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  • 1
    Publication Date: 2023-01-13
    Description: Down core marine sediment samples from ODP Site 1240 have been used for the analysis of the C28 and C30 1,14-diols, the C37:2 and C37:3 long chain ketones (alkenones) and the 24-methylcholesta-5,22-dien-3β-ol (brassicasterol) as proxies of primary productivity. Alkenones were also used to infer past sea surface temperatures through the unsaturation index UK'37. The C29 n-alkane was measured to obtain information on continental material inputs. δD of C37-alkenones and δ¹⁸O-seawater of Globigerinoides ruber were used as indicators of relative salinity changes. This data has been used for the study of the period between 150 and 110 ka (sediment depth from ca. 13 to 17 m), according to the age model from Rippert et al. (2017).
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 2
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    PANGAEA
    In:  Supplement to: Català, Albert; Cacho, Isabel; Frigola, Jaime; Pena, Leopoldo D; Lirer, Fabrizio (2019): Holocene hydrography evolution in the Alboran Sea: a multi-record and multi-proxy comparison. Climate of the Past, 15(3), 927-942, https://doi.org/10.5194/cp-15-927-2019
    Publication Date: 2023-01-30
    Description: All data are based on the planktonic foraminifera Globigerina bulloides. SST are based on Mg/Ca ratios converted to SST by applying the calibration from Cisneros et al. (2016, doi:10.5194/cp-12-849-2016). Since this calibration was performed on non-reductive cleaned samples and, the Mg/Ca ratios from ALB-2 and MD99-2343 cores were obtained with the full reductive cleaning procedure, Mg/Ca ratios were increased by 12% prior to the calibration application. δ18O are also based in the same planktonic foraminifera Globigerina bulloides. ALB-2 record: A new deglacial and Holocene sea surface temperature (SST) and δ18O reconstructions are presented for the Alboran Sea (western Mediterranean) with its age-model. MD99-2343: A new deglacial and Holocene sea surface temperature (SST) reconstruction is presented for the Menorca Drift (western Mediterranean). The age-model has been improved from the originally published by Frigola et al. (2007, doi:10.1029/2006PA001307) for the last 17 kyr. MD95-2043: A new deglacial and Holocene sea surface temperature (SST) reconstruction is presented for the Alboran Sea (western Mediterranean).
    Keywords: Alboran Sea; Holocene; Mediterranean Sea; Sea Surface Tempertures; Stable isotopes
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 3
    Publication Date: 2023-02-07
    Keywords: AGE; Age, 14C; Age, maximum/old; Age, minimum/young; Age model; ALB-2; Alboran Sea; calculated by R; Comment; Core; CORE; DEPTH, sediment/rock; HER-GC-ALB2; Holocene; Mediterranean Sea; Sample comment; Sea Surface Tempertures; Stable isotopes
    Type: Dataset
    Format: text/tab-separated-values, 88 data points
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  • 4
    Publication Date: 2023-05-12
    Keywords: Age, 14C AMS; Age, 14C calibrated; Age, comment; Age, dated; Age, dated standard deviation; Calendar age; Calendar age, standard deviation; Calibration; CALYPSO; Calypso Corer; Comment; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Fraction; Fraction modern carbon; IMAGES; International Marine Global Change Study; Marion Dufresne (1995); Material; MD02-2594; MD128; Method comment; Reservoir effect/correction; Sample code/label; Southern Ocean; SWAF; Traces
    Type: Dataset
    Format: text/tab-separated-values, 196 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Martínez Méndez, Gema; Zahn, Rainer; Hall, Ian R; Peeters, Frank J C; Pena, Leopoldo D; Cacho, Isabel; Negre, César (2010): Contrasting multiproxy reconstructions of surface ocean hydrography in the Agulhas Corridor and implications for the Agulhas Leakage during the last 345,000 years. Paleoceanography, 25(4), PA4227, https://doi.org/10.1029/2009PA001879
    Publication Date: 2023-06-01
    Description: [1] Planktonic d18O and Mg/Ca-derived sea surface temperature (SST) records from the Agulhas Corridor off South Africa display a progressive increase of SST during glacial periods of the last three climatic cycles. The SST increases of up to 4°C coincide with increased abundance of subtropical planktonic foraminiferal marker species which indicates a progressive warming due to an increased influence of subtropical waters at the core sites. Mg/Ca-derived SST maximizes during glacial maxima and glacial Terminations to values about 2.5°C above full-interglacial SST. The paired planktonic d18O and Mg/Ca-derived SST records yield glacial seawater d18O anomalies of up to 0.8 per mill, indicating measurably higher surface salinities during these periods. The SST pattern along our record is markedly different from a UK'37-derived SST record at a nearby core location in the Agulhas Corridor that displays SST maxima only during glacial Terminations. Possible explanations are lateral alkenone advection by the vigorous regional ocean currents or the development of SST contrasts during glacials in association with seasonal changes of Agulhas water transports and lateral shifts of the Agulhas retroflection. The different SST reconstructions derived from UK'37 and Mg/Ca pose a significant challenge to the interpretation of the proxy records and demonstrate that the reconstruction of the Agulhas Current and interocean salt leakage is not as straightforward as previously suggested.
    Keywords: IMAGES; International Marine Global Change Study
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 6
    Publication Date: 2023-06-27
    Keywords: 98; AGE; Benthic foraminifera; CALYPSO; Calypso Corer; Counting 〉63 µm fraction; Foraminifera, benthic; Grain size data; Gyroidina spp.; High oxygen indicators; IMAGES V; Low oxygen indicators; Marion Dufresne (1995); MD114; MD99-2343; North Minorca; Stable isotopes; TOC
    Type: Dataset
    Format: text/tab-separated-values, 400 data points
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  • 7
    Publication Date: 2023-06-27
    Keywords: 98; AGE; Benthic foraminifera; CALYPSO; Calypso Corer; Grain size data; IMAGES V; Marion Dufresne (1995); MD114; MD99-2343; North Minorca; Size fraction 〉 0.010 mm; Stable isotopes; TOC
    Type: Dataset
    Format: text/tab-separated-values, 188 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Pérez-Asensio, José N; Frigola, Jaime; Pena, Leopoldo D; Sierro, Francisco Javier; Reguera, Maria Isabel; Rodríguez-Tovar, Francisco Javier; Dorador, Javier; Asioli, Alessandra; Kuhlmann, Jannis; Huhn, Katrin; Cacho, Isabel (2020): Changes in western Mediterranean thermohaline circulation in association with a deglacial Organic Rich Layer formation in the Alboran Sea. Quaternary Science Reviews, 228, 106075, https://doi.org/10.1016/j.quascirev.2019.106075
    Publication Date: 2023-06-05
    Description: The accumulation of an Organic Rich Layer (ORL) during the last deglaciation in the Alboran Sea (western Mediterranean Sea) and its link to changes in deep and intermediate water circulation are here investigated. Benthic foraminiferal assemblages and the shallow infaunal foraminifer Uvigerina peregrina δ13C record support the establishment of sustained high organic matter fluxes, and thus eutrophic conditions at the sea floor, during the late phase of the ORL (Younger Dryas to early Holocene periods). Since organic matter fluxes were lower (mesotrophic conditions) during the Bølling-Allerød period, they cannot be solely responsible for the ORL initiation. Geochemical, sedimentological and micropalaeontological proxies support a major weakening of the deep-water convection in the Gulf of Lion as the main driver for the development of poorly-ventilated conditions from intermediate depths (946 m) to the deep western Mediterranean basin that promoted the beginning of the ORL deposition. Nevertheless, a better ventilation at intermediate depths was established during the late ORL, while the deep basin remained poorly ventilated. We propose that our data reflect the arrival of a new better-ventilated intermediate water mass analogue to the current Levantine Intermediate Water (LIW) and/or a new intermediate water mass from the Gulf of Lion. The ultimate source of this water mass needs to be further explored but chronologies of the changes recorded here indicate that intermediate and deep ventilation phases were decoupled between the western and eastern Mediterranean basins during the deglaciation and early-middle Holocene.
    Keywords: Benthic foraminifera; Grain size data; Stable isotopes; TOC
    Type: Dataset
    Format: application/zip, 18 datasets
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  • 9
    Publication Date: 2023-07-09
    Keywords: 98; Ammodiscus spp.; Ammolagena clavata; Ammonia falsobeccarii; Amphicoryna scalaris; Articulina tubulosa; Astacolus spp.; Astrononion stelligerum; Benthic foraminifera; Biloculinella elongata; Biloculinella globulus; Biloculinella wiesneri; Bolivina dilatata; Bolivina pseudoplicata; Bolivina spathulata; Brizalina alata; Brizalina subaenariensis; Bulimina aculeata; Bulimina alazanensis; Bulimina inflata; Bulimina marginata; Bulimina striata; CALYPSO; Calypso Corer; Cassidulina crassa; Cassidulina laevigata; Chilostomella oolina; Cibicides lobatulus; Cibicidoides pachyderma; Cibicidoides wuellerstorfi; Cornuspira foliacea; Cornuspira involvens; Cornuspira spp.; Counting 〉63 µm fraction; Cribrononion kerguelenense; Cycloforina spp.; Cyclophtalmidium spp.; Dentalina aphelis; Dentalina inflexa; Dentalina spp.; DEPTH, sediment/rock; Eggerella bradyi; Elphidium aculeatum; Elphidium advenum; Elphidium complanatum; Elphidium gensenii; Elphidium poeyanum; Fissurina radiata; Fissurina sp.; Foraminifera, benthic; Foraminifera, benthic agglutinated; Foraminifera, benthic indeterminata; Frondicularia spp.; Fursenkoina rotundata; Fursenkoina spp.; Gavelinopsis praegeri; Globobulimina pacifica; Globocassidulina subglobosa; Globulotuba spp.; Glomospira charoides; Grain size data; Gyroidina altiformis; Gyroidina parva; Gyroidinoides spp.; Hansenisca soldanii; Hanzawaia boueana; Hanzawaia spp.; Haplophragmoides spp.; Haynesina germanica; Haynesina spp.; Hoeglundina elegans; Hyalinea balthica; IMAGES V; Karreriella bradyi; Lagena acuticosta; Lagena doveyensis; Lagena hexagona; Lagena hispidula; Lagena sp.; Lagena spp.; Lagena striata; Lagena sulcata; Lenticulina gibba; Lenticulina iota; Lenticulina peregrina; Lenticulina spp.; Marginulina obesa; Marginulina spp.; Marion Dufresne (1995); MD114; MD99-2343; Melonis affinis; Melonis pompilioides; Miliolinella dilatata; Miliolinella elongata; Miliolinella spp.; Miliolinella subrotunda; Neoconorbina terquemi; Nodosaria spp.; Nonionella turgida; Nonion fabum; North Minorca; Nummoloculina sp.; Oolina hexagona; Oolina spp.; Paliolatella sp.; Patellina corrugata; Planorbulina mediterranensis; Polymorphina spp.; Praeglobobulimina pupoides; Procerolagena gracilis; Procerolagena gracillima; Pseudoglandulina glanduliniformis; Pseudotriloculina oblonga; Pullenia bulloides; Pullenia quinqueloba; Pullenia spp.; Pyrgo comata; Pyrgo depressa; Pyrgoella elongata; Pyrgoella sphaera; Pyrgo elongata; Pyrgo lucernula; Pyrgo sarsi; Quinqueloculina jugosa; Quinqueloculina lamarckiana; Quinqueloculina oblonga; Quinqueloculina seminulum; Quinqueloculina sp.; Quinqueloculina spp.; Quinqueloculina ungeriana; Quinqueloculina venusta; Rectuvigerina spp.; Robertina tasmanica; Rosalina auberiana; Rosalina bradyi; Rosalina globularis; Rosalina spp.; Sigmoilopsis schlumbergeri; Siphotextularia spp.; Spiroloculina bradyiana; Spiroloculina tenuiseptata; Spirophthalmidium acutimargo; Spirosigmoilina tenuis; Stable isotopes; Subreophax monile; Textularia pseudorugosa; TOC; Trifarina carinata; Triloculina adriatica; Triloculina sp.; Triloculina spp.; Triloculina tricarinata; Uvigerina mediterranea; Uvigerina peregrina; Uvigerina proboscidea; Valvulineria bradyana
    Type: Dataset
    Format: text/tab-separated-values, 12160 data points
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  • 10
    Publication Date: 2023-07-10
    Keywords: AGE; ALB-2; Alboran Sea; Core; CORE; Depth, composite; Globigerina bulloides, Magnesium/Calcium ratio; HER-GC-ALB2; Holocene; Mediterranean Sea; Sea surface temperature; Sea surface temperature, standard error; Sea Surface Tempertures; Stable isotopes
    Type: Dataset
    Format: text/tab-separated-values, 1460 data points
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