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  • 293G; AGE; Alboran Sea; Alkenone, unsaturation index UK'37; Calculated from LDI (Rampen et al., 2012); Calculated from UK'37 (Müller et al, 1998); DEPTH, sediment/rock; GC; Gravity corer; Long chain diol index; Professor Logachev; Sample code/label; Sea surface temperature, annual mean; TTR-12_293G; TTR-12/3  (1)
  • 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  (1)
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Keywords
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  • 1
    Publication Date: 2023-06-27
    Keywords: 293G; AGE; Alboran Sea; Alkenone, unsaturation index UK'37; Calculated from LDI (Rampen et al., 2012); Calculated from UK'37 (Müller et al, 1998); DEPTH, sediment/rock; GC; Gravity corer; Long chain diol index; Professor Logachev; Sample code/label; Sea surface temperature, annual mean; TTR-12_293G; TTR-12/3
    Type: Dataset
    Format: text/tab-separated-values, 485 data points
    Location Call Number Limitation Availability
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  • 2
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    PANGAEA
    In:  Supplement to: 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 (2012): The Medieval Climate Anomaly in the Iberian Peninsula reconstructed from marine and lake records. Quaternary Science Reviews, 43, 16-32, https://doi.org/10.1016/j.quascirev.2012.04.007
    Publication Date: 2023-12-20
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Limitation Availability
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