All abstracts by Steven L. Goldstein at Goldschmidt2018
| (2018) A New Look at Crust-Mantle Differentiation
Hofmann A, Goldstein S & Class C |
| (2018) Droughts and Tropical-Induced Rainfall in the East Mediterranean during Warm Periods
Kiro Y, Goldstein SL, Kushnir Y, Stein M & Lazar B |
| (2018) Northern Hemispheric Trigger for The Mid-Pleistocene Transition
Yehudai M, Kim J, Jaume-Seguí M, Goldstein SL, Pena LD, Knudson KP & Bickert T |
| (2018) Reconstruction of the North Atlantic End-Member of the Atlantic Meridional Overturning Circulation over the Last 1.5 Myr
Kim J, Jaume-Seguí M, Yehudai M, Knudson K, Goldstein S, Pena L & Ferretti P |
| (2018) The Atlantic Meridional Overturning Circulation over Time from Nd Isotopes
Goldstein SL, Pena LD, Yehudai M, Jaume-Seguí M, Kim J, Knudson K, Basak C, Hartman AE & Lupien R |
| (2018) Cs+ Cation Exchange Wash for Marine Clay Clarifies Provenance Signal & Assesses Cation Exchange Capacity
Babin DP, Simon MH, Hemming SR, Cai MY, Liu T, Goldstein SL, Han X, Haws AA, Johns MA & Lear C |
| (2018) Inclusions in Diamonds Constrain Thermo-Chemical Conditions of the Kaapvaal Cratonic Mantle
Weiss Y, Navon O, Goldstein S & Harris J |
| (2018) The Deep Ocean Carbon System Across the Mid-Pleistocene
Haynes L, Hönisch B, Farmer J, Clementi V, Ford H, Raymo M, Goldstein S, Pena L, Yehudai M, Bickert T & Lea D |
| (2018) Is the Argentinean Loess a Primary Dust Source in the Southern Hemisphere?
Gili S, Gaiero D, Mattielli N, Torre G, Goldstein S, Chemale F & Koester E |
| (2018) Distributions of Neodymium Isotopes and Rare Earth Elements in the Southwest Atlantic Ocean
Wu Y, Goldstein S, Pena L, Anderson R, Hartman A, Bolge L, Rijkenberg M & de Baar H |
| (2018) Detrital Calcites from the Sahara: Source of Alkalinity to the Dead Sea, the Mediterranean and the Atlantic Ocean
Stein M & Goldstein S |
| (2018) New Zealand as a Potential Source of Mineral Dust to the Atmosphere and Ocean during Glacials
Koffman B, Goldstein S, Winckler G, Kaplan M, Bolge L, Cai Y, Recasens C & Koffman T |