TY - JOUR A1 - Lenz, Josefine A1 - Grosse, Guido A1 - Jones, Benjamin M. A1 - Anthony, Katey M. Walter A1 - Bobrov, Anatoly A1 - Wulf, Sabine A1 - Wetterich, Sebastian T1 - Mid-Wisconsin to Holocene Permafrost and Landscape Dynamics based on a Drained Lake Basin Core from the Northern Seward Peninsula, Northwest Alaska JF - Permafrost and Periglacial Processes N2 - Permafrost-related processes drive regional landscape dynamics in the Arctic terrestrial system. A better understanding of past periods indicative of permafrost degradation and aggradation is important for predicting the future response of Arctic landscapes to climate change. Here, we used a multi-proxy approach to analyse a4m long sediment core from a drained thermokarst lake basin on the northern Seward Peninsula in western Arctic Alaska (USA). Sedimentological, biogeochemical, geochronological, micropalaeontological (ostracoda, testate amoebae) and tephra analyses were used to determine the long-term environmental Early-Wisconsin to Holocene history preserved in our core for central Beringia. Yedoma accumulation dominated throughout the Early to Late-Wisconsin but was interrupted by wetland formation from 44.5 to 41.5ka BP. The latter was terminated by the deposition of 1m of volcanic tephra, most likely originating from the South Killeak Maar eruption at about 42ka BP. Yedoma deposition continued until 22.5ka BP and was followed by a depositional hiatus in the sediment core between 22.5 and 0.23ka BP. We interpret this hiatus as due to intense thermokarst activity in the areas surrounding the site, which served as a sediment source during the Late-Wisconsin to Holocene climate transition. The lake forming the modern basin on the upland initiated around 0.23ka BP and drained catastrophically in spring 2005. The present study emphasises that Arctic lake systems and periglacial landscapes are highly dynamic and that permafrost formation as well as degradation in central Beringia was controlled by regional to global climate patterns as well as by local disturbances. Copyright (c) 2015 John Wiley & Sons, Ltd. KW - Beringia KW - palaeoenvironmental reconstruction KW - thermokarst lake dynamics KW - cryostratigraphy KW - tephra KW - bioindicators KW - yedoma Y1 - 2016 U6 - https://doi.org/10.1002/ppp.1848 SN - 1045-6740 SN - 1099-1530 VL - 27 SP - 56 EP - 75 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Martin-Puertas, Celia A1 - Lauterbach, Stefan A1 - Allen, Judy R. M. A1 - Perez, Marta A1 - Blockley, Simon A1 - Wulf, Sabine A1 - Huntley, Brian A1 - Brauer, Achim T1 - Initial Mediterranean response to major climate reorganization during the last interglacial-glacial transition JF - Quaternary science reviews : the international multidisciplinary research and review journal N2 - Millennial-scale Dansgaard Oeschger (DO) variability at northern high latitudes has influenced climatic and environmental conditions in the Mediterranean during the last glacial period. There is evidence that the hemispheric transmission of the DO variability occurred at the end of DO event 25; however, the exact timing and the trigger that activated the environmental response in the Mediterranean remains incompletely understood. Here, we provide evidence that the clear millennial-scale teleconnection between Greenland and the Mediterranean started at similar to 111.4 ka BP and was initiated by a sub-millennial scale cooling in Greenland (GI-25b). High-resolution sediment proxies and the pollen record of Lago Grande di Monticchio (MON), Italy, reflect climatic instability during the last millennium of the last interglacial, which was characterised by a first and short cooling episode (MON 1) at 111.44 +/- 0.69 ka BP, coinciding with the Greenland cold sub-event GI-25b in duration and timing (within dating uncertainties). MON and Greenland (NorthGRIP ice core) also agree in recording a subsequent warm rebound phase that abruptly culminated in the stadial MON 2/GS-25, marking the transition into the last glacial period. Our results show that the GI-25b triggered an early environmental response at MON to centennial-scale climate change in Greenland as a prelude to the millennial-scale teleconnection that was maintained during the glacial period. KW - Palaeoclimatology KW - Last interglacial-glacial transition KW - Millennial-scale variability KW - Mediterranean KW - Varved sediments Y1 - 2019 U6 - https://doi.org/10.1016/j.quascirev.2019.05.019 SN - 0277-3791 VL - 215 SP - 232 EP - 241 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Neugebauer, Ina A1 - Brauer, Achim A1 - Draeger, Nadine A1 - Dulski, Peter A1 - Wulf, Sabine A1 - Plessen, Birgit A1 - Mingram, Jens A1 - Herzschuh, Ulrike A1 - Brande, Arthur T1 - A Younger Dryas varve chronology from the Rehwiese palaeolake record in NE-Germany JF - Quaternary science reviews : the international multidisciplinary research and review journal N2 - The first 1400-year floating varve chronology for north-eastern Germany covering the late Allered to the early Holocene has been established by microscopic varve counts from the Rehwiese palaeolake sediment record. The Laacher See Tephra (LST), at the base of the studied interval, forms the tephrochronological anchor point. The fine laminations were examined using a combination of micro-facies and mu XRF analyses and are typical of calcite varves, which in this case provide mainly a warm season signal. Two varve types with different sub-layer structures have been distinguished: (I) complex varves consisting of up to four seasonal sub-layers formed during the Allered and early Holocene periods, and, (II) simple two sub-layer type varves only occurring during the Younger Dryas. The precision of the chronology has been improved by varve-to-varve comparison of two independently analyzed sediment profiles based on well-defined micro-marker layers. This has enabled both (1) the precise location of single missing varies in one of the sediment profiles, and, (2) the verification of varve interpolation in disturbed varve intervals in the parallel core. Inter-annual and decadal-scale variability in sediment deposition processes were traced by multi-proxy data series including seasonal layer thickness, high-resolution element scans and total organic and inorganic carbon data at a five-varve resolution. These data support the idea of a two-phase Younger Dryas, with the first interval (12,675-12,275 varve years BP) characterised by a still significant but gradually decreasing warm-season calcite precipitation and a second phase (12,275-11,690 varve years BP) with only weak calcite precipitation. Detailed correlation of these two phases with the Meerfelder Maar record based on the LST isochrone and independent varve counts provides clues about regional differences and seasonal aspects of YD climate change along a transect from a location proximal to the North Atlantic in the west to a more continental site in the east KW - Varve chronology KW - Micro-fades KW - Micro-XRF KW - Younger Dryas KW - North-eastern Germany Y1 - 2012 U6 - https://doi.org/10.1016/j.quascirev.2011.12.010 SN - 0277-3791 VL - 36 IS - 10 SP - 91 EP - 102 PB - Elsevier CY - Oxford ER - TY - THES A1 - Wulf, Sabine T1 - Methods and applications of tephrochronology in sedimentary archives Y1 - 2012 CY - Potsdam ER - TY - THES A1 - Wulf, Sabine T1 - Das tephrochronologische Referenzprofil des Lago Grande di Monticchio : eine detallierte Stratigraphie des süditalienischen explosiven Vulkanismus der letzten 100.000 Jahre Y1 - 2000 UR - http://www.gfz-potsdam.de/bib/pub/str0103/0103.pdf UR - https://nbn-resolving.org/urn:nbn:de:kobv:b103-010113 ER -