Western Mediterranean climate and environment since Marine Isotope Stage 3: a 50,000-year record from Lake Banyoles, Spain
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- 作者：Jack H. Lacey ; Melanie J. Leng ; Nicole Höbig ; Jane M. Reed…
- 关键词：Karstic lakes ; Palaeoclimate ; Isotopes ; Diatoms ; Iberian Peninsula ; Mediterranean
- 刊名：Journal of Paleolimnology
- 出版年：2016
- 出版时间：February 2016
- 年：2016
- 卷：55
- 期：2
- 页码：113-128
- 全文大小：2,309 KB
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Melanie J. Leng (1) (2)
Nicole Höbig (3)
Jane M. Reed (4)
Blas Valero-Garcés (5)
Klaus Reicherter (3)
1. NERC Isotope Geosciences Facilities, British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK
2. Centre for Environmental Geochemistry, School of Geography, University of Nottingham, Nottingham, NG7 2RD, UK
3. Institute of Neotectonics and Natural Hazards, RWTH Aachen University, Lochnerstraße 4-20, 52056, Aachen, Germany
4. Department of Geography, Environment and Earth Sciences, University of Hull, Hull, HU6 7RX, UK
5. Instituto Pirenaico de Ecología, CSIC, Avda Montañana 1005, Apdo 13034, 50080, Saragossa, Spain - 刊物类别：Earth and Environmental Science
- 刊物主题：Environment
Environment
Sedimentology
Climate Change
Physical Geography
Hydrobiology
Geology - 出版者：Springer Netherlands
- ISSN：1573-0417
文摘
We present new stable isotope (δ18Ocalcite and δ13Ccalcite) and diatom data from a 67-m sediment core (BAN II) from Lake Banyoles, northeastern Spain. We reassessed the chronology of the sequence by correlating stable isotope data with a shorter U-series-dated record from the lake, confirming a sedimentological offset between the two cores and demonstrating that BAN II spans Marine Isotope Stages (MIS) 3–1. Through comparison with previous records, the multi-proxy data are used to improve understanding of palaeolimnological dynamics and, by inference, western Mediterranean climate and environmental change during the past ca. 50,000 years. Three main zones, defined by isotope and diatom data, correspond to the MIS. The basal zone (MIS 3) is characterised by fluctuating δ18Ocalcite and benthic diatom abundance, indicating a high degree of environmental and climate variability, concomitant with large lake-level changes. During the full glacial (MIS 2), relatively constant δ18Ocalcite and a poorly preserved planktonic-dominated diatom assemblage suggest stability, and intermittently, unusually high lake level. In MIS 1, δ18Ocalcite and δ13Ccalcite initially transition to lower values, recording a pattern of Late Glacial to Holocene change that is similar to other Mediterranean records. This study suggests that Lake Banyoles responds limnologically to changes in the North Atlantic ocean–atmosphere system and provides an important dataset from the Iberian Peninsula, a region in need of longer-term records that can be used to correlate between marine and terrestrial archives, and between the western and eastern Mediterranean. Keywords Karstic lakes Palaeoclimate Isotopes Diatoms Iberian Peninsula Mediterranean