Projects per year
Abstract
Speleothem Delta 18 O and Delta 13 C signals have already proven to enable climate reconstructions at high resolution. However, seasonally resolved speleothem records are still scarce and often difficult to interpret in terms of climate due to the multitude of factors that can affect the proxy signals. In this paper, a fast growing (up to 2 mm yr? 1) seasonally laminated speleothem from the Han-sur-Lesse cave (Belgium) is analyzed for its delta 18 O andDelta 13 C values, layer thickness and changes in calcite fabric.
Original language | English |
---|---|
Pages (from-to) | 4149-4190 |
Number of pages | 42 |
Journal | Climate of the Past Discussions |
Volume | 10 |
Issue number | 5 |
Publication status | Published - 2014 |
Keywords
- Holocene climate
- Paleoclimate
- Little Ice Age
Fingerprint
Dive into the research topics of 'A 500 year seasonally resolved δ18 O and δ13C, layer thickness and calcite fabric record from a speleothem deposited in equilibrium of the Han-sur-Lesse cave, Belgium'. Together they form a unique fingerprint.Projects
- 2 Finished
-
SRP2: Strategic Research Programme: Tracing and Modelling of Past & Present Global Changes
Claeys, P., Elskens, M., Huybrechts, P., Gao, Y., Kervyn De Meerendre, M., Claeys, P., Baeyens, W. & Dehairs, F.
1/11/12 → 31/10/24
Project: Fundamental
Research output
- 1 Article
-
Paleoclimate in continental northwestern Europe during the Eemian and Early-Weichselian (125-97 ka): insights from a Belgian speleothem
Vansteenberge, S., Verheyden, S., Cheng, H., Edwards, L. R., Keppens, E. & Claeys, P., 8 Feb 2016, In: Climate of the Past. 2016, p. 1445-1458 14 p.Research output: Contribution to journal › Article › peer-review
Open Access28 Citations (Scopus)