Fluvial terrace formation in mountainous areas: (1) Influence of climate changes during the last glacial cycle in Albania
This work analyses terraces formation from the case of Albanian rivers. An allostratigraphy study of the fluvial terraces is combined with new numerical dating. 30 $\mbox {}^{14}$C and 4 $\mbox {}^{10}$Be new dated sites along four rivers and 45 ages previously acquired along three other rivers were...
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Académie des sciences
2024-01-01
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Series: | Comptes Rendus. Géoscience |
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Online Access: | https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.251/ |
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author | Guzmán, Oswaldo Mugnier, Jean-Louis Vassallo, Riccardo Koçi, Rexhep Carcaillet, Julien Jouanne, François |
author_facet | Guzmán, Oswaldo Mugnier, Jean-Louis Vassallo, Riccardo Koçi, Rexhep Carcaillet, Julien Jouanne, François |
author_sort | Guzmán, Oswaldo |
collection | DOAJ |
description | This work analyses terraces formation from the case of Albanian rivers. An allostratigraphy study of the fluvial terraces is combined with new numerical dating. 30 $\mbox {}^{14}$C and 4 $\mbox {}^{10}$Be new dated sites along four rivers and 45 ages previously acquired along three other rivers were used to define terrace chronologies at the scale of the whole Albania. Few terrace remnants are related to stages older than the last glacial period and are older than $194\pm 19$ ka. Terrace level (T1) includes plain-like terraces and T1 is related to a rapid succession of valley incision and valley fill that occurred during the warm Holocene climatic optimum. The other nine terrace levels (T2 to T10) formed during the last glacial period (MIS 5d to end of MIS 2). Terraces T2, T6 and T7 formed nearly synchronously with interstadial transitions toward warmer and wetter conditions. The formation of terraces T3, T4, T5 and T8 (${<}$60 ka) coincide with the warm climatic excursions of the Heinrich events. This result suggests that these short climatic events strongly punctuate the geomorphologic dynamics of rivers in mountainous areas. |
format | Article |
id | doaj-art-cb3b3259850547058bfad50aa330f689 |
institution | Kabale University |
issn | 1778-7025 |
language | English |
publishDate | 2024-01-01 |
publisher | Académie des sciences |
record_format | Article |
series | Comptes Rendus. Géoscience |
spelling | doaj-art-cb3b3259850547058bfad50aa330f6892025-02-07T10:40:43ZengAcadémie des sciencesComptes Rendus. Géoscience1778-70252024-01-01355G233135310.5802/crgeos.25110.5802/crgeos.251Fluvial terrace formation in mountainous areas: (1) Influence of climate changes during the last glacial cycle in AlbaniaGuzmán, Oswaldo0Mugnier, Jean-Louis1https://orcid.org/0000-0002-3403-7747Vassallo, Riccardo2https://orcid.org/0000-0003-2785-8835Koçi, Rexhep3https://orcid.org/0000-0002-8766-543XCarcaillet, Julien4https://orcid.org/0000-0001-5909-0184Jouanne, François5https://orcid.org/0000-0001-9374-7880Grupo de Investigación en Ciencias de La Tierra y Clima, Universidad Regional Amazónica Ikiam, Muyuna, Ecuador; ISTerre, Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, IRD, Le Bourget du Lac, FranceISTerre, Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, IRD, Le Bourget du Lac, FranceISTerre, Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, IRD, Le Bourget du Lac, FranceInstitute of Geosciences of the Polytechnical University of Tirana, AlbaniaISTerre, Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, IRD, Le Bourget du Lac, FranceISTerre, Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, IRD, Le Bourget du Lac, FranceThis work analyses terraces formation from the case of Albanian rivers. An allostratigraphy study of the fluvial terraces is combined with new numerical dating. 30 $\mbox {}^{14}$C and 4 $\mbox {}^{10}$Be new dated sites along four rivers and 45 ages previously acquired along three other rivers were used to define terrace chronologies at the scale of the whole Albania. Few terrace remnants are related to stages older than the last glacial period and are older than $194\pm 19$ ka. Terrace level (T1) includes plain-like terraces and T1 is related to a rapid succession of valley incision and valley fill that occurred during the warm Holocene climatic optimum. The other nine terrace levels (T2 to T10) formed during the last glacial period (MIS 5d to end of MIS 2). Terraces T2, T6 and T7 formed nearly synchronously with interstadial transitions toward warmer and wetter conditions. The formation of terraces T3, T4, T5 and T8 (${<}$60 ka) coincide with the warm climatic excursions of the Heinrich events. This result suggests that these short climatic events strongly punctuate the geomorphologic dynamics of rivers in mountainous areas.https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.251/Fluvial sedimentationClimatic and vegetation controlsRiver piracyLate glacial cycleInterstadials<i>In situ</i> produced $\mbox {}^{10}$Be dating$\mbox {}^{14}$C dating |
spellingShingle | Guzmán, Oswaldo Mugnier, Jean-Louis Vassallo, Riccardo Koçi, Rexhep Carcaillet, Julien Jouanne, François Fluvial terrace formation in mountainous areas: (1) Influence of climate changes during the last glacial cycle in Albania Comptes Rendus. Géoscience Fluvial sedimentation Climatic and vegetation controls River piracy Late glacial cycle Interstadials <i>In situ</i> produced $\mbox {}^{10}$Be dating $\mbox {}^{14}$C dating |
title | Fluvial terrace formation in mountainous areas: (1) Influence of climate changes during the last glacial cycle in Albania |
title_full | Fluvial terrace formation in mountainous areas: (1) Influence of climate changes during the last glacial cycle in Albania |
title_fullStr | Fluvial terrace formation in mountainous areas: (1) Influence of climate changes during the last glacial cycle in Albania |
title_full_unstemmed | Fluvial terrace formation in mountainous areas: (1) Influence of climate changes during the last glacial cycle in Albania |
title_short | Fluvial terrace formation in mountainous areas: (1) Influence of climate changes during the last glacial cycle in Albania |
title_sort | fluvial terrace formation in mountainous areas 1 influence of climate changes during the last glacial cycle in albania |
topic | Fluvial sedimentation Climatic and vegetation controls River piracy Late glacial cycle Interstadials <i>In situ</i> produced $\mbox {}^{10}$Be dating $\mbox {}^{14}$C dating |
url | https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.251/ |
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