RS
Member Since 1986
Reiner Schlitzer
Prof. Dr., Alfred Wegener Institute Helmholtz-Center for Polar and Marine Research Bremerhaven
AGU Research
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Biological Uptake, Water Mass Mixing and Scavenging Limit the Transport of Manganese‐Rich Waters From the East Antarctic Shelf
GLOBAL BIOGEOCHEMICAL CYCLES
16 august 2023
Pauline Latour, Pier van der Merwe, Kathrin Wuttig...
Manganese (Mn) is an essential element involved in photosynthesis, yet its concentrations in Southern Ocean open waters are very low, arising from ...
A Flux‐Based Threshold for Anaerobic Activity in the Ocean
GEOPHYSICAL RESEARCH LETTERS
06 march 2021
Emily Zakem, Jonathan M. Lauderdale, Reiner Schlit...
Anaerobic microbial activity in the ocean causes losses of bioavailable nitrogen and emission of nitrous oxide to the atmosphere, but its predictab...
Hydrothermal Fe flux analysis of Loihi Seamount using size partitioning and Fe isotopes
OCEAN SCIENCES 2020
chemical tracers, organic matter and trace elements | 17 february 2020
Nathan T. Lanning, Tim Conway, Jessica N. Fitzsimm...
Hydrothermal vents have gained attention as a source of dissolved iron (dFe; <0.2μm) to the ocean. Using δ3He as a conservative hydrothermal tracer...
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Late Spring Nitrate Distributions Beneath the Ice-Covered Northeastern Chukchi Shelf
JOURNAL OF GEOPHYSICAL RESEARCH: BIOGEOSCIENCES
18 september 2017
Kevin R. Arrigo, Matthew M. Mills, Gert van Dijken...
Measurements of late springtime nutrient concentrations in Arctic waters are relatively rare due to the extensive sea ice cover that makes sampling...
Net removal of major marine dissolved organic carbon fractions in the subsurface ocean
GLOBAL BIOGEOCHEMICAL CYCLES
04 february 2012
Dennis A. Hansell, Craig A. Carlson, Reiner Schlit...
Marine dissolved organic matter is a massive reservoir of carbon holding >200x the ocean biomass inventory. Primarily produced at th...