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LoDico, Jenna M; Flower, Benjamin P; Quinn, Terrence Michael (2006): High resolution stable isotope and Mg/Ca record of sediment core MD02-2550C2 [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.833786, Supplement to: LoDico, JM et al. (2006): Subcentennial-scale climatic and hydrologic variability in the Gulf of Mexico during the early Holocene. Paleoceanography, 21(3), PA3015, https://doi.org/10.1029/2005PA001243

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Abstract:
An early Holocene record from the Gulf of Mexico (GOM) reveals climatic and hydrologic changes during the interval from 10.5 to 7 thousand calendar years before present from paired analyses of Mg/Ca and d18O on foraminiferal calcite. The sea surface temperature record based on foraminiferal Mg/Ca contains six oscillations and an overall ~1.5°C warming that appears to be similar to the September-March insolation difference. The d18O of seawater in the GOM (d18OGOM) record contains six oscillations, including a -0.8 per mil excursion that may be associated with the "8.2 ka climate event" or a broader climate anomaly. Faunal census records from three GOM cores exhibit similar changes, suggesting subcentennial-scale variability in the incursions of Caribbean waters into the GOM. Overall, our results provide evidence that the subtropics were characterized by decadal- to centennial-scale climatic and hydrologic variability during the early Holocene.
Coverage:
Latitude: 26.946200 * Longitude: -91.345700
Date/Time Start: 2002-07-08T16:18:00 * Date/Time End: 2002-07-08T16:18:00
Event(s):
MD02-2550C2 (MD022550C2) * Latitude: 26.946200 * Longitude: -91.345700 * Date/Time: 2002-07-08T16:18:00 * Elevation: -2248.0 m * Recovery: 9.09 m * Location: Orca Basin * Campaign: MD127 (IMAGES IX - PAGE) * Basis: Marion Dufresne (1995) * Method/Device: Calypso Square Core System (CASQS)
Size:
2 datasets

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