If you want to know more, please, visit the GEA Home Page and the projects page. So, if you have suggestions about the site, comments or other, please, contact me. I have met wonderful people and learnt a lot from all of them. I adore soccer and NBA basketball, and I practise aquagym, ski and badminton. And finally, I enjoy cooking for myself and specially for my family and friends.
P is the limiting nutrient to oceanic productivity on geological time scales.
At the same time, the P distribution in the marine sediments is not so simple, due to the interaction between P, organic matter and Fe-Mn hydroxydes. Phosphate, specially the reactive phase of P, available for biological uptake, is the link between the P and the C cycle. So, by looking deeply into the P cycle and the different phases of P present in the oceanic sediments, it is possible to have a better constraint on continental weathering, nutrients cycles, climate changes and the connection and possible feedback mechanisms taking place among them. To get more information about the group or the project I am working on, visit the GEA Home Page and feel free to contact me.