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  • 2010-2014  (1,405)
  • 1925-1929
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  • 1
    Monograph available for loan
    Monograph available for loan
    Berlin : Robert-Koch-Institut
    Call number: PIK O 080-11-0135
    Description / Table of Contents: Contents: 1. Einleitung ; 2. Der gegenwärtige Klimawandel ; 3. Gesundheitliche Auswirkungen des Klimawandels im Überblick ; 4. Gesundheitliche Auswirkungen von Hitzewellen und anderen klimaassoziierten Ereignissen ; 5. Gesundheitliche Auswirkungen des Klimawandels unter dem Aspekt erhöhter UV-, Allergen- und Schadstoff-Exposition ; 6. Gesundheitliche Auswirkungen des Klimawandels aus infektiologischer Perspektive ; 7. Zusammenfassung und Schlussfolgerungen
    Type of Medium: Monograph available for loan
    Pages: 244 S. : Ill., graph. Darst.
    ISBN: 9783896061151
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: AWI Bio-22-94882
    Type of Medium: Monograph available for loan
    Pages: XXI, 506 Seiten , Illustrationen
    ISBN: 978-0-521-75777-5 (pbk) , 978-0-521-76763-7 (hbk)
    Language: English
    Note: Contents List of contributors Preface I Introductory Chapters 1 The Ecological Value of Biyophytes as Indicators of Climate Change / NANCY G. SLACK 2 Bryophyte Physiological Processes in a Changing Climate: an Overview / ZOLTÁN TUBA II Ecophysiology 3 Climatic Responses and Limits of Biyophytes: Comparisons and Contrasts with Vascular Plants / MICHAEL C. F. PROCTOR 4 Effects of Elevated Air C02 Concentration on Bryophytes: a Review / ZOLTÁN TUBA, EDIT ÖTVÖS, AND ILDIKÓ JÓCSÁK 5 Seasonal and Interannual Variability of Light and UV Acclimation in Mosses / NIINA M. LAPPALAINEN, ANNA HYYRYLÄINEN, AND SATU HUTTUNEN III Aquatic Bryophytes 6 Ecological and Physiological Effects of Changing Climate on Aquatic Bryophytes / JANICE M. GLIME 7 Aquatic Bryophytes under Ultraviolet Radiation / JAVIER MARTÍNEZ-ABAIGAR AND ENCARNACIÓN NÚÑEZ-OLIVERA IV Desert and Tropical Ecosystems 8 Responses of a Biological Crust Moss to Increased Monsoon Precipitation and Nitrogen Deposition in the Mojave Desert / LLOYD R. STARK, D. NICHOLAS MCLETCHIE, STANLEY D. SMITH, AND MELVIN J. OLIVER 9 Ecology of Bryophytes in Mojave Desert Biological Soil Crusts: Effects of Elevated CO2 on Sex Expression, Stress Tolerance, and Productivity in the Moss Syntrichia caninervis Mitt. / JOHN C. BRINDA, CATHERINE FERNANDO, AND LLOYD R. STARK 10 Responses of Epiphytic Bryophyte Communities to Simulated Climate Change in the Tropics / JORGE JÁCOME, S. ROBBERT GRADSTEIN, AND MICHAEL KESSLER V Alpine, Arctic, and Antarctic Ecosystems 11 Effects of Climate Change on Tundra Bryophytes / ANNIKA K. JÄGERBRAND, ROBERT G. BJÖRK, TERRY CALLAGHAN, AND RODNEY D. SEPPELT 12 Alpine Bryophytes as Indicators for Climate Change: a Case Study from the Austrian Alps / DANIELA HOHENWALLNER, HAROLD GUSTAV ZECHMEISTER, DIETMAR MOSER, HARALD PAULI, MICHAEL GOTTFRIED, KARL REITER, AND GEORG GRABHERR 13 Bryophytes and Lichens in a Changing Climate: An Antarctic Perspective / RODNEY D. SEPPELT VI Sphagnum and Peatlands 14 Living on the Edge: The Effects of Drought on Canada's Western Boreal Peatlands / MELANIE A. VILE, KIMBERLI D. SCOTT, ERIN BRAULT, R. KELMAN WlEDER, AND DALE H . VlTT 15 The Structure and Functional Features of Sphagnum Cover of the Northern West Siberian Mires in Connection with Forecasting Global Environmental and Climatic Changes / ALEKSEI V. NAUMOV AND NATALIA P. KOSYKH 16 The Southernmost Sphagnum-dominated Mires on the Plains of Europe: Formation, Secondary Succession, Degradation, and Protection / JÁNOS NAGY VII Changes in Bryophyte Distribution with Climate Change: Data and Models 17 The Role of Bryophyte Paleoecology in Quaternary Climate Reconstructions / GUSZTÁV JAKAB AND PÁL SÜMEGI 18 Signs of Climate Change in the Bryoflora of Hungary / TAMÁS PÓCS 19 Can the Effects of Climate Change on British Bryophytes be Distinguished from those Resulting from Other Environmental Changes? / JEFFREY W. BATES AND CHRISTOPHER D. PRESTON 20 Climate Change and Protected Areas: How well do British Rare Bryophytes Fare? / BARBARA J. ANDERSON AND RALF OHLEMÜLLER 21 Modeling the Distribution of Sematophyllum substrumulosum (Hampe) E. Britton as a Signal of Climatic Changes in Europe / CECÍLIA SÉRGIO, RUI FIGUEIRA, AND RUI MENEZES 22 Modeling Bryophyte Productivity Across Gradients of Water Availability Using Canopy Form-Function Relationships / STEVEN K. RICE, NATHALI NEAL, JESSE MANGO, AND KELLY BLACK VIII Conclusions 23 Bryophytes as Predictors of Climate Change / L. DENNIS GIGNAC 24 Conclusions and Future Research / NANCY G. SLACK AND LLOYD R. STARK Index
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 3
    Publication Date: 2011-05-09
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 4
    Publication Date: 2011-05-25
    Description: Converging data from rodents and humans have demonstrated an age-related decline in pattern separation abilities (the ability to discriminate among similar experiences). Several studies have proposed the dentate and CA3 subfields of the hippocampus as the potential locus of this change. Specifically, these studies identified rigidity in place cell remapping in similar environments in the CA3. We used high-resolution fMRI to examine activity profiles in the dentate gyrus and CA3 in young and older adults as stimulus similarity was incrementally varied. We report evidence for “representational rigidity” in older adults’ dentate/CA3 that is linked to behavioral discrimination deficits. Using ultrahigh-resolution diffusion imaging, we quantified both the integrity of the perforant path as well as dentate/CA3 dendritic changes and found that both were correlated with dentate/CA3 functional rigidity. These results highlight structural and functional alterations in the hippocampal network that predict age-related changes in memory function and present potential targets for intervention.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 5
    Publication Date: 2011-12-01
    Print ISSN: 0048-9697
    Electronic ISSN: 1879-1026
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Published by Elsevier
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  • 6
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    PANGAEA
    In:  Supplement to: Stark, Nina; Kopf, Achim J (2013): In-situ geotechnical investigation of sediment remobilitzation processes utilizing geotechnical measurement techniques to detect, quantify and describe sediment erosion and deposition. Sea Technology, 54
    Publication Date: 2023-03-03
    Description: Dynamic penetrometer data obtained with the Nimrod penetrometer (MARUM). Data is presented as (i) penetration depth (including for different layers if present), (ii) measured deceleration and (iv) estimated quasi-static bearing capacity including range of uncertainty due to the processing method. Lat/Long coordinates are given.
    Keywords: Center for Marine Environmental Sciences; Deceleration; Event label; Latitude of event; Layer number; Longitude of event; MARUM; NIM; NIMROD; Number; Penetration depth; Quasi-static bearing capacity; Raglan_1; Raglan_10; Raglan_11; Raglan_13; Raglan_15; Raglan_16; Raglan_17; Raglan_18; Raglan_19; Raglan_2; Raglan_20; Raglan_21; Raglan_3; Raglan_4; Raglan_5; Raglan_6; Raglan_7; Raglan_8; Raglan_9; Raglan, New Zealand; Uncertainty
    Type: Dataset
    Format: text/tab-separated-values, 178 data points
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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: Stark, Nina; Hanff, Hendrik; Svenson, C; Ernstsen, Verner Brandbyge; Lefebvre, Alice; Winter, Christian; Kopf, Achim J (2011): Coupled penetrometer, MBES and ADCP assessments of tidal variations in surface sediment layer characteristics along active subaqueous dunes, Danish Wadden Sea. Geo-Marine Letters, 31(4), 249-258, https://doi.org/10.1007/s00367-011-0230-6
    Publication Date: 2023-04-20
    Description: In-situ geotechnical measurements of surface sediments were carried out along large subaqueous dunes in the Knudedyb tidal inlet channel in the Danish Wadden Sea using a small free-falling penetrometer. Vertical profiles showed a typical stratification pattern with a resolution of ~1 cm depicting a thin surface layer of low sediment strength and a stiffer substratum below (quasi-static bearing capacity equivalent: 1–3 kPa in the top layer, 20–140 kPa in the underlying sediment; thickness of the top layer ca. 5–8 cm). Observed variations in the thickness and strength of the surface layer during a tidal cycle were compared to mean current velocities (measured using an acoustic Doppler current profiler, ADCP), high-resolution bathymetry (based on multibeam echo sounding, MBES) and qualitative estimates of suspended sediment distributions in the water column (estimated from ADCP backscatter intensity). The results revealed an ebb dominance in sediment remobilization, and a general accretion of the bed towards low water. A loose top layer occurred throughout the tidal cycle, likely influenced by bedload transport and small events of suspended sediment resettlement (thickness: 6 +-2 cm). Furthermore, this layer showed a significant increase in thickness (e.g. from 8 cm to 16 cm) related to periods of overall deposition. These findings imply that dynamic penetrometers can conveniently serve to (1) quantify potentially mobile sediments by determining the thickness of a loose sediment surface layer, (2) unravel sediment strength development in potentially mobile sediments and (3) identify sediment accumulation. Such data are an important complement and add a new geotechnical perspective during investigations of sediment remobilization processes in highly dynamic coastal environments.
    Keywords: Center for Marine Environmental Sciences; Deceleration; Event label; Free fall penetrometer, NIMROD; Knudedyb, Denmark; MARUM; N1; N10; N11; N12; N13; N14; N15; N16; N17; N18; N19; N2; N20; N21; N22; N23; N24; N25; N26; N27; N28; N29; N3; N30; N31; N32; N33; N34; N35; N36; N37; N38; N39; N4; N40; N41; N42; N43; N44; N45; N46; N47; N48; N49; N5; N50; N51; N52; N53; N54; N55; N56; N57; N58; N59; N6; N60; N61; N62; N63; N64; N65; N66; N67; N68; N69; N7; N70; N71; N72; N73; N74; N75; N76; N77; N78; N79; N8; N80; N81; N82; N83; N88; N89; N9; N90; N91; N92; N94; N95; N96; N97; NIM; NIMROD; Penetration depth; Penetration velocity; Senckenberg; Senckenberg_11_2008; Senckenberg_11_2008_N1; Senckenberg_11_2008_N10; Senckenberg_11_2008_N11; Senckenberg_11_2008_N12; Senckenberg_11_2008_N13; Senckenberg_11_2008_N14; Senckenberg_11_2008_N15; Senckenberg_11_2008_N16; Senckenberg_11_2008_N17; Senckenberg_11_2008_N18; Senckenberg_11_2008_N19; Senckenberg_11_2008_N2; Senckenberg_11_2008_N20; Senckenberg_11_2008_N21; Senckenberg_11_2008_N22; Senckenberg_11_2008_N23; Senckenberg_11_2008_N24; Senckenberg_11_2008_N25; Senckenberg_11_2008_N26; Senckenberg_11_2008_N27; Senckenberg_11_2008_N28; Senckenberg_11_2008_N29; Senckenberg_11_2008_N3; Senckenberg_11_2008_N30; Senckenberg_11_2008_N31; Senckenberg_11_2008_N32; Senckenberg_11_2008_N33; Senckenberg_11_2008_N34; Senckenberg_11_2008_N35; Senckenberg_11_2008_N36; Senckenberg_11_2008_N37; Senckenberg_11_2008_N38; Senckenberg_11_2008_N39; Senckenberg_11_2008_N4; Senckenberg_11_2008_N40; Senckenberg_11_2008_N41; Senckenberg_11_2008_N42; Senckenberg_11_2008_N43; Senckenberg_11_2008_N44; Senckenberg_11_2008_N45; Senckenberg_11_2008_N46; Senckenberg_11_2008_N47; Senckenberg_11_2008_N48; Senckenberg_11_2008_N49; Senckenberg_11_2008_N5; Senckenberg_11_2008_N50; Senckenberg_11_2008_N51; Senckenberg_11_2008_N52; Senckenberg_11_2008_N53; Senckenberg_11_2008_N54; Senckenberg_11_2008_N55; Senckenberg_11_2008_N56; Senckenberg_11_2008_N57; Senckenberg_11_2008_N58; Senckenberg_11_2008_N59; Senckenberg_11_2008_N6; Senckenberg_11_2008_N60; Senckenberg_11_2008_N61; Senckenberg_11_2008_N62; Senckenberg_11_2008_N63; Senckenberg_11_2008_N64; Senckenberg_11_2008_N65; Senckenberg_11_2008_N66; Senckenberg_11_2008_N67; Senckenberg_11_2008_N68; Senckenberg_11_2008_N69; Senckenberg_11_2008_N7; Senckenberg_11_2008_N70; Senckenberg_11_2008_N71; Senckenberg_11_2008_N72; Senckenberg_11_2008_N73; Senckenberg_11_2008_N74; Senckenberg_11_2008_N75; Senckenberg_11_2008_N76; Senckenberg_11_2008_N77; Senckenberg_11_2008_N78; Senckenberg_11_2008_N79; Senckenberg_11_2008_N8; Senckenberg_11_2008_N80; Senckenberg_11_2008_N81; Senckenberg_11_2008_N82; Senckenberg_11_2008_N83; Senckenberg_11_2008_N88; Senckenberg_11_2008_N89; Senckenberg_11_2008_N9; Senckenberg_11_2008_N90; Senckenberg_11_2008_N91; Senckenberg_11_2008_N92; Senckenberg_11_2008_N94; Senckenberg_11_2008_N95; Senckenberg_11_2008_N96; Senckenberg_11_2008_N97
    Type: Dataset
    Format: text/tab-separated-values, 13134 data points
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Stark, Nina; Coco, Giovanni; Bryan, Karin R; Kopf, Achim J (2012): In-situ geotechnical characterization of mixed-grain-size bedforms using a dynamic penetrometer. Journal of Sedimentary Research, 82(7-8), 540-544, https://doi.org/10.2110/jsr.2012.45
    Publication Date: 2023-07-11
    Description: We tested the ability of a small dynamic penetrometer, Nimrod, to infer geotechnical properties of sediment mixtures in the inner shelf. The penetrometer is light and easy to operate, and its operation by scuba divers ensures a greater degree of precision than ship-based penetrometer deployments. We have studied selected positions along a sorted bedform (~ 100 m wide) on the continental shelf off the Coromandel Peninsula close to Tairua, North Island of New Zealand, and additionally took sediment samples at the exact positions of penetrometer impact, also by scuba divers. The derived dynamic penetrometer signatures (i) measured deceleration of the probe and estimated quasi-static bearing capacity as a measure of sediment strength, (ii) reflected changes in grain-size distribution ranging from very fine to very coarse sands, and (iii) revealed the uppermost seafloor stratification (top layer 2-6 cm) potentially being an indicator for sediment dynamics. In this manner, the device proved to be suitable for spatially fine-scaled surveys using divers' support and might deliver complementary information about sediment dynamics, in this case sorted-bedform maintenance.
    Keywords: Calculated; Center for Marine Environmental Sciences; Comment; Deceleration; Distance; Event label; Layer thickness; MARUM; NIM; NIMROD; Number; Penetration depth; Penetration velocity; Quasi-static bearing capacity; Sediment type; Site; Size fraction; Tairua_T1_M; Tairua_T1_S; Tairua_T10_M; Tairua_T10_S; Tairua_T11_M; Tairua_T11_N; Tairua_T12_M; Tairua_T12_N; Tairua_T13_M; Tairua_T13_N; Tairua_T14_M; Tairua_T14_N; Tairua_T15_M; Tairua_T15_N; Tairua_T16_M; Tairua_T16_N; Tairua_T17_M; Tairua_T17_N; Tairua_T18_M; Tairua_T18_N; Tairua_T19_M; Tairua_T19_N; Tairua_T2_M; Tairua_T2_S; Tairua_T20_M; Tairua_T20_N; Tairua_T3_M; Tairua_T3_S; Tairua_T4_M; Tairua_T4_S; Tairua_T5_M; Tairua_T5_S; Tairua_T6_M; Tairua_T6_S; Tairua_T7_M; Tairua_T7_S; Tairua_T8_M; Tairua_T8_S; Tairua_T9_M; Tairua_T9_S; Tairua Beach
    Type: Dataset
    Format: text/tab-separated-values, 412 data points
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  • 9
    Publication Date: 2014-07-14
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 10
    Publication Date: 2019-07-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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