Age determination and sea surface temperature reconstruction from marine and lake records, Iberian Peninsula
Fuente:
PANGAEA
Salvato in:
| Autori principali: | , , , , , , , , , , , , , , , , , , , |
|---|---|
| Natura: | Dataset Open Access |
| Lingua: | en |
| Pubblicazione: |
PANGAEA
2012
|
| Soggetti: | |
| Accesso online: | |
| Tags: |
Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne!!
|
| _version_ | 1867168560318513152 |
|---|---|
| author | Moreno, Ana Pérez, Ana Frigola, Jaime Nieto-Moreno, Vanesa Rodrigo-Gámiz, Marta Martrat, Belén González-Sampériz, Penélope Morellón, Mario Martín-Puertas, Celia Corella, Juan Pablo Belmonte, Ánchel Sancho, Carlos Cacho, Isabel Herrera, Gemma Canals, Miquel Grimalt, Joan O Jiménez-Espejo, Francisco Jose Martinez-Ruiz, Francisca C Vegas-Vilarrúbia, Teresa Valero-Garcés, Blas L |
| author_facet | Moreno, Ana Pérez, Ana Frigola, Jaime Nieto-Moreno, Vanesa Rodrigo-Gámiz, Marta Martrat, Belén González-Sampériz, Penélope Morellón, Mario Martín-Puertas, Celia Corella, Juan Pablo Belmonte, Ánchel Sancho, Carlos Cacho, Isabel Herrera, Gemma Canals, Miquel Grimalt, Joan O Jiménez-Espejo, Francisco Jose Martinez-Ruiz, Francisca C Vegas-Vilarrúbia, Teresa Valero-Garcés, Blas L |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Selected multi-proxy and accurately dated marine and terrestrial records covering the past 2000 years in the Iberian Peninsula (IP) facilitated a comprehensive regional paleoclimate reconstruction for the Medieval Climate Anomaly (MCA: 900-1300 AD). The sequences enabled an integrated approach to land-sea comparisons and, despite local differences and some minor chronological inconsistencies, presented clear evidence that the MCA was a dry period in the Mediterranean IP. It was a period characterized by decreased lake levels, more xerophytic and heliophytic vegetation, a low frequency of floods, major Saharan eolian fluxes, and less fluvial input to marine basins. In contrast, reconstruction based on sequences from the Atlantic Ocean side of the peninsula indicated increased humidity. The data highlight the unique characteristics of the MCA relative to earlier (the Dark Ages, DA: ca. 500-900 years AD) and subsequent (the Little Ice Age, LIA: 1300-1850 years AD) colder periods. The reconstruction supports the hypothesis of Trouet et al. (2009, doi:10.1126/science.1166349), that a persistent positive mode of the North Atlantic Oscillation (NAO) dominated the MCA. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_780423 |
| institution | PANGAEA |
| language | en |
| publishDate | 2012 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Age determination and sea surface temperature reconstruction from marine and lake records, Iberian Peninsula Moreno, Ana Pérez, Ana Frigola, Jaime Nieto-Moreno, Vanesa Rodrigo-Gámiz, Marta Martrat, Belén González-Sampériz, Penélope Morellón, Mario Martín-Puertas, Celia Corella, Juan Pablo Belmonte, Ánchel Sancho, Carlos Cacho, Isabel Herrera, Gemma Canals, Miquel Grimalt, Joan O Jiménez-Espejo, Francisco Jose Martinez-Ruiz, Francisca C Vegas-Vilarrúbia, Teresa Valero-Garcés, Blas L 305G; 306G; Algerian-Balearic basin; Basa de la Mora lake; BSM08-1A-1U-1; BSM08-1A-2U-1; Central Pyrenees; CNRS_HERMES3; GC; Gravity corer; MIN2400, MIN1; MIN2400, MIN2; MINMC06-1; MINMC06-2; Minorca contourite; MUC; MultiCorer; Tethys II Selected multi-proxy and accurately dated marine and terrestrial records covering the past 2000 years in the Iberian Peninsula (IP) facilitated a comprehensive regional paleoclimate reconstruction for the Medieval Climate Anomaly (MCA: 900-1300 AD). The sequences enabled an integrated approach to land-sea comparisons and, despite local differences and some minor chronological inconsistencies, presented clear evidence that the MCA was a dry period in the Mediterranean IP. It was a period characterized by decreased lake levels, more xerophytic and heliophytic vegetation, a low frequency of floods, major Saharan eolian fluxes, and less fluvial input to marine basins. In contrast, reconstruction based on sequences from the Atlantic Ocean side of the peninsula indicated increased humidity. The data highlight the unique characteristics of the MCA relative to earlier (the Dark Ages, DA: ca. 500-900 years AD) and subsequent (the Little Ice Age, LIA: 1300-1850 years AD) colder periods. The reconstruction supports the hypothesis of Trouet et al. (2009, doi:10.1126/science.1166349), that a persistent positive mode of the North Atlantic Oscillation (NAO) dominated the MCA. |
| title | Age determination and sea surface temperature reconstruction from marine and lake records, Iberian Peninsula |
| topic | 305G; 306G; Algerian-Balearic basin; Basa de la Mora lake; BSM08-1A-1U-1; BSM08-1A-2U-1; Central Pyrenees; CNRS_HERMES3; GC; Gravity corer; MIN2400, MIN1; MIN2400, MIN2; MINMC06-1; MINMC06-2; Minorca contourite; MUC; MultiCorer; Tethys II |
| url | https://doi.org/10.1594/PANGAEA.780423 |