Geochemistry, Geophysics, Geosystems

Journal Information
ISSN / EISSN : 15252027 / 15252027
Current Publisher: American Geophysical Union (AGU) (10.1029)
Former Publisher: Wiley (10.1002)
Total articles ≅ 4,346
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Latest articles in this journal

Jeffrey Park, Danny M. Rye
Geochemistry, Geophysics, Geosystems; doi:10.1029/2019gc008493

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Jeffrey Park, Danny M. Rye
Geochemistry, Geophysics, Geosystems; doi:10.1029/2019gc008492

The publisher has not yet granted permission to display this abstract.
B. Steinberger, P.L. Nelson, S.P. Grand, W. Wang
Geochemistry, Geophysics, Geosystems; doi:10.1029/2019gc008490

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Michael Hamilton, Paul Wessel, Joaquim Luis, Brian Taylor, Youngtak Ko
Geochemistry, Geophysics, Geosystems; doi:10.1029/2018gc007891

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Bhavik Harish Lodhia, Gareth G. Roberts, Alastair J. Fraser, Jerry Jarvis, Richard Newton, Robbie J. Cowan
Geochemistry, Geophysics, Geosystems; doi:10.1029/2019gc008262

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F. Pöppelmeier, P. Blaser, M. Gutjahr, F. Süfke, D. J. R. Thornalley, J. Grützner, K. A. Jakob, J. M. Link, S. Szidat, J. Lippold
Geochemistry, Geophysics, Geosystems; doi:10.1029/2019gc008271

Abstract:Neodymium (Nd) isotopes extracted from authigenic sediment phases are increasingly used as a proxy for past variations in water mass provenance. To better constrain the controls of water mass provenance and non‐conservative effects on the archived Nd isotope signal, we present a new depth transect of Nd isotope reconstructions from the Blake Bahama Outer Ridge along the North American continental margin covering the past 30 ka. We investigated five sediment cores that lie directly within the main flow path of the Deep Western Boundary Current, a major advection route of North Atlantic Deep Water. We found offsets between core tops and seawater Nd isotopic compositions that are observed elsewhere in the Northwest Atlantic. A possible explanation for this is the earlier suggested redistribution of sediment by nepheloid layers at intermediate as well as abyssal depths, transporting material downslope and along the continental margin. These processes potentially contributed to Nd isotope excursions recorded in Northwest Atlantic sediment cores during the Bølling‐Allerød and early Holocene. An Atlantic‐wide comparison of Nd isotope records shows that the early Holocene excursions had an additional contribution from conservative advection of unradiogenic dissolved Nd. Nevertheless, the trends of the Nd isotope records are in general agreement with previous reconstructions of water mass provenance from the entire Atlantic and also reveal millennial‐scale changes during the last deglaciation in temporal high‐resolution, which have rarely been reported before. Further, the new records confirm that during cold periods the Northwest Atlantic was bathed by an increased contribution of southern sourced water.
Detao He, Cin‐Ty A. Lee, Xun Yu, Michael Farner
Geochemistry, Geophysics, Geosystems; doi:10.1029/2019gc008514

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Yujia Liu, Hailong Lu, Xijie Yin, Livio Ruffine, M. Namik Çağatay, Hailin Yang, Chunqing Chen, Dong He, Zhenli Zhu, Burak Yalamaz
Geochemistry, Geophysics, Geosystems; doi:10.1029/2019gc008364

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M. Siegrist, G. Yogodzinski, M. Bizimis, J. Fournelle, T. Churikova, C. Dektor, R. Mobley
Geochemistry, Geophysics, Geosystems; doi:10.1029/2019gc008478

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A. Nikulin, J. R. Bourke, J. R. Domino, J. Park
Geochemistry, Geophysics, Geosystems; doi:10.1029/2019gc008491

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