noaa-ocean-26910 Murray Canyon MD03-2611 Holocene Foraminifera Stable Isotope Data Moros, M.; De Deckker, P.; Jansen, E.; Perner, K.; Telford, R.J. Murray Canyon MD03-2611 Holocene Foraminifera Stable Isotope Data 2019-05-27 NCDC-Paleoclimatology ONLINE Files Pending https://www.ncdc.noaa.gov/paleo/study/26910 Investigator M. Moros Investigator P. De Deckker Investigator E. Jansen Investigator K. Perner Investigator R.J. Telford earth science paleoclimate paleocean oxygen isotopes earth science paleoclimate paleocean carbon isotopes geoscientificInformation 32512 cal yr BP 0 cal yr BP Complete -36.73 -36.73 136.55 136.55 -2420 -2420 Ocean Pacific Ocean South Pacific Ocean MD03-2611>LATITUDE -36.73>LONGITUDE 136.55 None Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site. English DOC/NOAA/NESDIS/NCEI National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce https://www.ncdc.noaa.gov/data-access/paleoclimatology-data DATA Center Contact Bruce Bauer bruce.a.bauer@noaa.gov paleo@noaa.gov 303-497-6280 303-497-6513

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Boulder CO 80305-3328 USA online ASCII Matthias Moros, Patrick De Deckker, Eystein Jansen, Kerstin Perner, Richard J. Telford 2009 Quaternary Science Reviews 28 19-20 1932-1940 10.1016/j.quascirev.2009.04.007 https://www.sciencedirect.com/science/article/pii/S0277379109001280

To understand Holocene climatic development and to determine drivers of climatic changes and climate variability, high-resolution marine proxy records are required from key oceanic locations. However, information on the Holocene climate development from the Southern Hemisphere is still rare and mainly based on terrestrial archives. Here, we present data with a high-resolution of circa 35 years from sediment cores taken east of the Great Australian Bight, where it is possible to determine Southern Ocean Holocene climate and the longer-term trends of the El Nino-Southern Oscillation (ENSO) conditions. For this purpose, we used the oxygen-isotope records of two planktonic foraminifer species Globigerinoides ruber and Globigerina bulloides which inhabit different water masses as well as faunal counts of planktonic foraminifers. After the ocean frontal systems off southern Australia were pushed northward by orbitally-forced insolation changes during the early Holocene, the data indicate increasing ENSO variability during the mid to late Holocene when the fronts shifted polewards again. A strong circa 1550 year cycle is found in the Globigerina bulloides record which reflects the wider Southern Ocean signal with prominent cold phases centred at circa 9.2, 7.3, 5.8, 4.3, 2.7, 1.4 ka BP and, possibly the Little Ice Age, which have global counterparts. STUDY NOTES: Holocene oxygen (d18O) and carbon (d13C) isotope data on foraminifera from marine sediment core MD03-2611 collected in Murray Canyon, South Australia.

GET DATA https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/moros2009/moros2009.txt NOAA Template File; Murray Canyon MD03-2611 Stable Isotope Data USA/NOAA DIF Version 9.8.4 2019-05-31 2019-05-31