Persona: Lario Gómez, Javier
Cargando...
Dirección de correo electrónico
ORCID
0000-0002-2582-5354
Fecha de nacimiento
Proyectos de investigación
Unidades organizativas
Puesto de trabajo
Apellidos
Lario Gómez
Nombre de pila
Javier
Nombre
12 resultados
Resultados de la búsqueda
Mostrando 1 - 10 de 12
Publicación La Cueva del Boquerón(TIASA, 1997) Lario Gómez, JavierPublicación Episodios marinos del Último Interglacial (Estadio Isotópico 5) del litoral de Málaga (SE Peninsular)(Universidad de Málaga (UMA), 1999) Zazo Cardeña, Caridad; Hillaire Marcel, Claude; Goy Goy, José Luis; Hoyos Gómez, Manuel; Lario Gómez, JavierLa cronoestratigrafía del Cuaternario en el litoral bético mediterráneo ha sido construida fundamentalmente en base a la cartografía y correlación entre las distintas secuencias de episodios marinos y continentales desarrollados en cada una de las cuencas. La cronología entre las distintas unidades morfosedimentarias se ha hecho en base a su disposición relativa, distribución regional, datos paleomagnéticos y contenido faunístico. El gran desarrollo que presentan en este litoral los depósitos tirrenienses con abundancia de fauna, ha hecho posible la utilización de dataciones isotópicas que han permitido caracterizar cronológicamente los episodios cálidos registrados desde el final del Pleistoceno medio.Publicación Geomorfología litoral y cárstica en la penibética malagueña(Universidad de Barcelona, 1998) Malvárez, G.; Zazo Cardeña, Caridad; Goy Goy, José Luis; Luque, L.; Lario Gómez, JavierPublicación Sea level and climate changes in the Cabo De Gata Lagoon (Almeria) during the last 6500 YR BP(INQUA, International Union For Quaternary Research, 1998) Goy Goy, José Luis; Zazo Cardeña, Caridad; Dabrio, Cristino José; Baena Preysler, Javier; Harvey, A. M.; Silva, Pablo Gabriel; González, F.; Lario Gómez, JavierThe Holocene evolution of the lagoon of Cabo de Gata in the geodynamic framework of the south-eastem lberian Península is presented for the first time. The work is based on detail geomorphological mapping of the Quaternary deposits, and radiocarbon measurements of samples collected in the spit barrier systems. The genesis of the Cabo de Gata and Roquetas lagoons is connected to the joint action of three factors. ( l ) Neotectonics, that controlled the occurrence of lowlands. (2) The general glacio-eustatic, Holocene transgression, that brought the sea level to elevations 1.5-2 m above its present values and, eventually, flooded the lowlands during the Flandrian maximum ca. 6500 yr BP. (3) The climate (humidity/aridity) that influenced the sediment supply to the coast and also the small fluctuations of sea level after the Flandrian maximum. Four spit-barrier units have been distinguished. Deposition of the two older ones (H1 and H2 ) took place between ca. 6500 and ca. 2500 yr BP under longshore drift towards the NW. Both units enclosed a lagoon that ·is placed to the NE of its present position. The more recent units (H3 and H4) close the present lagoon and were deposited between ca. 2300 and present under longshore drift to the SE. A more hum id period has been identified during the Gap separating units H1 and H2 (ca. 4400- 4200 yr BP) when most holocene alluvial fans were deposited. Aridity increased after ca. 2500 yr BP when aeolianPublicación Changes in littoral dynamics and sea level in southern Iberia and Canary Istands during the Holocene.(Sociedad Geológica de España, 1996) Zazo Cardeña, Caridad; Dabrio, Cristino José; Goy Goy, José Luis; Bardají, Teresa; Ghaleb, B.; Lario Gómez, Javier; https://orcid.org/0000-0003-2988-8077The interaction between global factors tglobal" glacio-eustatic sea-leve/ rise) and regional factors (tectonic trend, oceanographic factor) is analyzed in different areas of the lberian and Canary lsland littora/. Sea-leve/ changes and climatic variations are stated for the Mediterranean and Atlantic littora/s, with different tidal ranges and tectonic trends. Different stages can be envisaged in the coastal evolution of a/most ali the analyzed areas from the beginning of Holocene (10.000 BP): at ca. 7.000 BP (Flandrian maximum) with a change from open estuaries to aggradational processes (Cádiz Gulf, subsiding area), basal peat (Valencia Gulf, subsiding area) and development of microcliffs (Mediterranean uplifting areas). From 7,000 to 2,700 BP a first progradation phase with development of spit bars took place in the mediterranean uplifting areas, whilst in the atlantic subsiding one starts the aggradation processes in the formerly open estuaries, an a/so from ca.4,000 BP development of spit-bar system. A second progradation phase ofthe spit bars systems occurs between 2,400 and 500 BP both in Almería and Cádiz Gulf, where a change from aggradation to progradation takes place in the estuary environments, and with a change in the direction of /ongshore drift (Mediterranean) and prevailing winds (both areas) at ca.2,400 BP. At ca. 1,200 BP a sudden paleogeographic change took place in estuary environments. From 500 BP up to now a marked increase of coastal progradation in ali littorals is observed. Climatic interpretations /ed to corre/ate anticyclonic conditions (as it happened during Little Ice Ages) with the growing of spit bar systems and progradation, while low pressure conditions (as during Medieval Warm Period) coincides with no progradation. In the Canary lslands, the development of storm ridges at ca. 3,500 BP can be corre/ated with an intensification of trade winds.Publicación Petrología de los materiales karstificables(Federación Española de Espeleología, 1995) Rossi Nieto, Carlos; Lario Gómez, JavierPublicación Is the Younger Dryas recorded in the estuarine sediments from south western Iberia Peninsula?(INQUA Mediterranean and Black Sea Shorelines Subcom, 1997) Lario Gómez, JavierPublicación Holocene incised-valley fills and coastal evolution in the Gulf of Cádiz (Southern Spain)(INQUA, International Union For Quaternary Research, 1998) Dabrio, Cristino José; Zazo Cardeña, Caridad; Goy Goy, José Luis; Sierro, F. J.; Borja, Francisco; González Delgado, José Ángel; Flores Villarejo, José Abel; Lario Gómez, JavierPublicación Último y Presente Interglacial en el área de conexión Atlántico-Mediterráneo (sur de España). Variaciones del nivel del mar, Paleoclima y Paleoambientes.(Tesis)(['CSIC. Departamento de Geología Museo Nacional de Ciencias Naturales.', 'UCM. Departamento de Geodinámica de la Facultad de Ciencias Geológicas'], 1996) Lario Gómez, JavierPublicación Paraje Natural de las Marismas del Odiel(AEQUA, 1997) Rubio, Juan Carlos; Borja, Francisco; Bedia, Juana; Cáceres, Luis Miguel; Clemente, L.; Morón, M. Carmen; Barral, María de los Ángeles; Lario Gómez, Javier