RT Journal Article
T1 Timing of formation of neoglacial landforms in the South Shetland Islands (Antarctic Peninsula): Regional and global implications
A1 Palacios Estremera, David
A1 Ruiz-Fernández, Jesus
A1 Oliva, Marc
A1 De Andrés de Pablo, Nuria
A1 Fernández Fernández, José María
A1 Schimmelpfennig, Irene
A1 Leanni, Laëtitia
A1 González-Díaz, Benjamín
A1 Team, ASTER
AB The timing of neoglacial advances in the Antarctic Peninsula (AP) is not yet well constrained. Accurate temporal reconstruction of Neoglaciation in the AP is needed to better understand past glacial responses and regional and global teleconnections during the Holocene. Here, we examine all available information about neoglacial advances in the South Shetland Islands (SSI) as well as in the broader geographical context of the AP region and Antarctic continent. In order to shed light on the contrasting chronologies existing for neoglacial advances in these regions, we focused on a case study where a detailed picture of the Holocene deglaciation was already available. Lake sediments revealed that Byers Peninsula, west of Livingston Island (SSI), was fully deglaciated during the Holocene Thermal Maximum. To complement this approach, we identified glacially polished bedrock surfaces, erratic boulders and a moraine ridge near the present front of the glacier in the SE corner. We applied cosmogenic ray exposure (CRE) dating using in situ 36Cl for basalt rocks and 10Be for granitic rocks in: (i) 8 samples from glacial erratic and ice-rafted boulders, (ii) 2 samples from moraine boulders, (iii) 2 samples from polished bedrock surfaces, and (iv) 1 sample from an erratic boulder deposited on one of these surfaces. The CRE dates indicate that the onset of deglaciation started around 9.9 ± 1.2 ka, with two phases of glacier expansion during the Mid-Late Holocene forming moraines at ∼4.1 ± 0.5 and ∼1.0 ± 0.2 ka, respectively. The main neoglacial advances in the AP and the SSI were mostly synchronous and coincided with cold periods, as shown by other records (e.g. glacio-isostatic marine terraces, marine and lake sediments). In addition, these periods of glacial expansion show a similar timing to those recorded in the Arctic. These results suggest that Neoglaciation was driven by global climate forcing in both polar areas despite temporal variations at regional and local scale.
PB Elsevier
SN 0277-3791
YR 2020
FD 2020
LK https://hdl.handle.net/20.500.14352/113372
UL https://hdl.handle.net/20.500.14352/113372
LA eng
NO Palacios D, Ruiz-Fernández J, Oliva M, Andrés N, Fernández-Fernández JM, Schimmelpfennig I, et al. Timing of formation of neoglacial landforms in the South Shetland Islands (Antarctic Peninsula): Regional and global implications. Quaternary Science Reviews. 2020 Apr;234:106248.
NO Ministerio de Economía y Competitivdad (España)
NO Fundação para a Ciência e a Tecnologia (Portugal)
NO Programa Ramón y Cajal (España)
DS Docta Complutense
RD 27 abr 2025