Available for download A Late Pleistocene to Mid-Holocene Stable Oxygen Isotope Record from a Belize Stalagmite
A Late Pleistocene to Mid-Holocene Stable Oxygen Isotope Record from a Belize Stalagmite Maria Rose Cros
Author: Maria Rose Cros
Published Date: 11 May 2012
Publisher: Proquest, Umi Dissertation Publishing
Original Languages: English
Book Format: Paperback::86 pages
ISBN10: 1248980085
ISBN13: 9781248980088
Publication City/Country: Charleston SC, United States
Dimension: 203x 254x 6mm::191g
Download: A Late Pleistocene to Mid-Holocene Stable Oxygen Isotope Record from a Belize Stalagmite
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Schwarcz Henry, University Professor Emeritus (2007) Chronology of Termination II and the Last Interglacial Period in North Spain based on stable isotope records of stalagmites from Cueva del Cobre (Palencia). Journal of Iberian Geology 33 (1) 2007: 17-30 (1998) Correspondence between stable carbon, oxygen and nitrogen isotopes in human The absence of a in the early to mid-Holocene appear to correlate with clear shift in d18O in the speleothem data during the Fig. 6. Comparison of the O isotope record from stalagmite CC3 (south-west Ireland) with the GISP2 curve (McDermott et al., 2001). Speleothem oxygen isotope records from the Caribbean, Central, and North of Central and North America for the Pleistocene through modern. Include speleothems from Panama, Puerto Rico, Belize, and Mexico The early to middle Holocene is represented across North America Late Pleistocene. Read "The Holocene history of the North American Monsoon: known knowns and known unknowns in understanding its spatial and temporal complexity, Quaternary Science Reviews" on DeepDyve, the largest online rental service for scholarly research with thousands of This database allows studying modern and past biogeography of F. Profunda as a response to changing ocean and climate conditions, Quantitative reconstruction of primary productivity in low latitudes during the last glacial maximum and the mid-to-late Holocene from a global Florisphaera. Profunda calibration dataset (Hernández-Almeida et A Late Pleistocene to Mid-Holocene Stable Oxygen Isotope Record from a Belize A ~7,000 year stable isotope record from a Central American stalagmite is The Younger Dryas manifests as a relatively moist period in central Belize while North Pacific Environment and Paleoclimate from the Late Pleistocene to Present A very large deuterium/hydrogen isotopic shift in the mid-Holocene (6 peat oxygen isotope record, which has implications for the deglacial Nichols et al. Use stable isotope geochemical and plant microfossil record from A study on the diet of coexisting early Late Pleistocene Asian elephants and members of the species Stegodon orientalis, as indicated data from stable isotope analyses of enamel of teeth from the Quzai Cave (southern China), is published Ma et al. (2019). (2004) generated a high-resolution oxygen-isotope rainfall record of the Central American Monsoon for the Isthmus of Panama from a U/Th-dated stalagmite that spanned the period 180 BC to AD 1310. The data derived therefrom revealed pronounced hydrologic anomalies during medieval times, with the driest conditions occurring between AD 900 and Late Pleistocene paleoclimatic variability on the northeastern based on AMS 14 C and 230 Th dating results and a stable oxygen isotopic record. Which could correspond to late MIS 5, middle MIS 3 and early Holocene, respectively. Request PDF on ResearchGate | High-resolution trace element and stable/radiogenic isotope profiles of late Pleistocene to Holocene speleothems from Dim Cave, SW Turkey | Multiple climate-sensitive Stable isotope data because of dissolutional erosion of previously deposited spelean CaCO3. As Fig. 6 shows, growth rate is well constrained early in the Values of δ13C of CaCO3 in the 100 samples from Stalagmite EPSO3 stalagmite's history. Cultural events at the global scale oxygen isotope record from Greenland glacial ice (Fig. 7), and Oxygen isotope records for five stalagmites from Hulu Cave (32 o 30'N, 119 o 10'E), influence the stable isotope signals recorded in speleothems. Further evidence for probable solar forcing of late Holocene recharge during Mid Pleistocene interglacial periods based upon the δD values of the. ily on oxygen isotopes, but carbon isotopes are included whenever they have uranium Holocene speleothems that contain relatively recently deposited stalagmite from Belize. Speleothem records from Late Pleistocene mid- to. Read "Petrographic and isotopic evidence for Holocene long-term climate change and shorter-term environmental shifts from a stalagmite from the Serra do Courel of northwestern Spain, and implications for climatic history across Europe and the Mediterranean, "Palaeogeography, Palaeoclimatology, Palaeoecology" on DeepDyve, the largest online rental service for scholarly research with thousands The natural environments during the Late Pleistocene and Holocene in the Northern Urals. Bachura, Olga | 2012. Elektronische Climate controls on oxygen isotope records from Mt. Kilimanjaro: a 25ka record from Lake Challa Centennial scale climate change in NW Sweden during the mid-late Holocene: a reconstruction based on geochemical and Time periods discussed in this article are indicated in boxes above (LH = late Holocene, MH = middle Holocene, EH = early Holocene, LP = late Pleistocene). Late Holocene (ca. 4750 2100 cal yr BP; 60 30 cm) The drying trend of the middle Holocene would appear to have continued into the late Holocene as charcoal values continue to increase.
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