11,599 Works

(Table S1) U-series ages of corals from the North Atlantic

Tina van de Flierdt, Laura F Robinson, Jess Adkins, Sidney R Hemming & Steven L Goldstein

(Table 2) Tie points and sedimentation rates of sediment core MD04-2829

Ian R Hall, Elena Colmenero-Hidalgo, Rainer Zahn, Victoria L Peck & Sidney R Hemming
AGE [ka BP] is the GISP 2 cal ka BP.

(Table S01) Carbonate content of sediment core RC11-84

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table 1) Age determination of sediment core MD04-2829

Ian R Hall, Elena Colmenero-Hidalgo, Rainer Zahn, Victoria L Peck & Sidney R Hemming

(Table S2) Nd isotope ratios for corals from the North Atlantic

Tina van de Flierdt, Laura F Robinson, Jess Adkins, Sidney R Hemming & Steven L Goldstein

(Table S03) Magnetic susceptibility for sediment core RC11-86

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table S02) Magnetic susceptibility for sediment core RC11-84

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table S06) Magnetic susceptibility for sediment core V14-65

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table S07) Magnetic susceptibility for sediment core V18-184

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table S05) Magnetic susceptibility for sediment core RC17-69

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table S04) Magnetic susceptibility for sediment core RC11-87

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table TS07) Lithic grains of sediment core RC11-87

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table TS10) Age model tie points for sediment core V14-65

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table TS09) Carbonate content of sediment core RC17-55

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table TS11) Carbonate content of sediment core V19-225

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table TS08) Carbonate content of sediment core RC17-55

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table S3) Diatom species counts of IODP Hole 318-U1361A

Carys P Cook, Tina van de Flierdt, Trevor Williams, Sidney R Hemming, Masao Iwai, Munemasa Kobayashi, Francisco J Jiménez-Espejo, Carlota Escutia, Jhon Jairo Gonzàlez, Boo-Keun Khim, Robert M McKay, Sandra Passchier, Steven M Bohaty, Christina R Riesselman, Lisa Tauxe, Saiko Sugisaki, Alberto Lopez Galindo, Molly O Patterson, Francesca Sangiorgi, Elizabeth L Pierce, Henk Brinkhuis, Adam Klaus, Annick Fehr, James A Bendle, Peter K Bijl … & Masako Yamane
DEPTH, sediment/rock [m] is given in mbsf.

Neodymium isotope signature of Holocene corals, supplement to: van de Flierdt, Tina; Robinson, Laura F; Adkins, Jess; Hemming, Sidney R; Goldstein, Steven L (2006): Temporal stability of the neodymium isotope signature of the Holocene to glacial North Atlantic. Paleoceanography, 21, PA4102

Tina van de Flierdt, Laura F Robinson, Jess Adkins, Sidney R Hemming & Steven L Goldstein
The neodymium isotopic composition of marine precipitates is increasingly recognized as a powerful tool for identifying changes in ocean circulation and mixing on million year to millennial timescales. Unlike nutrient proxies such as d13C or Cd/Ca, Nd isotopes are not thought to be altered in any significant way by biological processes, and thus they can serve as a quasi-conservative water mass tracer. However, the application of Nd isotopes in understanding the role of thermohaline circulation...

(Table S1) Neodymium and strontium isotope composition of Pliocene detrital sediments from IODP Hole 318-U1361A and additional regional core top samples

Carys P Cook, Tina van de Flierdt, Trevor Williams, Sidney R Hemming, Masao Iwai, Munemasa Kobayashi, Francisco J Jiménez-Espejo, Carlota Escutia, Jhon Jairo Gonzàlez, Boo-Keun Khim, Robert M McKay, Sandra Passchier, Steven M Bohaty, Christina R Riesselman, Lisa Tauxe, Saiko Sugisaki, Alberto Lopez Galindo, Molly O Patterson, Francesca Sangiorgi, Elizabeth L Pierce, Henk Brinkhuis, Adam Klaus, Annick Fehr, James A Bendle, Peter K Bijl … & Masako Yamane
DEPTH, sediment/rock [m] is given in mbsf. Re-analysed values represent samples that were measured multiple times (same aliquot), while duplicate samples represent full procedural repeats (e.g. from digestion, through ion exchange chromatography, to mass spectrometry).

(Table S5) Biogenic opal content of IODP Hole 318-U1361A

Carys P Cook, Tina van de Flierdt, Trevor Williams, Sidney R Hemming, Masao Iwai, Munemasa Kobayashi, Francisco J Jiménez-Espejo, Carlota Escutia, Jhon Jairo Gonzàlez, Boo-Keun Khim, Robert M McKay, Sandra Passchier, Steven M Bohaty, Christina R Riesselman, Lisa Tauxe, Saiko Sugisaki, Alberto Lopez Galindo, Molly O Patterson, Francesca Sangiorgi, Elizabeth L Pierce, Henk Brinkhuis, Adam Klaus, Annick Fehr, James A Bendle, Peter K Bijl … & Masako Yamane
DEPTH, sediment/rock [m] is given in mbsf.

Calcium isotopes of planktonic foraminifera, supplement to: Heuser, Alexander; Eisenhauer, Anton; Böhm, Florian; Wallmann, Klaus; Gussone, Nikolaus; Pearson, Paul N; Nägler, Thomas F; Dullo, Wolf-Christian (2005): Calcium isotope (d44/40Ca) variations of Neogene planktonic foraminifera. Paleoceanography, 20(2), PA2013

Alexander Heuser, Anton Eisenhauer, Florian Böhm, Klaus Wallmann, Nikolaus Gussone, Paul N Pearson, Thomas F Nägler & Wolf-Christian Dullo
Measurements of the calcium isotopic composition (d44/40Ca) of planktonic foraminifera from the western equatorial Pacific and the Indian sector of the Southern Ocean show variations of about 0.6 per mil over the past 24 Myr. The stacked d44/40Ca record of Globigerinoides trilobus and Globigerina bulloides indicates a minimum in d44/40Casw (seawater calcium) at 15 to 16 Ma and a subsequent general increase toward the present, interrupted by a second minimum at 3 to 5 Ma....

(Table S08) Magnetic susceptibility for sediment core V19-224

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table TS 3) Measured or extrapolated ages of the core top, the depth of the 20 ka (LGM) horizon, and the average sedimentation rate between them for sediment cores from the Agulhas current

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

(Table TS05) Measured or extrapolated ages of core tops older than 5000 years of sediment cores from the Agulhas current

Allison M Franzese, Sidney R Hemming & Steven L Goldstein

Strontium isotopes, ages and carbonate content of sediments from the Agulhas Current, supplement to: Franzese, Allison M; Hemming, Sidney R; Goldstein, Steven L (2009): Use of strontium isotopes in detrital sediments to constrain the glacial position of the Agulhas Retroflection. Paleoceanography, 24(2), PA2217

Allison M Franzese, Sidney R Hemming & Steven L Goldstein
The Agulhas Leakage represents a significant portion of the warm, surface return flow of the global overturning circulation and thus may be an important feedback in the ocean climate system. Models indicate that reduced leakage could be caused by a stronger Agulhas Current and/or a more upstream (eastward) Agulhas Retroflection, while a weaker Agulhas Current would result in a more westward retroflection and increased leakage. However, data for the Last Glacial Maximum support both a...

Registration Year

  • 2014
    11,599

Resource Types

  • Dataset
    11,146
  • Collection
    453