Procesos geomorfológicos y formas del relieve en dos cuencas lacustres de la península Byers (isla Livingston, Antártida marítima): implicaciones paleoambientales = Geomorphological processes and landforms in two lake catchments of Byers Peninsula (Livingston Island, Maritime Antarctica): paleoenvironmental implications
En este artículo se estudian las cuencas y áreas circundantes de dos cuerpos lacustres situados en el sector oriental de la Península de Byers (isla Livingston, Antártida), Cerro Negro y Domo, con el objetivo de identificar los procesos geomorfológicos y formas de relieve existentes, así como las ár...
| Published in: | Polígonos. Revista de Geografía |
|---|---|
| Main Authors: | , , |
| Other Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | Spanish |
| Published: |
Universidad de León
2016
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| Subjects: | |
| Online Access: | http://revistas.unileon.es/index.php/poligonos/article/view/4294 https://doi.org/10.18002/pol.v0i28.4294 |
| _version_ | 1821751338741006336 |
|---|---|
| author | Ruiz-Fernández, Jesús Oliva, Marc García-Hernández, Cristina |
| author2 | Proyecto de investigación HOLOANTAR, financiado por la Fundación de Ciencia y Tecnología. Apoyo logístico del Programa Polar Portugués soporte de los programas antárticos de Brasil y Chile. Patrocinio de la AXA Research Fundation. Beca FPU |
| author_facet | Ruiz-Fernández, Jesús Oliva, Marc García-Hernández, Cristina |
| author_sort | Ruiz-Fernández, Jesús |
| collection | Revistas Universidad de León (ule) |
| container_issue | 28 |
| container_start_page | 211 |
| container_title | Polígonos. Revista de Geografía |
| description | En este artículo se estudian las cuencas y áreas circundantes de dos cuerpos lacustres situados en el sector oriental de la Península de Byers (isla Livingston, Antártida), Cerro Negro y Domo, con el objetivo de identificar los procesos geomorfológicos y formas de relieve existentes, así como las áreas fuente de sedimentos para los lagos. Para ello, se presenta una cartografía geomorfológica detallada de ambos sectores. En el área de Cerro Negro han sido diferenciadas cuatro unidades geomorfológicas: cerro, ladera Norte, escarpe meridional, y playas levantadas y playa actual. En el área de Domo se han diferenciado otras cuatro: lago y áreas planas adyacentes, laderas de la cuenca, interfluvios y afloramientos rocosos culminantes, y morrena del glaciar Rotch. Las evidencias geomorfológicas detectadas permiten realizar una reconstrucción paleoambiental en la que se diferencian tres fases: una fase de máxima expansión glaciar en la que solamente algunos nunataks sobresaldrían por encima del hielo; una segunda fase holocena de retroceso glaciar, formación de lagos e intensa dinámica periglaciar; y una tercera en la que se completa la deglaciación y la dinámica periglaciar se generaliza en las nuevas áreas libres de hielo, aunque con menor intensidad que en la fase previa.In this paper, lake catchments and surrounding areas of Cerro Negro and Domo lakes, eastern Byers Peninsula —Livingston Island, Antarctica—, are examined in order to identify both geomorphological processes and landforms, as well as to establish the sediment sources for lacustrine sedimentary processes. To do so, a detailed geomorphological mapping of both areas was carried out. Four geomorphological units were identified in the Cerro Negro area —hill, northern slope, southern scarp, and raised beaches and present-day beach—, as well as in the Domo area — lake and shorelines, slopes, watersheds and rocky outcrops, and moraine of Rotch Dome glacier—. Geomorphological evidences allowed to infer three paleoenvironmental stages: the first, in which only a reduced number of nunataks would protrude above the ice cap; a second stage characterized by glacial retreat during the Holocene, an intense periglacial dynamics and the formation of lakes; and the third one, in which the deglaciation was completed and periglacial activity became generalized, although with less intensity than in the previous phase. |
| format | Article in Journal/Newspaper |
| genre | Antarc* Antarctic and Alpine Research Antarctic Science Antarctica Antártida Arctic Berichte zur Polarforschung British Antarctic Survey Bulletin Ice Ice cap Livingston Island permafrost Permafrost and Periglacial Processes Polar Record Polar Science Polar Science Polarforschung |
| genre_facet | Antarc* Antarctic and Alpine Research Antarctic Science Antarctica Antártida Arctic Berichte zur Polarforschung British Antarctic Survey Bulletin Ice Ice cap Livingston Island permafrost Permafrost and Periglacial Processes Polar Record Polar Science Polar Science Polarforschung |
| geographic | Byers Byers peninsula Cerro Negro Dome Glacier Hielo isla Livingston Livingston Island península Byers Rotch Rotch Dome |
| geographic_facet | Byers Byers peninsula Cerro Negro Dome Glacier Hielo isla Livingston Livingston Island península Byers Rotch Rotch Dome |
| id | ftunivleonojs:oai:http://revpubli.unileon.es/ojs/:article/4294 |
| institution | Open Polar |
| language | Spanish |
| long_lat | ENVELOPE(-60.283,-60.283,-63.900,-63.900) ENVELOPE(-61.066,-61.066,-62.633,-62.633) ENVELOPE(-61.002,-61.002,-62.655,-62.655) ENVELOPE(-94.068,-94.068,79.452,79.452) ENVELOPE(-58.133,-58.133,-62.083,-62.083) ENVELOPE(-60.500,-60.500,-62.600,-62.600) ENVELOPE(-60.500,-60.500,-62.600,-62.600) ENVELOPE(-61.083,-61.083,-62.633,-62.633) ENVELOPE(-60.883,-60.883,-62.633,-62.633) ENVELOPE(-60.883,-60.883,-62.633,-62.633) |
| op_collection_id | ftunivleonojs |
| op_doi | https://doi.org/10.18002/pol.v0i28.4294 https://doi.org/10.18002/pol.v0i28 https://doi.org/10.1016/j.sedgeo.2015.08.002 https://doi.org/10.1016/j.geomorph.2014.03.041 |
| op_relation | http://revistas.unileon.es/index.php/poligonos/article/view/4294/3211 ARAYA, R. y HERVÉ, F. (1966): Estudio geomorfológico y geológico en las Islas Shetland del Sur, Antártida. Publicaciones del Instituto Antártico Chileno, 8, 76. BALCO; G., SCHAEFER, J.M. y LARISSA group (2013): «Exposure-age record of Holocene ice sheet and ice shelf change in the northeast Antarctic Peninsula». Quaternary Science Reviews, 59, 101-111. BAÑÓN, M.; JUSTEL, A.; VELÁZQUEZ, D. y QUESADA, A. (2013): «Regional weather survey on Byers Peninsula, Livingston Island, South Shetland Islands, Antarctica». Antarctic Science, 25, 146-156. BARONI, C.; BRUSCHI, G. y LÓPEZ-MARTÍNEZ, J. (1997): «Review of Antarctic geomorphological mapping». Geografia Fisica e Dinamica Quaternaria, 20, 15-31. BARONI, C. y OROMBELLI, G. (1994): «Holocene glaciar variations in the Terra Nova Bay area (Victoria Land, Antarctica)». Antarctic Science, 6, 497-505. BIASINI, A.; OSSO, P. y SALVATORE, M.C. (1997): «Geomorphological sketch map of the Mount Dickason area (Victoria Land, Antarctica) mapped by aerial photographs». Geografia Fisica e Dinamica Quaternaria, 20, 219-223. BIRKENMAJER, K. (1997): «Map of quaternary geology at Artowsky Station, King George Island, South Shetland Island (West Antarctica) 1/25000». Studia Geológica Polonica, 110. BENTLEY, M.J.; HODGSON, D.; SMITH, J.; O COFAIGH, C.; DOMACK, E.; LARTEER, R.; ROBERTS, S.; BRACHFELD, S.; LEVENTER, A.; HJORT, C.; HILLENBRAND, C. y EVANS, J. (2009): «Mechanisms of Holocene paleoenvironmental change in the Antarctic Peninsula region». The Holocene, 19, 51-69. BJORCK, S.; HJORT, C.; INGOLFSSON, O.; ZALE, R. y ISING, J. (1996): «Holocene deglaciation chronology from lake sediments» en Geomorphological Map of Byers Peninsula, Livingston Island (LÓPEZ-MARTÍNEZ, J.; THOMSON, M.R.A.; ARCHE, A.; BJORCK, S.; ELLIS-EVANS, J.C.; HATHWAY, B.; HERNÁNDEZ-CIFUENTES, F.; HJORT, C.; INGOLFSSON, O.; ISING, J.; LOMAS, S.; MARTÍNEZ DE PISÓN, E.; SERRANO, E.; KING, S. Eds.). British Antarctic Survey, Cambridge, 49-51. BRUNK, K. (1989): «Large scale geomorphologic-glaciological mapping of the arid high polar Borgmassivet, Neuschwabenland, Antarctica (1:50,000)». Berichte zur Polarforschung, 66, 102. CLAPPERTON, C.M. (1971): Geomorphology of the Stromness Bay-Cumberland Bay area, South Georgia. British Antarctic Survey Scientific Reports, 70, 1:50000, with supplementary text, 25 pp. Ó COFAIGH, C.; DAVIES, B.J.; LIVINGSTONE, S.J.; SMITH, J.A.; JOHNSON, J.S.; HOCKING, E.P.; HODGSON, D.A.; ANDERSON, J.B.; BENTLEY, M.J.; CANALS, M.; DOMACK, E.; DOWDESWELL, J.A.; EVANS, J.; GLASSER, N.F.; HILLENBRAND, C.D.; LARTER, R.D.; ROBERTS, S.J. y SIMMS, A.R. (2014): «Reconstruction of Ice-Sheet Changes in the Antarctic Peninsula since the Last Glacial Maximum». Quaternary Science Reviews, 100, 87-110. DAVIES, B.J.; GLASSER, N.F.; CARRIVICK, J.L.; HAMBREY, M.J.; SMELLIE, J.L. y NYVLT, D. (2013): «Landscape evolution and ice-sheet behaviour in a semi-arid polar environment: James Ross Island, NE Antarctic Peninsula». Special Publications of the Geological Society of London, 381 (1), 353-395. DE PABLO, M.A.; RAMOS, M. y MOLINA, A. (2014): «Thermal characterization of the active layer at the Limnopolar Lake CALM-S site on Byers Peninsula (Livingston Island), Antarctica». Solid Earth, 5, 721-739. DERBYSHIRE, E. y PETERSON, J.A. (1978): «A photo-geomorphic map of the Mt. Menzies Nunatak, Prince Charles Mountains, Australian Antarctic Territory». Zeitschrift Gletschergeshicte und Glazialgeologie, 14, 17-25. FRENCH, H.M. (2007): The periglacial environment. 3ª ed. Wiley, Chichester, UK. FORTIER, D. y Allard, M. (2004): «Late Holocene syngenetic ice-wedge polygons development, Bylot Island, Canadian Arctic Archipelago», Canadian Journal of Earth Sciences, 41, 997-1012. GÓMEZ-ORTIZ, A. (2006): La unidad geomorfológica del Veleta: enclave singular de Sierra Nevada, Organismo Autónomo Parques Nacionales, Ministerio Medio Ambiente, Bilbao. GOYANES, G.; VIEIRA, G.; CASELLI, A.; CARDOSO, M.; MAMY, A.; SANTOS, F.; BERNARDO, I. y HAUCK, C. (2014): «Local influences of geothermal anomalies on permafrost distribution in an active volcanic island (Deception Island, Antarctica)». Geomorphology, 225, 57-68. GUGLIELMIN, M.; BOSCHI, D.; D'AGATA, C.; ELLIS-EVANS, C. y WORLAND, M.R. (2008): «Periglacial and permafrost map of Signy Island, South Orkneys Islands, Maritime Antarctica» en Proceedings of 9th International Conference on Permafrost (KANE, D.L., HINKEL, K.M., Eds.). University of Alaska Fairbanks, Alaska, USA, 1, 569-574. HALL, B.L. y PERRY, E.R. (2004): «Variations in Ice Rafted Detritus on beaches in the South Shetland Islands: a possible climate proxy». Antarctic Science, 16, 339-344. HANSOM, J.D. (1979): «Radiocarbon dating of a raised beach at 10 m in the South Shetland Islands, Antarctica». Marine Geology, 53, 211-229. HATHWAY, B. y LOMAS, S.A. (1998): «The Upper Jurassic-Lower cretaceous Byers Group, South Shetland Islands, Antarctica: revised stratigraphy and regional correlations». Cretaceous Research, 19, 43-67. INGÓLFSSON, O.; HJORT, C.; BERKMAN, P.A.; BJÖRCK, S.; COLHOUN, E.; GOODWIN, I.D.; HALL, B.L.; HIRAKAWA, K.; MELLES, M. y PRENTICE, M.L. (1998): «Antarctic glacial history since the Last Glacial Maximum: an overview of the record on land». Antarctic Science, 10, 326-344. INGÓLFSSON, O.; HJORT, C. y HUMLUN; O. (2003): «Glacial and climate history of the Antarctic Peninsula since the Last Glacial Maximum». Arctic, Antarctic, and Alpine Research, 35, 175-186. JOLY, F. (1997): Glossaire de géomorphologie. Base de données sémiologiques pour la cartographie. Armand Colin, Paris. JOHN, B. y SUGDEN, D.E. (1971): «Raised marine features and phases of glaciation in the South Shetland Islands». British Antarctic Survey Bulletin, 24, 45-111. LIU, E.J.; OLIVA; M.; ANTONIADES, D.; GIRALT, S.; GRANADOS, I.; PLA-RABES, S.; TORO, M. y GEYER, A. (2015): «Expanding the tephrostratigraphical framework for the South Shetland Islands, Antarctica, by combining compositional and textural tephra characterisation». Sedimentary Geology, doi:10.1016/j.sedgeo.2015.08.002. LÓPEZ-MARTÍNEZ, J.; MARTÍNEZ DE PISÓN, E.; SERRANO, E. y ARCHE, A. (1996): Geomorphological map of Byers Peninsula, Livingston Island. BAS Geomap Series. Sheet 5-A, 1:25,000. British Antarctic Survey, Cambridge, UK. LÓPEZ-MARTÍNEZ, J. y SERRANO, E. (2002): «Geomorphology of Deception Island» en Geology and Geomorphology of Deception Island. BAS Geomap Series. Sheet 6-A and 6-B (LÓPEZ-MARTÍNEZ, J.; SMELLIE, J.L.; THOMSON, J.W.; THOMSON, M.R.A. Eds.), British Antarctic Survey, Cambridge, UK, 31–39. LÓPEZ-MARTÍNEZ, J.; SERRANO, E. y LEE, J.I. (2002): Geomorphological Map of Barton and Weaver Peninsulas. King George Island, Antarctica (1:10,000). Polar Science Laboratory, Korean Ocean Research and Development Institute KARP, Seul. LÓPEZ-MARTÍNEZ, J.; SERRANO, E.; REY, J. y SMELLIE, J.L. (2000): Geomorphological Map of Deception Island. BAS Geomap Series, Sheet 6-B, 1:25,000. British Antarctic Survey, Cambridge. LÓPEZ-MARTÍNEZ, J.; SERRANO, E.; SCHMID, T.; MINK, S. y LINÉS, C. (2012): «Periglacial processes and landforms in the South Shetland Islands (northern Antarctic Peninsula region)». Geomorphology, 155, 62-79. MARCHANT, D.R.; DENTON, G.H. y SWISHER, C.C. (1993): «Miocene-Pliocene-Pleistocene glacial history of Arena Valley, Quartermain Mountains, Antarctica». Geografiska Annaler, 75-A, 269-302. MARTÍNEZ-CORTIZAS, A.; ROZAS-MUÑIZ, I.; TABOADA, T.; TORO, T.; GRANADOS, I.; GIRAT, S. y PLA-RABAS, S. (2014): «Factors controlling the geochemical composition of Limnopolar Lake sediments (Byers Peninsula, Livingston Island, South Shetland Island, Antarctica) during the last ca. 1600 years». Solid Earth, 5, 651-663. MARTÍNEZ DE PISÓN, E. (2000): «El relieve de una vieja península volcánica en la Antártida: la Península de Byers en la Isla de Livingston». Ería, 53, 247-257. MARTÍNEZ DE PISÓN, E.; SERRANO, E.; ARCHE, A. y LÓPEZ-MARTÍNEZ, J. (1996): «Glacial geomorphology» en Geomorphological Map of Byers Peninsula, Livingston Island (LÓPEZ-MARTÍNEZ, J.; THOMSON, M.R.A.; ARCHE, A.; BJÖRCK, S.; ELLIS-EVANS, J.C.; HATHWAY, B.; HERNÁNDEZ-CIFUENTES, F.; HJORT, C.; INGOLFSSON, O.; ISING, J.; LOMAS, S.; MARTÍNEZ DE PISÓN, E.; SERRANO, E.; ZALE, R.; KING, S. Eds.). British Antarctic Survey, Cambridge, 23-27. MAYEWSKI, P.A. y GOLDTHWAIT R.P. (1985): «Glacial events in the Transantarctic Mountains». Antarctic Research Series, 36, 275-324. MICHEL, R.F.M.; SCHAEFER, C.E.G.R.; LÓPEZ-MARTÍNEZ, J.; SIMAS, F.N.B.; HAUS, N.W.; SERRANO, E. y BOCKHEIM, J. (2014): «Soils and landforms from Fildes Peninsula and Ardley Island, Maritime Antarctica». Geomorphology, DOI:10.1016/j.geomorph.2014.03.041. MILLIKEN, K.T.; ANDERSON, J.B.; WELLNER, J.S.; BOHATY, S.M. y MANLEY, P.L. (2009): «High resolution Holocene climate record from Maxwell Bay, South Shetland Islands, Antarctica». Geological Society of America Bulletin, 121, 1711-1725. MINK, S.; LÓPEZ-MARTÍNEZ, J.; MAESTRO, A.; GARROTE, J.; ORTEGA, J.A.; SERRANO, E.; DURÁN, J.J. y SCHMID, T. (2014): «Insights into deglaciation of the largest ice-free area in the South Shetland Islands (Antarctica) from quantitative analysis of the drainage system». Geomorphology, 225, 4-24. MULVANEY, R.; ABRAM, N.J.; GAGAN, M.K.; HINDMARSH, R.C.A.; ARROWSMITH, C. FLEET, L.; TRIEST, J.; SIME, L.C.; ALEMANEY, O. y FOORD, S. (2012): «Recent Antarctic Peninsula warming relative to Holocene climate and ice-shelf history». Nature, 489, 141-144. OLIVA, M.; ANTONIADES, D.; GIRALT, S.; GRANADOS, I.; PLA, S.; TORO, M.; SANJURJO, J.; LIU, E.J. y VIEIRA, G. (2016): «The Holocene deglaciation of the Byers Peninsula (Livingston Island, Antarctica) based on the dating of lake sedimentary records». Geomorphology. OLIVA, M.; VIEIRA, G.; PINA, P.; PEREIRA, P.; NEVES, M. y FREITAS, C. (2014): «Sedimentological characteristics of the ice-wedge polygon terrain in Adventalen (Svalbard) – environmental and climatic implications for the Late Holocene». Solid Earth, 5, 901-914. OLIVA, M. y RUIZ-FERNÁNDEZ, J. (2015): «Coupling patterns between para-glacial and permafrost degradation responses in Antarctica». Earth Surface Processes and Landforms, 40, 1227-1238. PARICA, C.A.; SALANI, F.M.; VERA, E.; REMESAL, M. y CÉSARI, S.N. (2007): «Geología de la formación Cerro Negro (Cretácico) en la isla Livingston: aportes a su geocronología y contenido paleontológico». Revista de la Asociación Geológica Argentina, 62, 553-567. PEARSON, M.; STEHBERG, R.; ZARANKÍN, A.; SENATORE, M.X. y GATICA, C. (2010): «Conserving the oldest historic sites in the Antarctic: the challenges in managing the sealing sites in the South Shetland Islands». Polar Record, 46, 57–64. RAFFI, R. y STENNI, B. (2011): «Isotopic composition and thermal regime of ice wedges in northern Victoria Land, East Antarctica». Permafrost and Periglacial Processes, 22, 65-83. SALVATORE, M.C.; BONDESAN, A.; MENEGHEL, M.; BARONI, C. y OROMBELLI, G. (1997): «Geomorphological sketch map of the Evans Cove area (Victoria Land, Antarctica)». Geografia Fisica e Dinamica Quaternaria, 20, 283-290. |
| op_rights | Copyright (c) 2016 Jesús Ruíz-Fernández, Marc Oliva, Cristina García-Hernández http://creativecommons.org/licenses/by-nc-sa/4.0 |
| op_rightsnorm | CC-BY-NC-SA |
| op_source | Polígonos. Revista de Geografía; Núm. 28 (2016): Periglaciarismo y Permafrost; 211-237 2444-0272 1132-1202 10.18002/pol.v0i28 |
| publishDate | 2016 |
| publisher | Universidad de León |
| record_format | openpolar |
| spelling | ftunivleonojs:oai:http://revpubli.unileon.es/ojs/:article/4294 2025-01-16T19:21:46+00:00 Procesos geomorfológicos y formas del relieve en dos cuencas lacustres de la península Byers (isla Livingston, Antártida marítima): implicaciones paleoambientales = Geomorphological processes and landforms in two lake catchments of Byers Peninsula (Livingston Island, Maritime Antarctica): paleoenvironmental implications Ruiz-Fernández, Jesús Oliva, Marc García-Hernández, Cristina Proyecto de investigación HOLOANTAR, financiado por la Fundación de Ciencia y Tecnología. Apoyo logístico del Programa Polar Portugués soporte de los programas antárticos de Brasil y Chile. Patrocinio de la AXA Research Fundation. Beca FPU 2016-10-11 application/pdf http://revistas.unileon.es/index.php/poligonos/article/view/4294 https://doi.org/10.18002/pol.v0i28.4294 spa spa Universidad de León http://revistas.unileon.es/index.php/poligonos/article/view/4294/3211 ARAYA, R. y HERVÉ, F. (1966): Estudio geomorfológico y geológico en las Islas Shetland del Sur, Antártida. Publicaciones del Instituto Antártico Chileno, 8, 76. BALCO; G., SCHAEFER, J.M. y LARISSA group (2013): «Exposure-age record of Holocene ice sheet and ice shelf change in the northeast Antarctic Peninsula». Quaternary Science Reviews, 59, 101-111. BAÑÓN, M.; JUSTEL, A.; VELÁZQUEZ, D. y QUESADA, A. (2013): «Regional weather survey on Byers Peninsula, Livingston Island, South Shetland Islands, Antarctica». Antarctic Science, 25, 146-156. BARONI, C.; BRUSCHI, G. y LÓPEZ-MARTÍNEZ, J. (1997): «Review of Antarctic geomorphological mapping». Geografia Fisica e Dinamica Quaternaria, 20, 15-31. BARONI, C. y OROMBELLI, G. (1994): «Holocene glaciar variations in the Terra Nova Bay area (Victoria Land, Antarctica)». Antarctic Science, 6, 497-505. BIASINI, A.; OSSO, P. y SALVATORE, M.C. (1997): «Geomorphological sketch map of the Mount Dickason area (Victoria Land, Antarctica) mapped by aerial photographs». Geografia Fisica e Dinamica Quaternaria, 20, 219-223. BIRKENMAJER, K. (1997): «Map of quaternary geology at Artowsky Station, King George Island, South Shetland Island (West Antarctica) 1/25000». Studia Geológica Polonica, 110. BENTLEY, M.J.; HODGSON, D.; SMITH, J.; O COFAIGH, C.; DOMACK, E.; LARTEER, R.; ROBERTS, S.; BRACHFELD, S.; LEVENTER, A.; HJORT, C.; HILLENBRAND, C. y EVANS, J. (2009): «Mechanisms of Holocene paleoenvironmental change in the Antarctic Peninsula region». The Holocene, 19, 51-69. BJORCK, S.; HJORT, C.; INGOLFSSON, O.; ZALE, R. y ISING, J. (1996): «Holocene deglaciation chronology from lake sediments» en Geomorphological Map of Byers Peninsula, Livingston Island (LÓPEZ-MARTÍNEZ, J.; THOMSON, M.R.A.; ARCHE, A.; BJORCK, S.; ELLIS-EVANS, J.C.; HATHWAY, B.; HERNÁNDEZ-CIFUENTES, F.; HJORT, C.; INGOLFSSON, O.; ISING, J.; LOMAS, S.; MARTÍNEZ DE PISÓN, E.; SERRANO, E.; KING, S. Eds.). British Antarctic Survey, Cambridge, 49-51. BRUNK, K. (1989): «Large scale geomorphologic-glaciological mapping of the arid high polar Borgmassivet, Neuschwabenland, Antarctica (1:50,000)». Berichte zur Polarforschung, 66, 102. CLAPPERTON, C.M. (1971): Geomorphology of the Stromness Bay-Cumberland Bay area, South Georgia. British Antarctic Survey Scientific Reports, 70, 1:50000, with supplementary text, 25 pp. Ó COFAIGH, C.; DAVIES, B.J.; LIVINGSTONE, S.J.; SMITH, J.A.; JOHNSON, J.S.; HOCKING, E.P.; HODGSON, D.A.; ANDERSON, J.B.; BENTLEY, M.J.; CANALS, M.; DOMACK, E.; DOWDESWELL, J.A.; EVANS, J.; GLASSER, N.F.; HILLENBRAND, C.D.; LARTER, R.D.; ROBERTS, S.J. y SIMMS, A.R. (2014): «Reconstruction of Ice-Sheet Changes in the Antarctic Peninsula since the Last Glacial Maximum». Quaternary Science Reviews, 100, 87-110. DAVIES, B.J.; GLASSER, N.F.; CARRIVICK, J.L.; HAMBREY, M.J.; SMELLIE, J.L. y NYVLT, D. (2013): «Landscape evolution and ice-sheet behaviour in a semi-arid polar environment: James Ross Island, NE Antarctic Peninsula». Special Publications of the Geological Society of London, 381 (1), 353-395. DE PABLO, M.A.; RAMOS, M. y MOLINA, A. (2014): «Thermal characterization of the active layer at the Limnopolar Lake CALM-S site on Byers Peninsula (Livingston Island), Antarctica». Solid Earth, 5, 721-739. DERBYSHIRE, E. y PETERSON, J.A. (1978): «A photo-geomorphic map of the Mt. Menzies Nunatak, Prince Charles Mountains, Australian Antarctic Territory». Zeitschrift Gletschergeshicte und Glazialgeologie, 14, 17-25. FRENCH, H.M. (2007): The periglacial environment. 3ª ed. Wiley, Chichester, UK. FORTIER, D. y Allard, M. (2004): «Late Holocene syngenetic ice-wedge polygons development, Bylot Island, Canadian Arctic Archipelago», Canadian Journal of Earth Sciences, 41, 997-1012. GÓMEZ-ORTIZ, A. (2006): La unidad geomorfológica del Veleta: enclave singular de Sierra Nevada, Organismo Autónomo Parques Nacionales, Ministerio Medio Ambiente, Bilbao. GOYANES, G.; VIEIRA, G.; CASELLI, A.; CARDOSO, M.; MAMY, A.; SANTOS, F.; BERNARDO, I. y HAUCK, C. (2014): «Local influences of geothermal anomalies on permafrost distribution in an active volcanic island (Deception Island, Antarctica)». Geomorphology, 225, 57-68. GUGLIELMIN, M.; BOSCHI, D.; D'AGATA, C.; ELLIS-EVANS, C. y WORLAND, M.R. (2008): «Periglacial and permafrost map of Signy Island, South Orkneys Islands, Maritime Antarctica» en Proceedings of 9th International Conference on Permafrost (KANE, D.L., HINKEL, K.M., Eds.). University of Alaska Fairbanks, Alaska, USA, 1, 569-574. HALL, B.L. y PERRY, E.R. (2004): «Variations in Ice Rafted Detritus on beaches in the South Shetland Islands: a possible climate proxy». Antarctic Science, 16, 339-344. HANSOM, J.D. (1979): «Radiocarbon dating of a raised beach at 10 m in the South Shetland Islands, Antarctica». Marine Geology, 53, 211-229. HATHWAY, B. y LOMAS, S.A. (1998): «The Upper Jurassic-Lower cretaceous Byers Group, South Shetland Islands, Antarctica: revised stratigraphy and regional correlations». Cretaceous Research, 19, 43-67. INGÓLFSSON, O.; HJORT, C.; BERKMAN, P.A.; BJÖRCK, S.; COLHOUN, E.; GOODWIN, I.D.; HALL, B.L.; HIRAKAWA, K.; MELLES, M. y PRENTICE, M.L. (1998): «Antarctic glacial history since the Last Glacial Maximum: an overview of the record on land». Antarctic Science, 10, 326-344. INGÓLFSSON, O.; HJORT, C. y HUMLUN; O. (2003): «Glacial and climate history of the Antarctic Peninsula since the Last Glacial Maximum». Arctic, Antarctic, and Alpine Research, 35, 175-186. JOLY, F. (1997): Glossaire de géomorphologie. Base de données sémiologiques pour la cartographie. Armand Colin, Paris. JOHN, B. y SUGDEN, D.E. (1971): «Raised marine features and phases of glaciation in the South Shetland Islands». British Antarctic Survey Bulletin, 24, 45-111. LIU, E.J.; OLIVA; M.; ANTONIADES, D.; GIRALT, S.; GRANADOS, I.; PLA-RABES, S.; TORO, M. y GEYER, A. (2015): «Expanding the tephrostratigraphical framework for the South Shetland Islands, Antarctica, by combining compositional and textural tephra characterisation». Sedimentary Geology, doi:10.1016/j.sedgeo.2015.08.002. LÓPEZ-MARTÍNEZ, J.; MARTÍNEZ DE PISÓN, E.; SERRANO, E. y ARCHE, A. (1996): Geomorphological map of Byers Peninsula, Livingston Island. BAS Geomap Series. Sheet 5-A, 1:25,000. British Antarctic Survey, Cambridge, UK. LÓPEZ-MARTÍNEZ, J. y SERRANO, E. (2002): «Geomorphology of Deception Island» en Geology and Geomorphology of Deception Island. BAS Geomap Series. Sheet 6-A and 6-B (LÓPEZ-MARTÍNEZ, J.; SMELLIE, J.L.; THOMSON, J.W.; THOMSON, M.R.A. Eds.), British Antarctic Survey, Cambridge, UK, 31–39. LÓPEZ-MARTÍNEZ, J.; SERRANO, E. y LEE, J.I. (2002): Geomorphological Map of Barton and Weaver Peninsulas. King George Island, Antarctica (1:10,000). Polar Science Laboratory, Korean Ocean Research and Development Institute KARP, Seul. LÓPEZ-MARTÍNEZ, J.; SERRANO, E.; REY, J. y SMELLIE, J.L. (2000): Geomorphological Map of Deception Island. BAS Geomap Series, Sheet 6-B, 1:25,000. British Antarctic Survey, Cambridge. LÓPEZ-MARTÍNEZ, J.; SERRANO, E.; SCHMID, T.; MINK, S. y LINÉS, C. (2012): «Periglacial processes and landforms in the South Shetland Islands (northern Antarctic Peninsula region)». Geomorphology, 155, 62-79. MARCHANT, D.R.; DENTON, G.H. y SWISHER, C.C. (1993): «Miocene-Pliocene-Pleistocene glacial history of Arena Valley, Quartermain Mountains, Antarctica». Geografiska Annaler, 75-A, 269-302. MARTÍNEZ-CORTIZAS, A.; ROZAS-MUÑIZ, I.; TABOADA, T.; TORO, T.; GRANADOS, I.; GIRAT, S. y PLA-RABAS, S. (2014): «Factors controlling the geochemical composition of Limnopolar Lake sediments (Byers Peninsula, Livingston Island, South Shetland Island, Antarctica) during the last ca. 1600 years». Solid Earth, 5, 651-663. MARTÍNEZ DE PISÓN, E. (2000): «El relieve de una vieja península volcánica en la Antártida: la Península de Byers en la Isla de Livingston». Ería, 53, 247-257. MARTÍNEZ DE PISÓN, E.; SERRANO, E.; ARCHE, A. y LÓPEZ-MARTÍNEZ, J. (1996): «Glacial geomorphology» en Geomorphological Map of Byers Peninsula, Livingston Island (LÓPEZ-MARTÍNEZ, J.; THOMSON, M.R.A.; ARCHE, A.; BJÖRCK, S.; ELLIS-EVANS, J.C.; HATHWAY, B.; HERNÁNDEZ-CIFUENTES, F.; HJORT, C.; INGOLFSSON, O.; ISING, J.; LOMAS, S.; MARTÍNEZ DE PISÓN, E.; SERRANO, E.; ZALE, R.; KING, S. Eds.). British Antarctic Survey, Cambridge, 23-27. MAYEWSKI, P.A. y GOLDTHWAIT R.P. (1985): «Glacial events in the Transantarctic Mountains». Antarctic Research Series, 36, 275-324. MICHEL, R.F.M.; SCHAEFER, C.E.G.R.; LÓPEZ-MARTÍNEZ, J.; SIMAS, F.N.B.; HAUS, N.W.; SERRANO, E. y BOCKHEIM, J. (2014): «Soils and landforms from Fildes Peninsula and Ardley Island, Maritime Antarctica». Geomorphology, DOI:10.1016/j.geomorph.2014.03.041. MILLIKEN, K.T.; ANDERSON, J.B.; WELLNER, J.S.; BOHATY, S.M. y MANLEY, P.L. (2009): «High resolution Holocene climate record from Maxwell Bay, South Shetland Islands, Antarctica». Geological Society of America Bulletin, 121, 1711-1725. MINK, S.; LÓPEZ-MARTÍNEZ, J.; MAESTRO, A.; GARROTE, J.; ORTEGA, J.A.; SERRANO, E.; DURÁN, J.J. y SCHMID, T. (2014): «Insights into deglaciation of the largest ice-free area in the South Shetland Islands (Antarctica) from quantitative analysis of the drainage system». Geomorphology, 225, 4-24. MULVANEY, R.; ABRAM, N.J.; GAGAN, M.K.; HINDMARSH, R.C.A.; ARROWSMITH, C. FLEET, L.; TRIEST, J.; SIME, L.C.; ALEMANEY, O. y FOORD, S. (2012): «Recent Antarctic Peninsula warming relative to Holocene climate and ice-shelf history». Nature, 489, 141-144. OLIVA, M.; ANTONIADES, D.; GIRALT, S.; GRANADOS, I.; PLA, S.; TORO, M.; SANJURJO, J.; LIU, E.J. y VIEIRA, G. (2016): «The Holocene deglaciation of the Byers Peninsula (Livingston Island, Antarctica) based on the dating of lake sedimentary records». Geomorphology. OLIVA, M.; VIEIRA, G.; PINA, P.; PEREIRA, P.; NEVES, M. y FREITAS, C. (2014): «Sedimentological characteristics of the ice-wedge polygon terrain in Adventalen (Svalbard) – environmental and climatic implications for the Late Holocene». Solid Earth, 5, 901-914. OLIVA, M. y RUIZ-FERNÁNDEZ, J. (2015): «Coupling patterns between para-glacial and permafrost degradation responses in Antarctica». Earth Surface Processes and Landforms, 40, 1227-1238. PARICA, C.A.; SALANI, F.M.; VERA, E.; REMESAL, M. y CÉSARI, S.N. (2007): «Geología de la formación Cerro Negro (Cretácico) en la isla Livingston: aportes a su geocronología y contenido paleontológico». Revista de la Asociación Geológica Argentina, 62, 553-567. PEARSON, M.; STEHBERG, R.; ZARANKÍN, A.; SENATORE, M.X. y GATICA, C. (2010): «Conserving the oldest historic sites in the Antarctic: the challenges in managing the sealing sites in the South Shetland Islands». Polar Record, 46, 57–64. RAFFI, R. y STENNI, B. (2011): «Isotopic composition and thermal regime of ice wedges in northern Victoria Land, East Antarctica». Permafrost and Periglacial Processes, 22, 65-83. SALVATORE, M.C.; BONDESAN, A.; MENEGHEL, M.; BARONI, C. y OROMBELLI, G. (1997): «Geomorphological sketch map of the Evans Cove area (Victoria Land, Antarctica)». Geografia Fisica e Dinamica Quaternaria, 20, 283-290. Copyright (c) 2016 Jesús Ruíz-Fernández, Marc Oliva, Cristina García-Hernández http://creativecommons.org/licenses/by-nc-sa/4.0 CC-BY-NC-SA Polígonos. Revista de Geografía; Núm. 28 (2016): Periglaciarismo y Permafrost; 211-237 2444-0272 1132-1202 10.18002/pol.v0i28 Geografía Geografía Física Cartografía geomorfológica Deglaciación Permafrost Evolución paleoambiental Paleolimnología Península Byers Antártida geomorphological mapping deglaciation paleoenvironmental evolution paleolimnology Byers Peninsula Antarctica info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Artículos 2016 ftunivleonojs https://doi.org/10.18002/pol.v0i28.4294 https://doi.org/10.18002/pol.v0i28 https://doi.org/10.1016/j.sedgeo.2015.08.002 https://doi.org/10.1016/j.geomorph.2014.03.041 2022-03-31T17:28:05Z En este artículo se estudian las cuencas y áreas circundantes de dos cuerpos lacustres situados en el sector oriental de la Península de Byers (isla Livingston, Antártida), Cerro Negro y Domo, con el objetivo de identificar los procesos geomorfológicos y formas de relieve existentes, así como las áreas fuente de sedimentos para los lagos. Para ello, se presenta una cartografía geomorfológica detallada de ambos sectores. En el área de Cerro Negro han sido diferenciadas cuatro unidades geomorfológicas: cerro, ladera Norte, escarpe meridional, y playas levantadas y playa actual. En el área de Domo se han diferenciado otras cuatro: lago y áreas planas adyacentes, laderas de la cuenca, interfluvios y afloramientos rocosos culminantes, y morrena del glaciar Rotch. Las evidencias geomorfológicas detectadas permiten realizar una reconstrucción paleoambiental en la que se diferencian tres fases: una fase de máxima expansión glaciar en la que solamente algunos nunataks sobresaldrían por encima del hielo; una segunda fase holocena de retroceso glaciar, formación de lagos e intensa dinámica periglaciar; y una tercera en la que se completa la deglaciación y la dinámica periglaciar se generaliza en las nuevas áreas libres de hielo, aunque con menor intensidad que en la fase previa.In this paper, lake catchments and surrounding areas of Cerro Negro and Domo lakes, eastern Byers Peninsula —Livingston Island, Antarctica—, are examined in order to identify both geomorphological processes and landforms, as well as to establish the sediment sources for lacustrine sedimentary processes. To do so, a detailed geomorphological mapping of both areas was carried out. Four geomorphological units were identified in the Cerro Negro area —hill, northern slope, southern scarp, and raised beaches and present-day beach—, as well as in the Domo area — lake and shorelines, slopes, watersheds and rocky outcrops, and moraine of Rotch Dome glacier—. Geomorphological evidences allowed to infer three paleoenvironmental stages: the first, in which only a reduced number of nunataks would protrude above the ice cap; a second stage characterized by glacial retreat during the Holocene, an intense periglacial dynamics and the formation of lakes; and the third one, in which the deglaciation was completed and periglacial activity became generalized, although with less intensity than in the previous phase. Article in Journal/Newspaper Antarc* Antarctic and Alpine Research Antarctic Science Antarctica Antártida Arctic Berichte zur Polarforschung British Antarctic Survey Bulletin Ice Ice cap Livingston Island permafrost Permafrost and Periglacial Processes Polar Record Polar Science Polar Science Polarforschung Revistas Universidad de León (ule) Byers ENVELOPE(-60.283,-60.283,-63.900,-63.900) Byers peninsula ENVELOPE(-61.066,-61.066,-62.633,-62.633) Cerro Negro ENVELOPE(-61.002,-61.002,-62.655,-62.655) Dome Glacier ENVELOPE(-94.068,-94.068,79.452,79.452) Hielo ENVELOPE(-58.133,-58.133,-62.083,-62.083) isla Livingston ENVELOPE(-60.500,-60.500,-62.600,-62.600) Livingston Island ENVELOPE(-60.500,-60.500,-62.600,-62.600) península Byers ENVELOPE(-61.083,-61.083,-62.633,-62.633) Rotch ENVELOPE(-60.883,-60.883,-62.633,-62.633) Rotch Dome ENVELOPE(-60.883,-60.883,-62.633,-62.633) Polígonos. Revista de Geografía 28 211 |
| spellingShingle | Geografía Geografía Física Cartografía geomorfológica Deglaciación Permafrost Evolución paleoambiental Paleolimnología Península Byers Antártida geomorphological mapping deglaciation paleoenvironmental evolution paleolimnology Byers Peninsula Antarctica Ruiz-Fernández, Jesús Oliva, Marc García-Hernández, Cristina Procesos geomorfológicos y formas del relieve en dos cuencas lacustres de la península Byers (isla Livingston, Antártida marítima): implicaciones paleoambientales = Geomorphological processes and landforms in two lake catchments of Byers Peninsula (Livingston Island, Maritime Antarctica): paleoenvironmental implications |
| title | Procesos geomorfológicos y formas del relieve en dos cuencas lacustres de la península Byers (isla Livingston, Antártida marítima): implicaciones paleoambientales = Geomorphological processes and landforms in two lake catchments of Byers Peninsula (Livingston Island, Maritime Antarctica): paleoenvironmental implications |
| title_full | Procesos geomorfológicos y formas del relieve en dos cuencas lacustres de la península Byers (isla Livingston, Antártida marítima): implicaciones paleoambientales = Geomorphological processes and landforms in two lake catchments of Byers Peninsula (Livingston Island, Maritime Antarctica): paleoenvironmental implications |
| title_fullStr | Procesos geomorfológicos y formas del relieve en dos cuencas lacustres de la península Byers (isla Livingston, Antártida marítima): implicaciones paleoambientales = Geomorphological processes and landforms in two lake catchments of Byers Peninsula (Livingston Island, Maritime Antarctica): paleoenvironmental implications |
| title_full_unstemmed | Procesos geomorfológicos y formas del relieve en dos cuencas lacustres de la península Byers (isla Livingston, Antártida marítima): implicaciones paleoambientales = Geomorphological processes and landforms in two lake catchments of Byers Peninsula (Livingston Island, Maritime Antarctica): paleoenvironmental implications |
| title_short | Procesos geomorfológicos y formas del relieve en dos cuencas lacustres de la península Byers (isla Livingston, Antártida marítima): implicaciones paleoambientales = Geomorphological processes and landforms in two lake catchments of Byers Peninsula (Livingston Island, Maritime Antarctica): paleoenvironmental implications |
| title_sort | procesos geomorfológicos y formas del relieve en dos cuencas lacustres de la península byers (isla livingston, antártida marítima): implicaciones paleoambientales = geomorphological processes and landforms in two lake catchments of byers peninsula (livingston island, maritime antarctica): paleoenvironmental implications |
| topic | Geografía Geografía Física Cartografía geomorfológica Deglaciación Permafrost Evolución paleoambiental Paleolimnología Península Byers Antártida geomorphological mapping deglaciation paleoenvironmental evolution paleolimnology Byers Peninsula Antarctica |
| topic_facet | Geografía Geografía Física Cartografía geomorfológica Deglaciación Permafrost Evolución paleoambiental Paleolimnología Península Byers Antártida geomorphological mapping deglaciation paleoenvironmental evolution paleolimnology Byers Peninsula Antarctica |
| url | http://revistas.unileon.es/index.php/poligonos/article/view/4294 https://doi.org/10.18002/pol.v0i28.4294 |