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Nutrient cycling in tropical and temperate coastal waters: Is latitude making a difference?
Journal article   Open access   Peer reviewed

Nutrient cycling in tropical and temperate coastal waters: Is latitude making a difference?

Christian Lønborg, Moritz Müller, Edward C.V Butler, Shan Jiang, Seng Keat Ooi, Dieu Huong Trinh, Pui Yee Wong, Suryati M Ali, Chun Cui, Wee Boon Siong, …
Estuarine, Coastal and Shelf Science, Vol.262, pp.1-17
05/11/2021
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Published (Version of record)CC BY V4.0 Open Access
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Abstract

Biogeochemical processes Coastal waters Nitrogen and phosphorus cycling Tropical and temperate
Tropical coastal waters are highly dynamic and amongst the most biogeochemically active zones in the ocean. This review compares nitrogen (N) and phosphorus (P) cycles in temperate and tropical coastal waters. We review the literature to identify major similarities and differences between these two regions, specifically with regards to the impact of environmental factors (temperature, sunlight), riverine inputs, groundwater, lateral fluxes, atmospheric deposition, nitrogen fixation, organic nutrient cycling, primary production, respiration, sedimentary burial, denitrification and anammox. Overall, there are some similarities but also key differences in nutrient cycling, with differences relating mainly to temperature, sunlight, and precipitation amounts and patterns. We conclude that due to the differences in biogeochemical processes, we cannot directly apply cause and effect relationships and models from temperate systems in tropical coastal waters. Our review also highlights the considerable gaps in knowledge of the biogeochemical processes of tropical coastal waters compared with temperate systems. Given the ecological and societal importance of tropical coastal waters, we hope that highlighting the differences and similarities to temperate systems as well as the existing gaps, will inspire further studies on their biogeochemical processes. Such knowledge will be essential to better understand and forecast impacts on tropical coastal nutrient cycling at local, regional, and global scales. •Temperature, sunlight, and precipitation drive differences in nutrient cycling between temperate and tropical systems.•Key differences include patterns of river input fluxes, nitrogen cycling processes, and organic nutrient cycling.•Therefore, models developed in temperate zones are not always transferable to the tropics.

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