Abstract

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.

Highlights

  • Coastal waters cover around 7% of the total ocean surface (26 × 106 km2) while contributing more than 50% of the economic value of the ocean’s total ecosystem services (Costanza et al, 2014; Jahnke, 2010)

  • Enhanced in coastal waters by about two orders of magnitude compared to the open ocean

  • Identi­ fying how biogeochemical processes of tropical coastal waters differ from temperate areas may further highlight that information from temperate zones is not necessarily applicable to tropical systems and could, if transferred to these systems, lead to incorrect conclusions

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Summary

Introduction

Coastal waters cover around 7% of the total ocean surface (26 × 106 km2) while contributing more than 50% of the economic value of the ocean’s total ecosystem services (Costanza et al, 2014; Jahnke, 2010). They are the most biogeochemically active zones of the ocean, having the highest per area nitrogen (N) and phosphorus (P) standing stocks, process rates and transport fluxes (influx and efflux) (Gattuso et al, 1998). Enhanced in coastal waters by about two orders of magnitude compared to the open ocean

C CaCO3 CDOM CFA DOC DON DOP DIN DNRA DSi N N2 N2O P PN PP Si SGD SRP
Major environmental differences between tropical and temperate systems
Nutrient inputs
Riverine inputs
Groundwater inputs
Lateral nutrient fluxes
Atmospheric deposition
Nitrogen fixation
Recycling
Cycling of organic nutrients
Primary production and respiration
Sedimentary nutrient burial
Findings
Denitrification and anammox
Full Text
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