The age of the Hengelo interstadial revisited

Vandenberghe, Jef; Plicht, Johannes van der

doi:10.1016/j.quageo.2015.12.004

Cited by 19 publications

(13 citation statements)

References 50 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…Layer 6 was dated to approximately 41-37 cal kyr BP, chronologically corresponding with GIS 8. The development of the soil sediments is consistent with Denekamp Interstadial (Vandenberghe and van der Plicht, 2016) and soils marked as PK1 (Kukla, 1969). The Interstadial "Pod hradem" was also placed in this timespan, however this regional and outdated term should now be abandoned (Lisa et al, 2018).…”

Section: Accepted Manuscriptsupporting

confidence: 67%

See 1 more Smart Citation

Cave deposits as a sedimentary trap for the Marine Isotope Stage 3 environmental record: The case study of Pod Hradem, Czech Republic

Nejman

Lisá

Doláková

et al. 2018

Palaeogeography, Palaeoclimatology, Palaeoecology

View full text Add to dashboard Cite

Section: Accepted Manuscriptsupporting

confidence: 67%

“…It is likely that Europe comprised a mosaic of different environments during this period. The relevance and validity of former local stratigraphic schemes also needs to be taken into account (Lisa et al, 2018;Vandenberghe and van der Plicht, 2016).…”

Section: A C C E P T E Dmentioning

confidence: 99%

Cave deposits as a sedimentary trap for the Marine Isotope Stage 3 environmental record: The case study of Pod Hradem, Czech Republic

Nejman

Lisá

Doláková

et al. 2018

Palaeogeography, Palaeoclimatology, Palaeoecology

View full text Add to dashboard Cite

“…The only two exceptions are related to low sedimentation rates during the Middle Pleniglacial. The tundra gley Gm3, which is twice the thickness of Gm2 and Gm1, most likely stacks two successive tundra gleys formed during GI 11 and GI 10 (i.e., during the Hengelo interstadial) (36,37). Similarly, the Lohne Soil appears likely as a stack of two soil horizons developed during GI 8 and GI 7c (i.e., during the initial phase of the Denekamp interstadial complex) (36).…”

Section: Discussionmentioning

confidence: 99%

The impact of Last Glacial climate variability in west-European loess revealed by radiocarbon dating of fossil earthworm granules

Moine

Antoine

Hatté

et al. 2017

Proc. Natl. Acad. Sci. U.S.A.

102

103

View full text Add to dashboard Cite

The characterization of Last Glacial millennial-timescale warming phases, known as interstadials or Dansgaard-Oeschger events, requires precise chronologies for the study of paleoclimate records. On the European continent, such chronologies are only available for several Last Glacial pollen and rare speleothem archives principally located in the Mediterranean domain. Farther north, in continental lowlands, numerous high-resolution records of loess and paleosols sequences show a consistent environmental response to stadial-interstadial cycles. However, the limited precision and accuracy of luminescence dating methods commonly used in loess deposits preclude exact correlations of paleosol horizons with Greenland interstadials. To overcome this problem, a radiocarbon dating protocol has been developed to date earthworm calcite granules from the reference loess sequence of Nussloch (Germany). Its application yields a consistent radiocarbon chronology of all soil horizons formed between 47 and 20 ka and unambiguously shows the correlation of every Greenland interstadial identified in isotope records with specific soil horizons. Furthermore, eight additional minor soil horizons dated between 27.5 and 21 ka only correlate with minor decreases in Greenland dust records. This dating strategy reveals the high sensitivity of loess paleoenvironments to Northern Hemisphere climate changes. A connection between loess sedimentation rate, Fennoscandian ice sheet dynamics, and sea level changes is proposed. The chronological improvements enabled by the radiocarbon "earthworm clock" thus strongly enhance our understanding of loess records to a better perception of the impact of Last Glacial climate changes on European paleoenvironments

show abstract

“…The Gorzów Wielkopolski stratigraphic sequence was the result of a virtually uninterrupted accumulation of siliciclastic and organic sediments from the decline of the Saalian glaciation (MIS 6), through the Eemian Interglacial (MIS 5e) to the Hengelo and Denekamp Interstadials (MIS 3). Sites with similar periods are Hengelo and Moershoofd, in the eastern Netherlands, and Oerel, in Germany (Behre and Lade, 1986; Vandenberghe and Plicht, 2016). Remains of S. kirchbergensis had been found at 10 other Polish sites, but most are of unknown age.…”

Section: Discussionmentioning

confidence: 96%

Geology, stratigraphy and palaeoenvironmental evolution of the Stephanorhinus kirchbergensis‐bearing Quaternary palaeolake(s) of Gorzów Wielkopolski (NW Poland, Central Europe)

Sobczyk

Borówka

Badura

et al. 2020

J Quaternary Science

View full text Add to dashboard Cite

The sedimentary succession exposed in the Gorzów Wielkopolski area includes Eemian Interglacial (MIS 5e) or Early Weichselian (MIS 5d-e) deposits. The sedimentary sequence has been the object of intense interdisciplinary study, which has resulted in the identification of at least two palaeolake horizons. Both yielded fossil remains of large mammals, alongside pollen and plant macrofossils. All these proxies have been used to reconstruct the environmental conditions prevailing at the time of deposition, as well as to define the geological context and the biochronological position of the fauna. Optically stimulated luminescence dating of the glaciofluvial layers of the GS3 succession to 123.6 ± 10.1 (below the lower palaeolake) and 72.0 ± 5.2 ka (above the upper palaeolake) indicate that the site formed during the Middle-Late Pleistocene (MIS 6 -MIS 5). Radiocarbon-dating of the lacustrine organic matter revealed a tight cluster of Middle Pleniglacial Period (MIS 3) ages in the range of~41-32 ka cal BP (Hengelo -Denekamp Interstadials). Holocene organic layers have also been found, with 14 C ages within a range of 4330-4280 cal BP (Neolithic). Pollen and plant macrofossil records, together with sedimentological and geochemical data, confirm the dating to the Eemian Interglacial.

show abstract

The age of the Hengelo interstadial revisited

Cited by 19 publications

References 50 publications

Cave deposits as a sedimentary trap for the Marine Isotope Stage 3 environmental record: The case study of Pod Hradem, Czech Republic

Cave deposits as a sedimentary trap for the Marine Isotope Stage 3 environmental record: The case study of Pod Hradem, Czech Republic

The impact of Last Glacial climate variability in west-European loess revealed by radiocarbon dating of fossil earthworm granules

Geology, stratigraphy and palaeoenvironmental evolution of the Stephanorhinus kirchbergensis‐bearing Quaternary palaeolake(s) of Gorzów Wielkopolski (NW Poland, Central Europe)

Contact Info

Product

Resources

About