S
Steven J. Manganini
Researcher at Woods Hole Oceanographic Institution
Publications - 50
Citations - 4965
Steven J. Manganini is an academic researcher from Woods Hole Oceanographic Institution. The author has contributed to research in topics: Sediment trap & Total organic carbon. The author has an hindex of 28, co-authored 50 publications receiving 4685 citations.
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Particulate organic carbon fluxes to the ocean interior and factors controlling the biological pump: A synthesis of global sediment trap programs since 1983
TL;DR: In this article, the authors investigated the geographic contrasts of POC export at m/b and the supply rate of ∑CO2 to the world mesopelagic water column.
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Increased particle flux to the deep ocean related to monsoons
R.R. Nair,Venugopalan Ittekkot,Steven J. Manganini,Venkitasubramani Ramaswamy,B. Haake,Egon T. Degens,B.N. Desai,Susumu Honjo +7 more
TL;DR: In this article, the authors deployed three moored arrays consisting of six time-series sediment traps at selected locations in the western, central and eastern parts of the deep northern Arabian Sea.
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Sedimentation of biogenic matter in the deep ocean
TL;DR: The major constituents of biogenic particles that settle through the water column of the ocean are carbonate tests, opaline shells, and particulate organic matter (cellular and amorphous) as mentioned in this paper.
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Export production of particles to the interior of the equatorial Pacific Ocean during the 1992 EqPac experiment
TL;DR: In this article, 24 time-series, moored sediment traps were deployed between 2/2/92 and 1/27/93 along 140°W at water depths of approximately 1200 m and 2200 m, and 700 m above the bottom.
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Biogenic barium fluxes to the deep sea: Implications for paleoproductivity reconstruction
TL;DR: In this paper, the authors show that dissolved Ba concentration is not an important factor in regulating the flux of bio-Ba to the seafloor, and instead, the high Corg/bio-Ba ratios found in the western Atlantic, the Panama Basin, the Arabian Sea, and some stations in the Nordic Seas result from the addition of refractory organic carbon from nearby continents, shelves, or slopes.