globalchange  > 气候减缓与适应
DOI: 10.1016/j.quascirev.2018.03.011
Scopus记录号: 2-s2.0-85045926059
论文题名:
The marine isotope stage 1–5 cryptotephra record of Tenaghi Philippon, Greece: Towards a detailed tephrostratigraphic framework for the Eastern Mediterranean region
作者: Wulf S.; Hardiman M.J.; Staff R.A.; Koutsodendris A.; Appelt O.; Blockley S.P.E.; Lowe J.J.; Manning C.J.; Ottolini L.; Schmitt A.K.; Smith V.C.; Tomlinson E.L.; Vakhrameeva P.; Knipping M.; Kotthoff U.; Milner A.M.; Müller U.C.; Christanis K.; Kalaitzidis S.; Tzedakis P.C.; Schmiedl G.; Pross J.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2018
卷: 186
起始页码: 236
结束页码: 262
语种: 英语
英文关键词: Eastern Mediterranean region ; Italian volcanism ; Last glacial-interglacial cycle ; Peat record ; Santorini eruptions ; Tenaghi philippon ; Tephrochronology
Scopus关键词: Barium compounds ; Bayesian networks ; Climate change ; Peat ; Eastern Mediterranean ; Italian volcanism ; Last glacial ; Santorini eruptions ; Tenaghi philippon ; Tephrochronology ; Quality control ; environmental change ; glacial-interglacial cycle ; marine isotope stage ; Mediterranean environment ; paleoclimate ; peat ; tephrochronology ; volcanic eruption ; volcanism ; Central Macedonia ; Greece ; Serrai [Central Macedonia] ; Tenaghi Philippon
英文摘要: The iconic climate archive of Tenaghi Philippon (TP), NE Greece, allows the study of short-term palaeoclimatic and environmental change throughout the past 1.3 Ma. To provide high-quality age control for detailed palaeoclimate reconstructions based on the TP archive, (crypto)tephra studies of a peat core ‘TP-2005’ have been carried out for the 0–130 ka interval. The results show that the TP basin is ideally positioned to receive tephra fall from both the Italian and Aegean Arc volcanic provinces. Two visible tephra layers, the Santorini Cape Riva/Y-2 (c. 22 ka) and the Campanian Ignimbrite (CI)/Y-5 (c. 39.8 ka) tephras, and six primary cryptotephra layers, namely the early Holocene E1 tephra from the Aeolian Islands (c. 8.3 ka), the Campanian Y-3 (c. 29 ka) and X-6 tephras (c. 109.5 ka), as well as counterpart tephras TM-18-1d (c. 40.4 ka), TM-23-11 (c. 92.4 ka) and TM-33-1a (c. 116.7 ka) from the Lago Grande di Monticchio sequence (southern Italy), were identified along with repeatedly redeposited Y-2 and CI tephra material. Bayesian modelling of the ages of seven of the primary tephra layers, 60 radiocarbon measurements and 20 palynological control points have been applied to markedly improve the chronology of the TP archive. This revised chronology constrains the age of tephra TM-18-1d to 40.90–41.66 cal ka BP (95.4% range). Several tephra layers identified in the TP record form important isochrons for correlating this archive with other terrestrial (e.g., Lago Grande di Monticchio, Sulmona Basin and Lake Ohrid) and marine (e.g., Adriatic Sea core PRAD 1-2 and Aegean Sea core LC21) palaeoclimate records in the Mediterranean region. © 2018 Elsevier Ltd
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/112250
Appears in Collections:气候减缓与适应

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作者单位: Senckenberg Research Institute and Natural History Museum, Senckenberganlage 25, Frankfurt, D-60325, Germany; Institute of Earth Sciences, Heidelberg University, Im Neuenheimer Feld 234-236, Heidelberg, D-69120, Germany; Department of Geography, University of Portsmouth, Buckingham Building, Lion Terrace, Portsmouth, PO1 3HE, United Kingdom; Scottish Universities Environmental Research Centre (SUERC), University of Glasgow, Scottish Enterprise Technology Park, Rankine Avenue, East Kilbride, G75 0QF, United Kingdom; Research Laboratory for Archaeology and the History of Art, University of Oxford, 1-2 South Parks Rd, Oxford, OX1 3TG, United Kingdom; Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Section 4.3 Chemistry and Physics of Earth Materials, Telegrafenberg, Potsdam, D-14773, Germany; Centre for Quaternary Research, Department of Geography, Royal Holloway, University of London, Egham, Surrey, TW20 0EX, United Kingdom; National Research Council of Italy (CNR)-Institute of Geosciences and Earth Resources (IGG), Unit of Pavia, Via A. Ferrata 1, Pavia, 27100, Italy; Department of Geology, Trinity College Dublin, The University of Dublin, Dublin 2, Ireland; Institute of Botany, University of Hohenheim, Garbenstraße 30, Stuttgart, D-70593, Germany; Center for Natural History, University of Hamburg, Bundesstraße 55, Hamburg, D-20146, Germany; Institute for Geology, University of Hamburg, Bundesstrasse 55, Hamburg, D-20146, Germany; Parlamentsstraße 32, Frankfurt, D-60385, Germany; Department of Geology, University of Patras, Rio-Patras, GR-26504, Greece; Environmental Change Research Centre, Department of Geography, University College London, Pearson Building, Gower Street, London, WC1E 6BT, United Kingdom; Center for Earth System Research and Sustainability, University of Hamburg, Bundesstrasse 55, Hamburg, D-20146, Germany

Recommended Citation:
Wulf S.,Hardiman M.J.,Staff R.A.,et al. The marine isotope stage 1–5 cryptotephra record of Tenaghi Philippon, Greece: Towards a detailed tephrostratigraphic framework for the Eastern Mediterranean region[J]. Quaternary Science Reviews,2018-01-01,186
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