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- W2143295587 abstract "Loess‐paleosol sequences are important terrestrial archives of palaeoenvironmental change. Such sequences are rich in pedogenic carbonate, the oxygen and carbon isotopic values of which can provide important palaeoenvironmental information. Although some studies have pioneered the use of O and C isotopes in loess‐paleosol sequences, they are not routinely used as palaeoclimate proxies. In this study we analysed the sedimentology, micromorphology, geochronology and isotopic geochemistry of a M iddle P leistocene loess‐paleosol section, located at K ärlich, G ermany. The section studied correlates with the E lsterian glacial ( MIS 12) and H olsteinian interglacial ( MIS 11). Embedded tephra layers yielded 40 A r/ 39 A r ages of 466±3 ka, 447±1 ka and 361±3 ka. The sedimentology and micromorphology of the sequence record a shift from accretionary loess accumulation ( MIS 12) to prolonged pedogenesis at a stable land surface ( MIS 11). Soil carbonate δ 18 O values record an enrichment of ∼3‰ during the accumulation of the loess, reaching peak values comparable with those found in the MIS 11 soil. The δ 18 O signal is interpreted as reflecting temperature, highlighting the potential of δ 18 O analysis of E uropean loess soil carbonates as a means of reconstructing palaeotemperature history." @default.
- W2143295587 created "2016-06-24" @default.
- W2143295587 creator A5000536303 @default.
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- W2143295587 creator A5066961999 @default.
- W2143295587 date "2014-02-13" @default.
- W2143295587 modified "2023-10-03" @default.
- W2143295587 title "Stable isotopic evidence for Middle Pleistocene environmental change from a loess-paleosol sequence: Kärlich, Germany" @default.
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- W2143295587 doi "https://doi.org/10.1111/bor.12065" @default.
- W2143295587 hasPublicationYear "2014" @default.
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