Deglaciation chronology and post-glacial environmental evolution of the Upper Garonne valley (Central Pyrenees)

• Main Author: Fernandes, Marcelo
• Publication Date: 2023
• Language: eng
• Source: Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
• Download full: http://hdl.handle.net/10451/58284
• topic: Geomorfologia; Quaternário Superior; Deglaciação; datações por isótopos cosmogénicos; alto Vale do rio Garona; Geomorphology; Late Quaternary; Deglaciation; Cosmic-ray exposure dating; Upper Garonne; Domínio/Área Científica::Ciências Sociais::Geografia Económica e Social

This PhD dissertation focuses on the Upper Garonne basin, Central Pyrenees. The study area ranges from the highest peaks at >2800-3000 m to the lowest moraine deposits located in the Loures Barousse Barbazan basin (LBBB) at 400-500 m. This catchment hosted the largest Quaternary glacier in the Pyrenees, although little was known about its glacial chronology. An accurate geomorphological analysis and mapping of the distribution of glacial and periglacial phenomena in the study area revealed the existence of a wide variety of landforms indicative of the occurrence of several periods of intense glacial and periglacial activity. The moraine distribution indicates that glaciers formed three moraine complexes at (1) moraines at the glacial terminal basin (420-820 m), (2) moraines at the mountain slopes and high valleys (1000-2100 m) and moraines at the glacial cirques (>2100 m). In the foreland of the Pyrenees, we find the LBBB, which includes the lowest moraine system of the Upper Garonne basin at 80 km from the headwaters of the catchment. Here, the external moraine (ca. 420 m) was dated by means of cosmic-ray exposure (CRE) and yielded an age of 128.5 ± 9.1 ka. This age constitutes the most solid chronological record of glacier advance in the Pyrenees during the Last Glacial Cycle and suggests that the past Equilibrium Line Altitude (palaeoELA) at that time was set at 1705 m and summer temperatures were ca. 9.3 ºC lower than the current values. The Garonne palaeoglacier must have also reached the LBBB during the Last Glacial Cycle (LGC), as confirmed by lake sediments from the Barbazan lake, although CRE results from boulders in the internal moraine system reported very scattered ages (73.1 ± 4.6 to 17.1 ± 1.8 ka). Such a large extension of the Garonne palaeoglacier during the global Last Glacial Maximum (GLGM) is also suggested by two CRE ages from the polished surfaces near the Marignac basin (7 km south of the LBBB). These ages of 24.2 ± 2.1 and 20.7 ± 1.2 ka indicate that this palaeoglacier was retreating during the GLGM while in Northern Europe, glaciers were still growing or at their maximum. The long-term recession was interrupted by brief periods of glacier expansion. No evidence has been dated yet of a glacial advance during the Oldest Dryas in this valley. Warm temperatures prevailing during the first half of the Bølling-Allerød (B-A) favoured a massive glacial retreat, with glaciers mostly disappearing from the highest catchments from 16.0 ± 1.0 to 13.5 ± 0.8 ka. During the late B-A and early Younger Dryas (YD), short episodes of lower temperatures and higher precipitation promoted glacial expansion and moraine formation, with 4.5 to 0.5-km-long glaciers advancing towards the high valley bottoms by 13.5 ± 0.9, 13.2 ± 1.1 and 13.0 ± 0.8 ka. These moraines are indicative of palaeoELAs up to 2461-2505 m and summer palaeotemperatures of 4.2-3.9 ºC lower than present-day. During the cold YD, small glaciers developed in the highest northern and western cirques by 12.8 ± 0.5 and 12.6 ± 1.3 ka. However, the increasing aridity during this stadial promoted their disappearance from larger cirques below 2800 m by 12.8 ± 0.8 and 12.7 ± 0.8 ka. During this short event, palaeoELAs were located at 2504-2571 m and summer palaeotemperatures of 3.4-3ºC lower than today. The deglaciation of the cirques and mountain slopes favoured paraglacial adjustment, triggering widespread slope failures and generating rock glaciers. In the Upper Garonne basin, paraglacial dynamics were largely controlled by lithology, as shown by the occurrence of large rock failures in the slates and lutites with limestones and rock glaciers in granitoids. The application of the CRE dating in rock glaciers showed that the glacial to periglacial transition was underway by 13.6 ± 0.9 ka, when rock glaciers started developing. These features stabilised soon after their formation and became relict by 11.9 ± 0.7 ka. During the cold phases of the Holocene, glaciers could have formed within sheltered areas in the highest cirques of the Central Pyrenees forming moraines above 2500 m, although no evidence has been found yet in the study area.