Towards a comparison of interglacial climate variability in the tropics during the last 300.000 years
- 1Institute of Earth Sciences, Ruprecht-Karls-University Heidelberg, Im Neuenheimer Feld 234, 69120 Heidelberg, Germany (amielke@iup.uni-heidelberg.de)
- 2Institute of Environmental Physics, Ruprecht-Karls-University Heidelberg, Im Neuenheimer Feld 229, 69120 Heidelberg, Germany
- 3Scripps Institution of Oceanography, University of California, San Diego, USA
- 4Anthropology Department, University of California, San Diego, USA
- 5Department of Physics & Chemistry, University of Puerto Rico, Arecibo, USA
- 6Earth and Environmental Systems Department, Indiana State University, Terre Haute, USA
To better estimate effects of current climate change on the water cycle in the highly variable tropical region, past periods of similarly warm climate conditions can provide unique insights. The interglacial phases of the past 800,000 years are promising targets for this purpose, since these provide a natural variety of different climate configurations. While several reconstructions of past interglacial periods are available, the terrestrial, and in particular tropical regions are still under-represented in the record. Speleothems can be used to observe changes and effects on the eco- and climate system as well as their coupling on seasonal to millennial time scales, which usually cannot be resolved by climate model simulations.
This project aims to further close the research gap of these regions with investigations of stalagmites from Cueva Larga, Puerto Rico. Cueva Larga is a well-monitored location1,2,, and speleothem records from this cave have demonstrated a high sensitivity to regional and global climatic variations, in particular changes in the position of the ITCZ, Atlantic sea surface temperatures and ocean circulation3,4. First precise 230Th/U ages on previously collected stalagmites show the potential to reconstruct climatic variations during parts of the past interglacials of the past 300,000 years, i.e., MIS1, MIS, 5, MIS7, and MIS9. In the next step, time series from high-resolution trace element and stable isotope measurements (δ18O and δ13C) from these interglacials will be conducted.
The multi-proxy speleothem time series will allow to improve the quantitative and qualitative understanding of precipitation intensity and variability during interglacials and also help to constrain both the sensitivity of the Earth system in the tropics to different climatic drivers and the extent of current climate change compared to natural variability.
References:
1 Vieten et al. (2017). Monitoring of Cueva Larga, Puerto Rico—A First Step to Decode Speleothem Climate Records. Advances in Karst Science, Springer International Publishing, p.319-331
2 Vieten et al. (2018). Hurricane Impact on Seepage Water in Larga Cave, Puerto Rico. Journal of Geophysical Research: Biogeosciences, Vol. 123, No. 3
3 Warken et al. (2020). Persistent Link Between Caribbean Precipitation and Atlantic Ocean Circulation During the Last Glacial Revealed by a Speleothem Record from Puerto Rico. Paleoceanography and Paleoclimatology, Vol. 35, No. 11
4 Warken et al. (2022). Last glacial millennial-scale hydro-climate and temperature changes in Puerto Rico constrained by speleothem fluid inclusion δ18O and δ2H values. Climate of the Past, Vol. 18, No. 1
How to cite: Mielke, A., Warken, S., Garcia, N., Charles, C., Keppler, F., Rivera Collazo, I., Acosta Colon, A., and Winter, A.: Towards a comparison of interglacial climate variability in the tropics during the last 300.000 years, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-20041, https://doi.org/10.5194/egusphere-egu24-20041, 2024.
