Reading room
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  • 5
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    Unknown
    PKDB286302 (2000)
    PANGAEA
    Details
    Publication Date: 2023-03-08
    Keywords: AGE; Age, comment; Age, maximum/old; Age, minimum/young; Interpretation from literature (PKDB); Latitude of event; Longitude of event; Paleoclimate Database of the Quaternary; PKDB; PKDB286302; Precipitation, relative difference; Temperature, relative difference; Wind speed, relative difference
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 6
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    PKDB286302 (2000)
    PANGAEA
    Details
    Publication Date: 2023-03-08
    Keywords: AGE; Age, comment; Age, maximum/old; Age, minimum/young; LATITUDE; LONGITUDE; OUTCROP; Outcrop sample; Paleoclimate Database of the Quaternary; PKDB; PKDB66154; Snow line elevation
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 7
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    Unknown
    Description of loess sections in China
    PANGAEA
    In:  Supplement to: An, Zhisheng; Kukla, George J; Porter, Stephen C; Xiao, Jule (1991): Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of Central China during the last 130000 years. Quaternary Research, 36(1), 29-36, https://doi.org/10.1016/0033-5894(91)90015-W
    Details
    Publication Date: 2023-05-12
    Description: The magnetic susceptibility of loess and paleosols in central China represents a proxy climate index closely related to past changes of precipitation and vegetation, and thus to summer monsoon intensity. Time series of magnetic susceptibility constructed for three loess-paleosol sequences in the southern part of the Chinese Loess Plateau document the history of summer monsoon variation during the last 130,000 yr. They correlate closely with the oxygen isotope record of stages 1 to 5 in deep-sea sediments. Soils were forming during intervals of strong summer monsoon, whereas loess units were deposited at times of reduced monsoon intensity. The Chinese loess-paleosol sequence can thus be viewed as a proxy record of Asian monsoon variability extending over the last 2.5 myr.
    Keywords: AGE; Age, comment; Age, maximum/old; Age, minimum/young; Calculated; Geology, comment; Interpretation from literature (PKDB); LATITUDE; LONGITUDE; ORDINAL NUMBER; Paleoclimate Database of the Quaternary; PKDB; PKDB15611; Precipitation, relative difference; Sedimentation rate; Temperature, relative difference; Wind direction; Wind speed, relative difference
    Type: Dataset
    Format: text/tab-separated-values, 150 data points
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  • 8
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    The Little Ice Age: glacier variations and climate since AD 1250 [abstract] (2021)
    In:  http://aquaticcommons.org/id/eprint/15803 | 8 | 2014-12-08 21:21:56 | 15803
    Details
    Publication Date: 2021-07-10
    Description: EXTRACT (SEE PDF FOR FULL ABSTRACT):During the past hundred years, mountain glaciers throughout the world have retreated significantly from moraines built during the previous several centuries. In the 1930s, Francois Matthes of the U.S. Geological Survey concluded that the moraines represent the greatest advances of glaciers since the end of the last glacial age, some 10,000 years earlier, and informally referred to this late Holocene interval of expanded ice cover as the Little Ice Age.
    Keywords: Atmospheric Sciences ; Earth Sciences ; PACLIM
    Repository Name: AquaDocs
    Type: conference_item
    Format: application/pdf
    Format: application/pdf
    Format: 181-182
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  • 9
    Electronic Resource
    Electronic Resource
    HERBICIDES AND TRANSFORMATION PRODUCTS IN SURFACE WATERS OF THE MIDWESTERN UNITED STATES (2003)
    Oxford, UK : Blackwell Publishing Ltd
    Journal of the American Water Resources Association 39 (2003), S. 0 
    Details
    ISSN: 1752-1688
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Notes: : Most herbicides applied to crops are adsorbed by plants or transformed (degraded) in the soil, but small fractions are lost from fields and either move to streams in overland runoff, near surface flow, or subsurface drains, or they infiltrate slowly to ground water. Herbicide transformation products (TPs) can be more or less mobile and more or less toxic in the environment than their source herbicides. To obtain information on the concentrations of selected herbicides and TPs in surface waters of the Midwestern United States, 151 water samples were collected from 71 streams and five reservoir outflows in 1998. These samples were analyzed for 13 herbicides and 10 herbicide TPs. Herbicide TPs were found to occur as frequently or more frequently than source herbicides and at concentrations that were often larger than their source herbicides. Most samples contained a mixture of more than 10 different herbicides or TPs. The ratios of TPs to herbicide concentrations can be used to determine the source of herbicides in streams. Results of a two-component mixing model suggest that on average 90 percent or more of the herbicide mass in Midwestern streams during early summer runoff events originates from the runoff and 10 percent or less comes from increased ground water discharge.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1752-1688.2003.tb04402.x
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  • 10
    Electronic Resource
    Electronic Resource
    Distribution of benthic algae in the upper Illinois River basin in relation to geology and land use (2000)
    Oxford, UK : Blackwell Science Ltd
    Freshwater biology 44 (2000), S. 0 
    Details
    ISSN: 1365-2427
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: 〈list style="custom"〉1Benthic-algal distributions in the upper Illinois River basin, IL, U.S.A., were examined in relation to geology, land use, water chemistry and stream habitat using (detrended) (canonical) correspondence analysis, autecological metrics and indicator-species analysis in order to identify the major environmental gradients influencing community variation.2Ionic composition and major nutrient [i.e. nitrogen (N) and phosphorus (P)] concentration of surface waters, salinity (Na-Cl type), substratum type and physiognomic form of dominant species were primary factors contributing to variation in benthic-algal assemblages of the basin. Basin geology was a significant contributing factor, but the explained variance associated with this factor was less than that related to land use.3Proportions of algal biomass consisting of cyanophytes, filamentous chlorophytes, halophilic diatoms and diatoms which utilize nitrogen heterotrophically were greater in eutrophic river segments than in less nutrient-enriched segments. Composition of the benthic flora indicated meso-eutrophic or eutrophic conditions throughout the basin; there were few diatoms indicative of hypertrophic waters. Shifts in diatom-assemblage structure in response to nutrient loading provided an incomplete representation of the community-response curve.4A weighted-averages regression model based on total P and benthic-algal abundances (all divisions included) yielded a highly significant correlation (r2 = 0.83) between species-inferred [WA(tol)] and observed total P, with systematic bias (increased deviation of residuals) occurring only at concentrations greater than ∼ 1.0 mg L−1 total P. This result indicates that total P regression and calibration models can be predictable for a river basin receiving excessive loadings of phosphorus.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1046/j.1365-2427.2000.00536.x
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