Mareike Paul

Mareike Paul
University of Helsinki | HY · Department of Geosciences and Geography

Master of Science

About

6
Publications
1,069
Reads
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32
Citations
Citations since 2017
6 Research Items
32 Citations
201720182019202020212022202302468101214
201720182019202020212022202302468101214
201720182019202020212022202302468101214
201720182019202020212022202302468101214
Introduction
I am a PhD researcher in the Environmental Geochemistry Group lead by Tom Jilbert, at the University of Helsinki. In my PhD project, I study the use of redox-sensitive trace metals (TM) in coastal marine sediments as indicators for coastal deoxygenation. Specifically, I investigate to what extent other factors than oxygen control TM enrichments in those sediments. The project is funded by the Research Council of Finland and Onni Talas Foundation.
Additional affiliations
January 2019 - present
University of Helsinki
Position
  • PhD Student
January 2018 - December 2018
GEOMAR Helmholtz Centre for Ocean Research Kiel
Position
  • Master's Student
Description
  • Student job | Administrative support of Group Leader, Co-Organization of UDEMM Symposium 2018, RV Littorina cruise to mined areas in the Baltic Sea
June 2016 - August 2016
Dalhousie University
Position
  • Intern
Description
  • Supervisor: Prof. Dr. Markus Kienast PROMOS Scholarship (DAAD) in collaboration with University of Kiel and GEOMAR. Alkenone measurements and data analyses (Lipid extraction - GC)
Education
September 2014 - October 2018
September 2011 - August 2014
University of Hamburg
Field of study
  • Geoscience

Publications

Publications (6)
Article
Full-text available
Fjord systems are typically affected by low‐oxygen conditions, which are increasing in extent and severity, forced by ongoing global changes. Fjord sedimentary records can provide high temporal resolution archives to aid our understanding of the underlying mechanisms and impacts of current deoxygenation. However, such archives can only be interpret...
Preprint
Full-text available
Sedimentary molybdenum (Mo) and uranium (U) enrichments are often used as redox proxies to reconstruct bottom water redox changes. However, these redox proxies may not be equally reliable across a range of coastal settings due to varying depositional environments. Fjords vary greatly in their depositional conditions, due to their unique bathymetry...
Article
Full-text available
Sedimentary molybdenum (Mo) and uranium (U) enrichments are widely used to reconstruct changes in bottom water oxygen conditions in aquatic environments. Until now, most studies using Mo and U have focused on restricted suboxic-euxinic basins and continental margin oxygen minimum zones (OMZs), leaving mildly reducing and oxic (but eutrophic) coasta...
Article
Full-text available
Increasing occurrences of extreme weather events, such as the 2018 drought over northern Europe, are a concerning issue under global climate change. High-resolution archives of natural hydroclimate proxies, such as rapidly accumulating sediments containing biogenic carbonates, offer the potential to investigate the frequency and mechanisms of such...
Preprint
Full-text available
Increasing occurrences of extreme weather events, such as the 2018 drought over northern Europe, are a concerning issue under global climate change. High resolution archives of natural hydroclimate proxies, such as rapidly accumulating sediments containing biogenic carbonates, offer the potential to investigate the frequency and mechanisms of such...
Article
Full-text available
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 ∼200 and 500 m water depth. BSi burial (2,100 mmol m⁻² yr⁻¹) and recycling fluxes (3,300 mmol m⁻² yr⁻¹)...

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