I work in Nicholas Tosca‘s group and my current DPhil research aims at providing physico-chemical constraints on different growth morphologies of carbonate crystals. Carbonate minerals and carbonate rocks are widespread across the geological record and on the surface of Earth, comprising important elements that allow us to probe deep into Earth’s past environmental conditions. Calcite crystals, in particular, are known to occur in a variety of forms, and to complicate matters one given morphology may usually result from slightly different surface environmental processes. Thus, one important question is whether or not a given morphology can be directly interpreted as a proxy for some specific environmental condition. I am currently studying carbonate precipitation in somewhat alkaline conditions, and such solutions may also have provided the necessary conditions for the onset of life, although in higher temperatures than what is being considered in our current experiments, and across a proton gradient, to be more specific.

I’ve been working for nearly 13 years in the oil industry, where I have applied inorganic and isotopic geochemistry as chemostratigraphic tools for stratigraphic correlation, palaeoenvironment reconstruction, and diagenesis studies. In industry, I could extend my scientific interests to the search for solutions to more applied geological problems, and I also have been able to develop a wider perception of our society’s demand for natural resources and for energy. Human society does not move forward without relying so much on Earth’s resources. And this is actually a general principle for all life, in such a way that this idea is connected with the broader underlying concepts regarding the onset of life itself.

I developed my background in geochemistry, environmental sciences, geology and palaeoclimate. My MSc in Earth Sciences (Geochemistry) focused on tracing the origin and distribution of some classes of persistent organic pollutants (POPs) in an estuarine environment in southern Brazil, among them polycyclic aromatic hydrocarbons (PAHs) and some organochlorine compounds. I also did experimental work on the sorption behaviour of selected heavy metals as they derived from the use of fertilisers applied to tropical soils (my BSc concluding study).

I am keen to promote discussions on any of these topics and to engage in scientific outreach for the public. For this latter purpose I created my blog a few years ago (in Portuguese), where I’ve tried to raise awareness on issues concerning science and education for the Brazilian community.

  • Pietzsch, R., Martins, D.O., Tedeschi, L.R., Queiroz Neto, J.V., Figueiredo, M.F., Vazquez, J.C., Souza, R.S. 2018. Palaeohydrology of the Lower Cretaceous pre-salt lacustrine system, from rift to post-rift phase, based on elemental geochemistry, biostratigraphy and radiogenic strontium isotope data, Santos Basin, Brazil. Palaeogeography, Palaeoclimatology, Palaeoecology 507, 60-80. doi: 10.1016/j.palaeo.2018.06.043

 

  • Freire, A.F.M., Leite, C.M.M., Oliveira, F.M., Guimarães, M.F., Milhomem, P.S., Pietzsch, R., D’Ávila, R.S.F. 2017. Fluid escape structures as possible indicators of past gas hydrate dissociation during the deposition of the Barremian sediments in the RecôncavoBasin, NE, Brazil. Brazilian Journal of Geology 47, 79-93. doi: 10.1590/2317-4889201720160090

 

  • Pietzsch, Raphael, Patchineelam, Sambasiva R., Torres, João P.M. 2010. Polycyclic aromatic hydrocarbons in recent sediments from a subtropical estuary in Brazil. Marine Chemistry 118, 56 – 66. doi: 10.1016/j.marchem.2009.10.004

 

  • Pietzsch, R., Polivanov, H., Silva, A.S., Alamino, R.C.J., Campos, T.M.P. 2009. Study on the interaction of heavy metals on farmland in Petropolis, Rio de Janeiro, Brazil.  10.1144/EGSP22.I