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J. K. Klar

Researcher at University of Toulouse

Publications -  15
Citations -  768

J. K. Klar is an academic researcher from University of Toulouse. The author has contributed to research in topics: Authigenic & Mixed layer. The author has an hindex of 11, co-authored 15 publications receiving 599 citations. Previous affiliations of J. K. Klar include National Oceanography Centre, Southampton & National Oceanography Centre.

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The GEOTRACES Intermediate Data Product 2017

Reiner Schlitzer, +313 more
- 20 Aug 2018 - 
TL;DR: The GEOTRACES Intermediate Data Product 2017 (IDP2017) as discussed by the authors is the second publicly available data product of the international GEOTrACES programme, and contains data measured and quality controlled before the end of 2016.
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Natural iron fertilization by the Eyjafjallajökull volcanic eruption

TL;DR: Aerosol deposition from the 2010 eruption of the Icelandic volcano Eyjafjallajokull resulted in significant dissolved iron (DFe) inputs to the Iceland Basin of the North Atlantic as mentioned in this paper.
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Seasonal ITCZ migration dynamically controls the location of the (sub)tropical Atlantic biogeochemical divide

TL;DR: It is demonstrated that wet deposition in the region of the intertropical convergence zone acts as the major dissolved iron source to surface waters and that the underlying biogeochemical mechanisms would likely characterize the response of oligotrophic systems to altered environmental forcing over longer timescales.
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Stability of dissolved and soluble Fe(II) in shelf sediment pore waters and release to an oxic water column.

TL;DR: Modelling indicates significant diffusive fluxes of Fe(II) (on the order of 23–31 µmol m−2 day−1) are possible during late spring when oxygen penetration depths are shallow, and pore water Fe(I) concentrations are highest, and oxic continental shelves can supply dFe to the water column.
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Behaviour of chromium isotopes in the eastern sub-tropical Atlantic Oxygen Minimum Zone

TL;DR: In this article, the authors presented dissolved chromium (CrT) concentrations for shelf, slope and open ocean waters within the oxygen minimum zone (OMZ) of the eastern sub-tropical Atlantic Ocean.