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Projekt Druckansicht

Metabolismus des Stickstoffs in der Amazonasfahne und dem westlichen, tropischen Nordatlantik (MeNARP)

Fachliche Zuordnung Physik, Chemie und Biologie des Meeres
Biochemie und Physiologie der Tiere
Ökologie und Biodiversität der Tiere und Ökosysteme, Organismische Interaktionen
Förderung Förderung von 2020 bis 2024
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 439440452
 
Erstellungsjahr 2024

Zusammenfassung der Projektergebnisse

For the first time, the nitrogen cycle of the world's largest river and adjacent coastal ocean was studied incl. the plankton community and the food web. Although a zonation along the river plume had been described before, it was for the first time detailed including nutrient uptake and primary production. We described the sediment as a reactor, low primary production and high recycling rates in the high turbidity zone leading to the export of recycled N rather than riverine nitrogen. Interestingly, primary production was strongly ammonium driven in the northern plume, where nitrogen fixation rates remained low. Combining tracer and natural abundance data of bulk and compound specific stable nitrogen isotope data allowed for the first time to directly apply a mesozooplankton community production approach. This unexpectedly allowed for both, quantifying secondary production and identifying its physiological and environmental regulation, both of which have been unreached long term goals in marine science for the longest time now. In contrast to phytoplankton, which expresses high overall production rates, mesozooplankton production was strongly regulated by phytoplankton structure and function as well as habitat heterogenity. Contrary to the expectation that significant changes in the river loads due to the drastic human influences in the catchment area would be visible at the time of the cruise, these were not detected. However, this is to be expected in the coming years. Whether factors such as deforestation, dam construction, and global warming reinforce or cancel each other out is impossible to assess. In biogeochemical models, k2 (or NGE) and TP of mesozooplankton are constants e.g. set to 0.4 and 2.0 (herbivore), which leads to exponential errors in the estimation of secondary production and ammonium regeneration by mesozooplankton in models. We suggest to use adjusted TP and NGE or k2 values for mesozooplankton depending on the dominant phytoplankton in the habitat. Mixotrophy in phytoplankton seems to be an formerly unidentified strategie for optimal nutrient drawdown in the ARP.

Projektbezogene Publikationen (Auswahl)

 
 

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