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Data Publication

Depth versus age based on relative magnetic paleointensity correlations for all six investigated sites

Demory, Francois | Nowaczyk, Norbert | Witt, Annette | Oberhänsli, Hedi

Deutsches GeoForschungsZentrum GFZ

(2006)

Descriptions

In order to characterise Lake Baikal sedimentary responses to global climatic changes that may be recorded in marine sediments, we compared our paleomagnetically dated climate-proxy record from Lake Baikal with benthic and plankontic δ18O curves of ODP Site 983, a site close to ODP Site 984. The neighbouring site was chosen for comparison because although the quality of the ODP Site 984 paleomagnetic record is high, its δ18O records are of lower quality than those of ODP Site 983. Synchronous paleomagnetic variations observed in ODP Sites 983 and 984 sediments (Fig. 10) show that the premise of our age model based on paleomagnetic correlation is identical, if the reference curve used for correlation is from ODP Site 983. We can, therefore, compare climatic records from ODP site 983 and Lake Baikal. The climatic proxy used for Lake Baikal sediment is the HIRM record since it displays the detrital input variations (Peck et al., 1994).

Keywords


Originally assigned keywords
Vereshchagin 98 Expedition
Vereshchagin Long Cores Expedition 2001
R/V Vereshchagin
age (calendar years)
calculation

MSL enriched keywords
Measured property
paleointensity
Inferred behavior
natural remanent magnetisation processing
relative paleointensity

MSL enriched sub domains i

paleomagnetism


Source publisher

Deutsches GeoForschungsZentrum GFZ


DOI

10.1594/gfz.sddb.1014


Creators

Demory, Francois

Nowaczyk, Norbert

Witt, Annette

Oberhänsli, Hedi


Citation

Demory, F., Nowaczyk, N., Witt, A., & Oberhänsli, H. (2006). Depth versus age based on relative magnetic paleointensity correlations for all six investigated sites [Data set]. Deutsches GeoForschungsZentrum GFZ. https://doi.org/10.1594/GFZ.SDDB.1014


Dates

Issued:

2006-09-13


Language

en