Tongue of the Ocean - Sclerosponge Stable Isotope Data Swart, P.K.; Torrold, S.; Esienhauer, A.; Rosenheim, B.; Harrison, C.G.A.; Grammer, M.; Latkoczy, C. Swart, P.K. Torrold, S. Esienhauer, A. Rosenheim, B. Harrison, C.G.A. Grammer, M. Latkoczy, C. earth science/paleoclimate/corals and sclerosponges (delta 13C,Ceratoporella nicholsoni,null,per mil VPDB,annual,corals and sclerosponges,averaged,isotope ratio mass spectrometry,N,null) earth science/paleoclimate/corals and sclerosponges (age,null,null,null,null,corals and sclerosponges,null,null,N,null) earth science/paleoclimate/corals and sclerosponges (delta 18O,Ceratoporella nicholsoni,null,per mil VPDB,annual,corals and sclerosponges,averaged,isotope ratio mass spectrometry,N,null) earth science/paleoclimate/corals and sclerosponges earth science/paleoclimate/corals and sclerosponges (Tongue of the Ocean>LATITUDE 23.92>LONGITUDE -76.83) This paper presents data to support the presence of (i) intra-annual signals in the chemical composition of the skeletons of sclerosponges from the Bahamas, and (ii) variable rates of skeletal accretion. These conclusions are based on data obtained by using a microsampling method for the stable oxygen and carbon isotopes in which material was extracted at a resolution of one sample every 32 mm and a laser microprobe which obtained trace element data every 20 mm (Sr, Mg, and Pb). An age model was established using a combination of U-Th dating, changes in the concentration of Pb, and the change in the d13C of the skeleton of the sclerosponges. These methods yield a mean growth rate of 220 mm/yr, but suggest that the growth rate in this particular sclerosponge was in fact not constant and varied between 100 and 400 mm/yr. The variable growth rate was confirmed through spectral analysis of the d18O and Sr/Ca data that showed peaks corresponding to the annual cycle in these parameters as well as peaks corresponding to growth rates of approximately 128, 212, 270, and 400 mm/yr. The presence of these additional frequencies suggests a growth rate between approximately 100 and 400 mm/yr. These conclusions were supported by modeling of oxygen isotopic data measured on a scleractinian coral as well as model isotope data generated on synthetic time series. These findings have important implications for the use of sclerosponges as proxies of paleoclimate, because they emphasize the need for a precise yearly chronology in order that proxy data can be compared with climatic variables such as the North Atlantic Oscillation or the Atlantic Multidecadal Oscillation. NCDC-Paleoclimatology https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce Investigator : Swart, P.K. Investigator : Torrold, S. Investigator : Esienhauer, A. Investigator : Rosenheim, B. Investigator : Harrison, C.G.A. Investigator : Grammer, M. Investigator : Latkoczy, C. 2002-07-01 ONLINE Files online, ASCII https://www.ncdc.noaa.gov/paleo/study/1887 https://www1.ncdc.noaa.gov/pub/data/paleo/coral/atlantic/bahamas-sclerosponge-2002.txt https://www1.ncdc.noaa.gov/pub/data/paleo/coral/atlantic/bahamas-sclerosponge-2002.txt English https://www.ncdc.noaa.gov/paleo/study/1887 https://www1.ncdc.noaa.gov/pub/data/paleo/coral/atlantic/bahamas-sclerosponge-2002.txt Swart, P.K., S. Torrold, A. Esienhauer, B. Rosenheim, C.G.A. Harrison, M. Grammer, and C. Latkoczy. 2002. Intra-annual variation in the stable oxygen and carbon and trace element composition of sclerosponges. Paleoceanography 17(3):1045. START YEAR: 1885 AD * END YEAR: 1992 AD -76.83 23.92 -76.83 23.92