ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

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
  • Last Interglacial  (2)
  • AGE; Age, maximum/old; Age, minimum/young; Age model; Age model, Bacon (Blaauw & Christen, 2011); Apennines; Bayesian; Calcium; Carbon, inorganic, total; Carbon, organic, total; Carbon, organic, total/Nitrogen, total ratio; CDRILL; centennial; Central; change; Coherent scatter, counts; Core; Core drilling; Depth, composite; DEPTH, sediment/rock; Eemian; environmental; F1; F3; Fucino; Fucino_F1-3; Holocene; independent; Italy; lake; Mediterranean; millennial; MIS 1; MIS 2; MIS 3; MIS 4; MIS 5; MIS 6; multiproxy; Nitrogen, total; orbital; Position, length; Saalian; Sample ID; Size fraction 〈 15.6 µm, 6.0 phi; Tephra; Titanium; Weichselian; X-ray fluorescence ITRAX core scanner; XRF; Zirconium  (1)
Collection
Keywords
Publisher
Years
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Mannella, Giorgio; Giaccio, Biagio; Zanchetta, Giovanni; Regattieri, Eleonora; Niespolo, Elizabeth M; Pereira, Alison; Renne, Paul; Nomade, Sébastien; Leicher, Niklas; Perchiazzi, Natale; Wagner, Bernd (2019): Palaeoenvironmental and palaeohydrological variability of mountain areas in the central Mediterranean region: A 190 ka-long chronicle from the independently dated Fucino palaeolake record (central Italy). Quaternary Science Reviews, 210, 190-210, https://doi.org/10.1016/j.quascirev.2019.02.032
    Publication Date: 2023-12-15
    Description: Here we present a multi-proxy record from palaeolake Fucino (Abruzzo, Central Italy), acquired during the F1-F3 drilling campaign. This is the first continuous and high-resolution palaeoenvironmental record in the central Mediterranean region continuously spanning over the last two glacial-interglacial cycles and providing an independent chronology. The record consists of a core composite resulting from two parallel and adjacent core series (F1 and F3). Cores were analysed via high resolution XRF scanning and through geochemical, mineralogical and grain-size analyses on discrete samples. Selected XRF elemental counts (Ca, Ti and Zr), Total Nitrogen (TN), Total Organic and Inorganic Carbon (TOC, TIC), X-ray powder diffraction and grain-size data are used to develop proxies for local environmental processes strictly dependent on the hydro-climatic regime of the Central Mediterranean region. The chronology of the record is based on 17 radioisotopically dated tephra layers interbedded within the sedimentary succession. 14C and 40Ar/39Ar age points are interpolated with the bayesian age modelling package Bacon allowing a robust assessment of age uncertainties.
    Keywords: AGE; Age, maximum/old; Age, minimum/young; Age model; Age model, Bacon (Blaauw & Christen, 2011); Apennines; Bayesian; Calcium; Carbon, inorganic, total; Carbon, organic, total; Carbon, organic, total/Nitrogen, total ratio; CDRILL; centennial; Central; change; Coherent scatter, counts; Core; Core drilling; Depth, composite; DEPTH, sediment/rock; Eemian; environmental; F1; F3; Fucino; Fucino_F1-3; Holocene; independent; Italy; lake; Mediterranean; millennial; MIS 1; MIS 2; MIS 3; MIS 4; MIS 5; MIS 6; multiproxy; Nitrogen, total; orbital; Position, length; Saalian; Sample ID; Size fraction 〈 15.6 µm, 6.0 phi; Tephra; Titanium; Weichselian; X-ray fluorescence ITRAX core scanner; XRF; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 30089 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2018-03-30
    Description: A trace element record (Mg, Sr, Ba, Al, Si, P, Y, Zn) covering the ca. 133 ka to ca. 124 ka time interval was acquired from a flowstone core from Tana che Urla Cave (central Italy). It was compared with stable isotope data to investigate the environmental evolution in response to regional and extra-regional climate changes in the period corresponding to the latter part of the Penultimate Deglaciation and the first part of the Last Interglacial (Eemian). Trace element geochemical changes on centennial and millennial time scales responded to changes in hydrological input, variations in the supply and transport of catchment erosion products to the cave, including those linked to intense rainfall events, and to the state of the overlying soil and vegetation. Abrupt increases in precipitation and the progressive development of soil and vegetation occurred at ca. 132 ka, in response to the development of the global deglacial phase. The major changes in trace element composition are coherent with the previous hydrological interpretation of speleothem oxygen stable isotope composition (δ18O) as predominantly a rainfall-amount proxy. However, reduced growth rate persisted until ca. 130 ka, suggesting still depressed temperatures. An abrupt event of climatic deterioration, with marked decrease in precipitation and soil degradation, is apparent between ca. 131 and 130 ka. Cool-wet conditions between ca. 132 and 131 ka and the subsequent dry period may represent the local hydrological response to an interval of North Atlantic cooling and ice-rafted-debris (IRD) deposition known as Heinrich event 11 (H11). After 129.6 ka there was a rapid recovery according to all of the studied speleothem properties, indicating the onset of full interglacial conditions. A minor amplitude event of reduced precipitation is recorded within the LIG at ca. 127 ka. The record highlights the growing regional evidence for a complex penultimate deglacial climate involving major reorganization of oceanic and atmospheric patterns.
    Description: Published
    Description: 80-92
    Description: 5A. Paleoclima e ricerche polari
    Description: JCR Journal
    Keywords: trace elements ; Penultimate deglaciation ; Last Interglacial
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2024-01-29
    Description: The current rapid change of the Earth’s climate has resulted in an increasing interest for the past warm periods as potential long-term scenarios of the effects of the present global warming. The last such a period occurred 129–116 ka, known as the Last Interglacial (LIG), when the continental ice volume was significantly smaller than present, leading to a global sea-level (GSL) higher than present one. Detailed morpho-stratigraphic data, supported by a robust U/Th chronology, from Grotta delle Capre, central Italy, provided new chronological insights on the relative sea-level (RSL) dynamic during the LIG in the Mediterranean region. Our results indicate that, on Tyrrhenian Sea coasts of the central Italy, after having stationed at ~9 m a.s.l., the LIG RSL fell at an elevation 〈3 m a.s.l. as early as before 123 ka, and then no longer rose above this elevation either during the later stages of the LIG or afterwards. The results match previous studies based on U/Th dating of terrestrial limiting points from Grotta Infreschi, ~200 km SE from Grotta delle Capre along the same Tyrrhenian Sea coasts, and are in agreement with the Red Sea RLS and GSL records and the probabilistic LIG sea level assessments based on globally distributed records. On the other hand, our reconstruction is not supported by implications of U/Th dating of corals and phreatic overgrowth on speleothems from the Balearic Island of Mallorca. Such an inconsistency in the overall knowledge around the LIG RSL reconstruction results in a high uncertainty in modelling the ice and sea-level dynamic during this warm period, which needs to be reduced through more and more highresolution, stratigraphic and chronological investigations of the morphological and sedimentary sea-level records.
    Description: Published
    Description: 104321
    Description: OSA2: Evoluzione climatica: effetti e loro mitigazione
    Description: JCR Journal
    Keywords: Last Interglacial ; relative sea level ; U/Th chronology ; Terrestrial limiting points ; Mediterranean
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...