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The influence of terrigenous particulate material dissolution on ocean chemistry and global element cycles
C Jeandel, EH Oelkers - Chemical Geology, 2015 - Elsevier
Land to ocean transfer of material largely controls the chemical composition of seawater and
the global element cycles. Overall this transfer is dominated by the riverine transport of …
the global element cycles. Overall this transfer is dominated by the riverine transport of …
The global biogeochemical cycle of the rare earth elements
To improve our understanding and guide future studies and applications, we review the
biogeochemistry of the rare earth elements (REE). The REEs, which form a chemically …
biogeochemistry of the rare earth elements (REE). The REEs, which form a chemically …
Neodymium in the oceans: a global database, a regional comparison and implications for palaeoceanographic research
The neodymium (Nd) isotopic composition of seawater has been used extensively to
reconstruct ocean circulation on a variety of time scales. However, dissolved neodymium …
reconstruct ocean circulation on a variety of time scales. However, dissolved neodymium …
Are clay minerals the primary control on the oceanic rare earth element budget?
The rare earth elements (REEs) are an important tool for understanding biogeochemical
cycling and sedimentary processes in the global ocean. However, ambiguities in the marine …
cycling and sedimentary processes in the global ocean. However, ambiguities in the marine …
The large-scale evolution of neodymium isotopic composition in the global modern and Holocene ocean revealed from seawater and archive data
Abstract Neodymium isotopic compositions (143 Nd/144 Nd or ε Nd) have been used as a
tracer of water masses and lithogenic inputs to the ocean. To further evaluate the …
tracer of water masses and lithogenic inputs to the ocean. To further evaluate the …
Reactivity of neodymium carriers in deep sea sediments: Implications for boundary exchange and paleoceanography
The dissolved neodymium (Nd) isotopic distribution in the deep oceans is determined by
continental weathering inputs, water mass advection, and boundary exchange between …
continental weathering inputs, water mass advection, and boundary exchange between …
Neodymium isotopes in authigenic phases, bottom waters and detrital sediments in the Gulf of Alaska and their implications for paleo-circulation reconstruction
The isotopic composition of neodymium (ε Nd) extracted from sedimentary Fe–Mn
oxyhydroxide offers potential for reconstructing paleo-circulation, but its application depends …
oxyhydroxide offers potential for reconstructing paleo-circulation, but its application depends …
Widespread lithogenic control of marine authigenic neodymium isotope records? Implications for paleoceanographic reconstructions
Our understanding of past ocean-climate dynamics is informed by multiple paleocirculation
proxies including δ 13 C, 231 Pa/230 Th, and radiogenic neodymium isotopes (ε Nd). Of …
proxies including δ 13 C, 231 Pa/230 Th, and radiogenic neodymium isotopes (ε Nd). Of …
Evolution of the Global Overturning Circulation since the Last Glacial Maximum based on marine authigenic neodymium isotopes
Abstract The Global Overturning Circulation is linked to climate change on glacial-
interglacial and multi-millennial timescales. The understanding of past climate-circulation …
interglacial and multi-millennial timescales. The understanding of past climate-circulation …
The effect of particulate dissolution on the neodymium (Nd) isotope and Rare Earth Element (REE) composition of seawater
The exchange of material between particulates and seawater along the continental margins,
a process commonly referred to as boundary exchange, is thought to play a significant role …
a process commonly referred to as boundary exchange, is thought to play a significant role …