Pregled bibliografske jedinice broj: 1085904
A 180 ka record of environmental change at Erdut (Croatia): a new chronology for the loess-palaeosol sequence and its implications for environmental interpretation.
A 180 ka record of environmental change at Erdut (Croatia): a new chronology for the loess-palaeosol sequence and its implications for environmental interpretation. // Journal of quaternary science, 35 (4) (2020), 582-593 doi:10.1002/jqs.3201 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 1085904 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
A 180 ka record of environmental change at
Erdut (Croatia): a new chronology for the
loess-palaeosol sequence and its implications
for environmental interpretation.
Autori
Fenn, Kaja ; Durcan, Julie ; Thomas, S.G.David ; Banak, Adriano
Izvornik
Journal of quaternary science (0267-8179) 35 (4)
(2020);
582-593
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
luminescence dating, MARs, MIS 6, pIRIR, Quaternary
Sažetak
While there are numerous thick loess–palaeosol sequences preserved across the Carpathian Basin, well dated sites that provide terrestrial palaeoenvironmental records extending beyond last glacial–interglacial cycle are scarce. Robust chronologies are essential for correlations of loess with other long‐term Quaternary records and to further understanding ofthe palaeoenvironment and climate of this important region beyond the last 125 ka. Here a new geochronology based on 13post‐infrared infrared stimulated luminescence ages focused on the lower part of the loess–palaeosol sequence at Erdut is presented. The results show that the lower part of the Erdut profile spans the penultimate glacial cycle (MIS 7 to MIS 5). The considerable sediments overlaying the investigated part of the profile suggest that this section spans two glacial cycles, rather than the previously suggested one. The most likely source of the discrepancy is the use of uncorrected infrared stimulated luminescence signal, which can cause age underestimation if not accounted for. This study demonstrates the need to revisit sites such as Erdut, re‐date them using updated measurement protocols, and update existing palaeoenvironmental interpretations.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus