onr:"swepub:oai:DiVA.org:su-103998"
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| Fältnamn | Indikatorer | Metadata |
|---|---|---|
| 000 | 03415naa a2200457 4500 | |
| 001 | oai:DiVA.org:su-103998 | |
| 003 | SwePub | |
| 008 | 140527s2014 | |||||||||||000 ||eng| | |
| 024 | 7 | a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1039982 URI |
| 024 | 7 | a https://doi.org/10.1016/j.yqres.2013.12.0092 DOI |
| 040 | a (SwePub)su | |
| 041 | a engb eng | |
| 042 | 9 SwePub | |
| 072 | 7 | a ref2 swepub-contenttype |
| 072 | 7 | a art2 swepub-publicationtype |
| 100 | 1 | a Finné, Martinu Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)4 aut0 (Swepub:su)mafi0763 |
| 245 | 1 0 | a Speleothem evidence for late Holocene climate variability and floods in Southern Greece |
| 264 | c 2017-01-20 | |
| 264 | 1 | b Cambridge University Press (CUP),c 2014 |
| 338 | a print2 rdacarrier | |
| 500 | a AuthorCount:6; | |
| 520 | a We present stable isotope data (delta O-18, delta C-13) from a detrital rich stalagmite from Kapsia Cave, the Peloponnese, Greece. The cave is rich in archeological remains and there are reasons to believe that flooding of the cave has directly affected humans using the cave. Using a combination of U-Th and C-14 dating to constrain a site-specific correction factor for (Th-232/U-238) detrital molar ratio, a linear age model was constructed. The age model shows that the stalagmite grew during the period from ca. 950 BC to ca. AD 830. The stable oxygen record from Kapsia indicates cyclical changes of close to 500 yr in precipitation amount, with rapid shifts towards wetter conditions followed by slowly developing aridity. Superimposed on this signal, wetter conditions are inferred around 850, 700, 500 and 400-100 BC, and around AD 160-300 and AD 770; and driest conditions are inferred to have occurred around 450 BC, AD 100-150 and AD 650. Detrital horizons in the stalagmite indicate that three major floods took place in the cave at 500 BC, 70 BC and AD 450. The stable carbon isotope record reflects changes in biological activity being a result of both climate and human activities. (c) 2014 University of Washington. | |
| 650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskapx Naturgeografi0 (SwePub)105072 hsv//swe |
| 650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Physical Geography0 (SwePub)105072 hsv//eng |
| 653 | a Mediterranean | |
| 653 | a Southern Greece | |
| 653 | a late Holocene | |
| 653 | a Stalagmite | |
| 653 | a Stable isotopes | |
| 653 | a Climate variability | |
| 653 | a Flooding history | |
| 653 | a Hellenistic period | |
| 700 | 1 | a Bar-Matthews, Miryam4 aut |
| 700 | 1 | a Holmgren, Karinu Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)4 aut0 (Swepub:su)kahol |
| 700 | 1 | a Sundqvist, Hanna S.u Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)4 aut0 (Swepub:su)sundq |
| 700 | 1 | a Liakopoulos, Ilias4 aut |
| 700 | 1 | a Zhang, Qiongu Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)4 aut0 (Swepub:su)qzhan |
| 710 | 2 | a Stockholms universitetb Institutionen för naturgeografi och kvartärgeologi (INK)4 org |
| 773 | 0 | t Quaternary Researchd : Cambridge University Press (CUP)g 81:2, s. 213-227q 81:2<213-227x 0033-5894x 1096-0287 |
| 856 | 4 8 | u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-103998 |
| 856 | 4 8 | u https://doi.org/10.1016/j.yqres.2013.12.009 |
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