noaa-ocean-17176 Subtropical North Atlantic Oxygen Isotope Data Spanning Marine Isotope Stages 6 thru 8 Billups, K.; Scheinwald, A. Subtropical North Atlantic Oxygen Isotope Data Spanning Marine Isotope Stages 6 thru 8 2014-09-09 NCDC-Paleoclimatology ONLINE Files Pending https://www.ncdc.noaa.gov/paleo/study/17176 Investigator K. Billups Investigator A. Scheinwald earth science paleoclimate paleoceanography depth,null,null,meter,null,paleoceanography,composited,null,N,null earth science paleoclimate paleoceanography notes,null,null,null,null,paleoceanography,null,null,C,null earth science paleoclimate paleoceanography age,null,null,calendar kiloyear before present,null,paleoceanography,null,null,N,null earth science paleoclimate paleoceanography age,null,null,calendar kiloyear before present,null,paleoceanography,null,null,N,from Gruetzner et al (2002) earth science paleoclimate paleoceanography delta 18O,Globigerinoides ruber white,null,per mil VPDB,null,paleoceanography,null,null,N,null earth science paleoclimate paleoceanography delta 18O,Globigerinoides ruber white,null,per mil VPDB,null,paleoceanography,corrected,null,N,minus 0.4 per mil earth science paleoclimate paleocean oxygen isotopes geoscientificInformation 281537 cal yr BP 130050 cal yr BP Complete 31.683333 31.683333 -75.416667 -75.416667 -2985 -2985 Ocean Atlantic Ocean North Atlantic Ocean ODP 1059>LATITUDE 31.683333>LONGITUDE -75.416667 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 Billups, K. and A. Scheinwald 2014 Paleoceanography 29 612-627 10.1002/2014PA002641

We present a high-resolution planktonic foraminiferal stable isotope record (Globigerinoides ruber) spanning marine oxygen isotope stages (MISs) 6 through 8 in the northwestern subtropical Atlantic Ocean (Ocean Drilling Program Leg 172 Site 1059). The record fills a gap to produce an about 1.3?Myr long continuous time series of high-frequency (> ~1/12?kyr) surface ocean hydrography, the first of this kind. We test the hypothesis that the suborbital climate signals (i.e., half and quarter precession cycles) are linked to precession forcing in tropical latitudes. Semiprecession cycles present between 0 and 320?ka are of the right periodicity to relate to the dominant precession forcing (23?kyr). These cycles are evident as double peaks within the given precession framework, and there is good match in the amplitude modulation of the filter output and the d18O time series. Quarter precession cycles dominate the suborbital spectra between 320?ka and 1.3?Ma. Periodicities are close to those expected from the harmonics of the dominant precession peaks in the d18O record, but present in the time series only intermittently, and their amplitude modulation does not match that of the primary precession period. Thus, only the half precession cycles evidence a response to low-latitude insolation such as that introduced by insolation maxima at the equinoxes or solstices during the course of a precession cycle. Additionally, we find well-defined, rapid (~1.5–2?kyr) variations across the first of the interglacial maxima of MIS 7 adding to evidence of non–ice sheet-related forcing factors in driving climate instabilities. STUDY NOTES: G. ruber white d18O data spanning marine isotope stages 6 through 8 (~130-280 Ka). Provided keywords: Pleistocene, millennial-scale, oxygen isotopes, planktic foraminifera.

GET DATA https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/billups2014/billups2014-odp1059.txt Formatted Text File; ODP1059 d18O Data USA/NOAA DIF Version 9.8.4 2018-12-11 2018-12-11