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Iron (Fe) speciation in marine sediments and suspended particulate matter (SPM) are widely used to investigate the role of Fe minerals in marine biogeochemical cycling and to reconstruct paleo-redox conditions. A traditional method for the determinat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bc2f1215ce2ca7d4d5a51748b85df722
https://doi.org/10.1016/j.marchem.2023.104249
https://doi.org/10.1016/j.marchem.2023.104249
Autor:
Anna Plass, Christian Schlosser, Stefan Sommer, Andrew W. Dale, Eric P. Achterberg, Florian Scholz
Publikováno v:
Biogeosciences, Vol 17, Pp 3685-3704 (2020)
Sediments in oxygen-depleted marine environments can be an important sink or source of bio-essential trace metals in the ocean. However, the key mechanisms controlling the release from or burial of trace metals in sediments are not exactly understood
Marine sediments are an important source and sink of bio-essential trace metals to the ocean. However, the different mechanisms leading to trace metal release or burial are not fully understood and the associated fluxes are not well quantified. Here,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7e764073c4d577a09207155fa9a8c781
https://doi.org/10.1016/j.marchem.2021.103982
https://doi.org/10.1016/j.marchem.2021.103982
Autor:
Sonja Geilert, Florian Scholz, Ulrike Schroller-Lomnitz, David Clemens, Anna Plass, Patricia Grasse, Stefan Sommer, Klaus Wallmann, Christian Hensen, Volker Liebetrau, Andrew W. Dale, K. M. Paul
Publikováno v:
Global Biogeochemical Cycles. 35
An extensive data set of biogenic silica (BSi) fluxes is presented for the Peruvian oxygen minimum zone (OMZ) at 11°S and 12°S. Each transect extends from the shelf to the upper slope (∼1,000 m) and dissects the permanently anoxic waters between
Autor:
Rebekah C. White, Anna Plassart
Publikováno v:
i-Perception, Vol 6 (2015)
In stimulus-parity synaesthesia, a range of stimuli—for example, letters, numbers, weekdays, months, and colours (the inducers)—elicit an automatic feeling of oddness or evenness (the concurrent). This phenomenon was first described by Théodore
Externí odkaz:
https://doaj.org/article/f69619d775de4ae6b4a449f343f73d76