about
Iron stable isotopes track pelagic iron cycling during a subtropical phytoplankton bloom.Return of naturally sourced Pb to Atlantic surface waters.Coastal ocean and shelf-sea biogeochemical cycling of trace elements and isotopes: lessons learned from GEOTRACES.Determination of Mn, Fe, Co, Ni, Cu, Zn, Cd and Pb in seawater using high resolution magnetic sector inductively coupled mass spectrometry (HR-ICP-MS).Investigation of iron(III) reduction and trace metal interferences in the determination of dissolved iron in seawater using flow injection with luminol chemiluminescence detection.The Role of External Inputs and Internal Cycling in Shaping the Global Ocean Cobalt Distribution: Insights From the First Cobalt Biogeochemical Model.The GEOTRACES Intermediate Data Product 2017Iron limits primary productivity during spring bloom development in the central North AtlanticParticulate phases are key in controlling dissolved iron concentrations in the (sub)tropical North AtlanticUncertainty contributions to the measurement of dissolved Co, Fe, Pb and V in seawater using flow injection with solid phase preconcentration and detection by collision/reaction cell—quadrupole ICP–MSThe interplay between regeneration and scavenging fluxes drives ocean iron cyclingIncreasing picocyanobacteria success in shelf waters contributes to long-term food web degradation
P50
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P50
description
hulumtuese
@sq
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Angela Milne
@ast
Angela Milne
@en
Angela Milne
@es
Angela Milne
@nl
type
label
Angela Milne
@ast
Angela Milne
@en
Angela Milne
@es
Angela Milne
@nl
altLabel
A Milne
@en
prefLabel
Angela Milne
@ast
Angela Milne
@en
Angela Milne
@es
Angela Milne
@nl
P1053
O-2786-2016
P106
P1153
23482403500
P21
P31
P3829
P496
0000-0002-3304-8962