ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

X
feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Collection
Keywords
Publisher
Years
  • 1
    Monograph available for loan
    Monograph available for loan
    Speleothem science : from process to past environments (2012)
    Chichester [u.a.] : Wiley-Blackwell
    Details Availability
    Call number: PIK N 421-13-0175
    Description / Table of Contents: Contents: I Scientifi c and geological context ; 1 Introduction to speleothems and systems ; 2 Carbonate and karst cave geology ; 3 Surface environments: climate, soil and vegetation ; II Transfer processes in karst ; 4 The speleothem incubator ; 5 Inorganic water chemistry ; 6 Biogeochemistry of karstic environments ; III Speleothem properties ; 7 The architecture of speleothems ; 8 Geochemistry of speleothems ; 9 Dating of speleothems ; IV Palaeoenvironments ; 10 The instrumental era: calibration and validation of proxy-environment relationships ; 11 The Holocene epoch: testing the climate and environmental proxies ; 12 The Pleistocene and beyond ; APPENDIX 1 Archiving speleothems and speleothem data
    Type of Medium: Monograph available for loan
    Pages: XIV, 432 S. : Ill., zahlr. graph. Darst., Kt.
    ISBN: 9781405196208
    Series Statement: Blackwell quaternary geoscience series
    Location: A 18 - must be ordered
    Branch Library: PIK Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    BOOK
    Link to Library Catalog
    get availability status
  • 2
    Electronic Resource
    Electronic Resource
    Fluorescence of Dissolved Organic Matter as a Natural Tracer of Ground Water (2001)
    Oxford, UK : Blackwell Publishing Ltd
    Ground water 39 (2001), S. 0 
    Details
    ISSN: 1745-6584
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences
    Notes: The fluorescence properties of dissolved organic matter (DOM) in ground water in the Permian limestone of northeast England is determined from six monitoring boreholes, a private water supply well and from a natural resurgence in a flooded collapse doline in the environs of Darlington, County Durham, northeast England. Measurements of both protein and “fulvic-like” fluorescence was undertaken from January to December 1999. The wavelengths of fulvic-like fluorescence excitation and emission and of protein fluorescence emission were all determined to be sensitive fingerprints of organic matter fluxes through the ground water, with water within the till and within both gypsum and limestone strata deep inside the Magnesian Limestone being differentiated by these parameters. Previous research has suggested that proteins in waters are “young” in age, hence our seasonal variations suggest that we are sampling recently formed DOM. The rapid response of all deep borehole samples suggests relatively rapid ground water flow, probably through karstic cave systems developed in the gypsum and solution widened features in the dolomitic limestone. Our results suggest that use of both protein and fulvic-like fluorescence wavelength variations provides a DOM signature that can be used as a natural tracer.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1745-6584.2001.tb02365.x
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    Paper (German National Licenses)
    Fulltext
  • 3
    Electronic Resource
    Electronic Resource
    Annual growth banding in a cave stalagmite (1993)
    [s.l.] : Nature Publishing Group
    Nature 364 (1993), S. 518-520 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Forty-three speleothem samples were collected from karst areas in the United Kingdom. After cutting along the axis of growth, 2-mm-thick polished sections were prepared. These were observed under a standard Zeiss microscope fitted with an IV Fl epi-fluorescence condenser containing a 50 W ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/364518a0
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    Paper (German National Licenses)
    Fulltext
  • 4
    facet.materialart.
    Unknown
    Global analysis reveals climatic controls on the oxygen isotope composition of cave drip water (2019)
    Nature Publishing Group
    In:  EPIC3Nature Communications, Nature Publishing Group, 10(1), pp. 1-7, ISSN: 2041-1723
    Details
    Publication Date: 2019-07-15
    Description: The oxygen isotope composition of speleothems is a widely used proxy for past climate change. Robust use of this proxy depends on understanding the relationship between precipitation and cave drip water δ18O. Here, we present the first global analysis, based on data from 163 drip sites, from 39 caves on five continents, showing that drip water δ18O is most similar to the amount-weighted precipitation δ18O where mean annual temperature (MAT) is 〈 10 °C. By contrast, for seasonal climates with MAT 〉 10 °C and 〈 16 °C, drip water δ18O records the recharge-weighted δ18O. This implies that the δ18O of speleothems (formed in near isotopic equilibrium) are most likely to directly reflect meteoric precipitation in cool climates only. In warmer and drier environments, speleothems will have a seasonal bias toward the precipitation δ18O of recharge periods and, in some cases, the extent of evaporative fractionation of stored karst water.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    PAPER (OA)
  • 5
    facet.materialart.
    Unknown
    United States Groundwater Chemistry - Dissolved Organic Carbon Model (2019)
    PANGAEA
    In:  Supplement to: McDonough, Liza K; Santos, Isaac R; Andersen, Martin; O'Carroll, Denis; Rutlidge, Helen; Meredith, Karina; Oudone, Phetdala; Baker, Andy (2018): Changes in global groundwater organic carbon driven by climate change and urbanization. EarthArXiv Preprints, 11 pp, https://doi.org/10.31223/osf.io/vmaku
    Details
    Publication Date: 2023-03-14
    Description: This data set is predominantly sourced from the National Water Quality Monitoring Council (https://www.waterqualitydata.us/portal) and contains water quality data for the United States as well as climate and other ancillary data. This data was used to develop a model to explain groundwater dissolved organic carbon concentrations in the manuscript "Changes in global groundwater organic carbon driven by climate change and urbanization". Units for variables are included in the file "Units for Variables". --- National Water Quality Monitoring Council water chemistry data (https://www.waterqualitydata.us/portal) was obtained from: Chapelle, F. H., Bradley, P. M., Journey, C. A., & McMahon, P. B. (2013). Assessing the Relative Bioavailability of DOC in Regional Groundwater Systems. Ground water 51(3), doi:10.1111/j.1745-6584.2012.00987.x. --- Water table depth data obtained from: Fan, Y., Li, H., & Miguez-Macho, G. (2013). Global patterns of groundwater table depth. Science, 339, 940–943, doi:10.1126/science.1229881. --- Climatic data obtained from www.worldclim.org: Hijmans, R. J., Cameron, S. E., Parra, J. L., Jones, P. G., & Jarvis, A. (2005). Very high resolution interpolated climate surfaces for global land areas. International Journal of Climatology, 25, 1965-1978, doi:10.1002/joc.1276. --- Land use data obtained from: Channan, S., Collins, K., & Emanuel, W. R. (2014). Global mosaics of the standard MODIS land cover type data. University of Maryland and the Pacific Northwest National Laboratory, College Park, Maryland, USA. Retrieved from University of Maryland and the Pacific Northwest National Laboratory. - Friedl, M. A., Sulla-Menasche, D., Tan, B., Schneider, A., Ramankutty, N., Sibley, A., & Huang, X. (n.d.). MODIS Collection 5 global land cover: Algorithm refinements and characterization of new datasets, 2001-2012. Collection 5.1 IGBP Land Cover. Boston University, Boston, MA, USA.
    Keywords: Age, comment; Alabama; Area/locality; Arkansas; Arsenic; Calcium; California; Carbon, organic, dissolved; Chloride; Colorado; Conductivity, electrical; Connecticut; Continent; Country; Delaware; Depth, groundwater table; Depth, well; ELEVATION; Event label; Florida; Fluoride; Georgia; Idaho; Illinois; Indiana; Iowa; Iron; Kansas; Land use; LATITUDE; Lithology/composition/facies; LONGITUDE; Louisiana; Magnesium; Manganese; Maryland; Massachusetts; Michigan; Minnesota; Mississippi; Missouri; MULT; Multiple investigations; Nebraska; Nevada; New Hampshire; New Jersey; New Mexico; New York; North Carolina; North Dakota; Number; Ohio; Oklahoma; Oxygen, dissolved; Pennsylvania; pH; Potassium; Precipitation, annual mean; Precipitation, mean; Precipitation of the driest month; Precipitation of the wettest month; Ratio; Sample ID; Silica, dissolved; Sodium; South Carolina; South Dakota; Sulfate; Temperature, annual range; Temperature, coldest month, minimum; Temperature, mean; Temperature, range daily; Temperature, warmest month, maximum; Temperature, water; Temperature, water, annual mean; Tennessee; Texas; United States; US-AL; US-AR; US-CA; US-CO; US-CT; US-DE; US-FL; US-GA; US-IA; US-ID; US-IL; US-IN; US-KS; US-LA; US-MA; US-MD; US-MI; US-MN; US-MO; US-MS; US-NC; US-ND; US-NE; US-NH; US-NJ; US-NM; US-NV; US-NY; US-OH; US-OK; US-PA; US-SC; US-SD; US-TN; US-TX; US-UT; US-VA; US-VT; US-WA; US-WI; US-WV; US-WY; Utah; Vermont; Virginia; Washington; West Virginia; Wisconsin; Wyoming
    Type: Dataset
    Format: text/tab-separated-values, 232522 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 6
    facet.materialart.
    Unknown
    Golgotha Cave stalagmite records 1 ka (2022)
    PANGAEA
    Details
    Publication Date: 2024-02-03
    Description: Stalagmites GL-S1, GL-S2, GL-S3 and GL-S4 were collected under scientific license issued by Western Australia's Department of Biodiversity, Conservation and Attractions from Golgotha Cave (34.1°S, 115.1°E) in southwest Western Australia, with collection dates of 2005, 2005, 2008 and 2012, respectively. Cave location is rounded to nearest tenth of a degree as exact locations not disclosed for cave conservation purposes. Speleothems were collected for paleoclimate and paleohydrology studies. Golgotha Cave is located in Eucalyptus forest with dense understorey in the Leeuwin-Naturaliste National Park. The hostrock is Quaternary aeolinite and the soil thickness is variable with measurements ranging from 0.3-3 m deep. The cave entrance is 70 m above sea level. Stalagmites GL-S1 and GL-S4 are located approximately 60 m from the entrance where the limestone thickness overhead is 30 m while GL-S2 and GL-S3 are located approximately 90 m from the entrance where the limestone thickness overhead is 40 m. Mean annual site temperature is 15.6 ±0.5°C and mean annual rainfall is 1101±157 mm (1911-2018 period; Australian Bureau of Meteorology AWRA-L dataset http://www.bom.gov.au/water/landscape. Inside the cave, temperature ranges from 14.5-14.8°C, windspeed is low (≤0.03 m s-1) and relative humidity ranges from 98-100% (Treble et al 2019). Each speleothem was sectioned along the growth axis and milled using a Taig micromill to produce homogenised powders representing increments of 0.1 to 0.2 mm, depending on the speleothem growth rate. Powders were weighed to 180–220 μg and analysed for O and C isotopic values (δ18O and δ13C) using a Finnigan MAT-251 isotope ratio mass spectrometer coupled to a Kiel I carbonate device, or a Thermo MAT-253 isotope ratio mass spectrometer coupled to a Kiel IV carbonate device (using 110–130 μg samples), at the Research School of Earth Sciences, ANU. Analyses were calibrated using NBS-19 standard (δ18Ov-PDB = -2.20 ‰ and δ13Cv-PDB = 1.95 ‰). A further linear correction for δ18O measurements was carried out using the NBS-18 standard (δ18Ov-PDB = -23.0 ‰). The original delta values for NBS-19 and NBS-18 are used to maintain consistency of results through time in the RSES Stable Isotope Facility. Analytical precision for the analyses reported here (NBS-19) are ±0.04 ‰ for δ18O and ±0.02 ‰ for δ13C (N=236) for the MAT-251; and ±0.05 ‰ for δ18O and ±0.01 ‰ (N=27) for the MAT-253 instrument (±1σ standard deviation). Speleothem chronologies were determined by combining information from the date of collection, bomb pulse chronology, laminae counting of annual Sr concentration and U-series disequilibrium (see Supplementary Table 8 in Treble et al., 2022). For GL-S1, the age-depth model for 17th percentile was used in Treble et al., (2022) and the 50th percentile used for other stalagmites.
    Keywords: Golgotha Cave; Last millennium; speleothem; stalagmite; Western Australia
    Type: Dataset
    Format: application/zip, 10 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 7
    facet.materialart.
    Unknown
    Age chronology based on U/Th ages, bomb pulse 14C data and year of collection (2012) of Stalagmite GL-S1 from the Golgotha Cave in southwest Western Australia (2022)
    PANGAEA
    Details
    Publication Date: 2024-02-03
    Description: Stalagmite GL-S1 chronology in ka CE based on U/Th ages, bomb pulse 14C data and year of collection (2005). Treble et al. (2022) used 17th percentile age-depth model.
    Keywords: Age; Determined according to Treble et al. (2021); DISTANCE; Golgotha_Cave; Golgotha Cave; Last millennium; speleothem; stalagmite; Western Australia
    Type: Dataset
    Format: text/tab-separated-values, 260 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 8
    facet.materialart.
    Unknown
    δ13C and δ18O record of Stalagmite GL-S1 from the Golgotha Cave in southwest Western Australia (2022)
    PANGAEA
    Details
    Publication Date: 2024-02-03
    Description: GolgothaCave_GLS1_stalagmite_O&C_isotopes: median depth, d18O and d13C values in VPDB. Chronology is that used for Treble et al (2022).
    Keywords: Age; Determined according to Treble et al. (2021); DISTANCE; Golgotha_Cave; Golgotha Cave; Last millennium; Mass spectrometer Finnigan MAT 251; Sample ID; speleothem; stalagmite; Western Australia; δ13C; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 532 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 9
    facet.materialart.
    Unknown
    Drip water analysis of site 1A, 1IV, 2B and 2E from the Golgotha Cave in southwest Western Australia (2022)
    PANGAEA
    Details
    Publication Date: 2024-02-03
    Description: Dripwater was collected every 4-6 weeks from Golgotha Cave (34.1°S, 115.1°E) in southwest Western Australia from 2005 until 2019, although beginning in 2008 for site 2E and in 2013 for site 1IV. Cave location is rounded to nearest tenth of a degree as exact locations not disclosed for cave conservation purposes. Dripwaters were collected for paleoclimate and paleohydrology studies. Data from August 2005 until March 2012 were previously published in Treble et al. (2013) and the longer dataset in Treble et al (2021). Please cite Treble et al. (2013, 2021) when using these data. Dripwaters were collected at 4-6 week intervals from bulk 1 L high-density polyethylene collection vessels, fitted with funnels, that were emptied following collection of water for analyses. Drip rates were manually timed during each collection visit. The drip sites pair with stalagmites collected from these locations as follows: site 1A (GL-S1), site 1IV (GL-S4), site 2B (GL-S2), site 2E (GL-S3). Stable water isotopes (δ18O and δ2H) collected between August 2005 and April 2011 were determined by: 1. offline equilibration technique at the Research School of Earth Sciences, Australian National University; 2. using an LGR-24 d cavity ringdown mass spectrometer at the University of New South Wales for samples from May 2011-March 2012; and 3. using Picarro L2120-I Water Analyser at ANSTO from 2012 onwards. Analytical error all techniques was 0.1 ‰ (1 s.d.; calculated from within-run internal references materials). See citations in Treble et al. (2013) for details of methods. Golgotha Cave is located in Eucalyptus forest with dense understorey in the Leeuwin-Naturaliste National Park. The hostrock is Quaternary aeolinite and the soil thickness is variable with measurements ranging from 0.3 – 3 m deep. The cave entrance is 70 m above sea level. Dripwater sites 1A, 1IV are located approximately 60 m from the entrance where the limestone thickness overhead is 30 m while dripwater sites 2B and 2E are located approximately 90 m from the entrance where the limestone thickness overhead is 40 m. Mean annual site temperature is 15.6 ±0.5°C and mean annual rainfall is 1101±157 mm (1911-2018 period; Australian Bureau of Meteorology AWRA-L dataset http://www.bom.gov.au/water/landscape. Inside the cave, temperature ranges from 14.5-14.8°C, windspeed is low (≤0.03 m s-1) and relative humidity ranges from 98-100% (Treble et al 2019). Rainfall water isotope measurements from Calgardup Cave, located 5 km from Golgotha Cave and complimentary to this dataset, are available from the IAEA Water Isotope System for data analysis, visualization and Electronic Retrieval, https://nucleus.iaea.org/wiser/ using station code 9564101.
    Keywords: cave monitoring; dripwater; water isotopes; Western Australia
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 10
    facet.materialart.
    Unknown
    Age chronology (modern) based on U/Th ages, bomb pulse 14C data and year of collection (2012) of Stalagmite GL-S3 from the Golgotha Cave in southwest Western Australia (2022)
    PANGAEA
    Details
    Publication Date: 2024-02-03
    Description: Stalagmite GL-S3 chronology in Years CE for upper 4 mm based on laminae count and year of collection (2008).
    Keywords: Age; Determined according to Treble et al. (2021); DISTANCE; Golgotha_Cave; Golgotha Cave; Last millennium; speleothem; stalagmite; Western Australia
    Type: Dataset
    Format: text/tab-separated-values, 177 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...