Abstract

IntroductionThe Florida Everglades has undergone significant ecological change spanning the continuum of disturbance to restoration. While the restoration effort is not complete and the ecosystem continues to experience short duration perturbations, a better understanding of long-term C dynamics of the Everglades is needed to facilitate new restoration efforts. This study evaluated temporal trends of different aquatic carbon (C) pools of the northern Everglades Protection Area over a 20-year period to gauge historic C cycling patterns. Dissolved inorganic C (DIC), dissolved organic C (DOC), particulate organic C (POC), and surface water carbon dioxide (pCO2(aq)) were investigated between May 1, 1994 and April 30, 2015.ResultsAnnual mean concentrations of DIC, DOC, POC, and pCO2(aq) significantly decreased through time or remained constant across the Water Conservation Areas (WCAs). Overall, the magnitude of the different C pools in the water column significantly differed between regions. Outgassing of CO2 was dynamic across the Everglades ranging from 420 to 2001 kg CO2 year−1. Overall, the historic trend in CO2 flux from the marsh declined across our study area while pCO2(aq) largely remained somewhat constant with the exception of Water Conservation Area 2 which experienced significant declines in pCO2(aq). Particulate OC concentrations were consistent between WCAs, but a significantly decreasing trend in annual POC concentrations was observed.ConclusionsHydrologic condition and nutrient inputs significantly influenced the balance, speciation, and flux of C pools across WCAs suggesting a subsidy-stress response in C dynamics relative to landscape scale responses in nutrient availability. The interplay between nutrient inputs and hydrologic condition exert a driving force on the balance between DIC and DOC production via the metabolism of organic matter which forms the base of the aquatic food web. Along the restoration trajectory as water quality and hydrology continues to improve, it is expected that C pools will respond accordingly.

Highlights

  • The Florida Everglades has undergone significant ecological change spanning the continuum of disturbance to restoration

  • Hydrologic condition and nutrient inputs significantly influenced the balance, speciation, and flux of C pools across Water Conservation Areas (WCAs) suggesting a subsidy-stress response in C dynamics relative to landscape scale responses in nutrient availability

  • The interplay between nutrient inputs and hydrologic condition exert a driving force on the balance between Dissolved inorganic C (DIC) and dissolved organic C (DOC) production via the metabolism of organic matter which forms the base of the aquatic food web

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Summary

Introduction

The Florida Everglades has undergone significant ecological change spanning the continuum of disturbance to restoration. Wetlands, including peatlands, are net C sinks that store a large amount of the global C created by an unbalanced accumulation of C via plant productivity and export from decomposition of organic matter via C dioxide (CO2) or methane (CH4) to the atmosphere Carbon forms such as dissolved inorganic C (DIC), particulate organic C (POC), and dissolved organic C (DOC) can be transported laterally through run-off (Updegraff et al.1995; Freeman et al 2004; Billett and Moore 2008) and contribute to wetlands’ carbon budgets. This type of export C, organic species from wetlands, represents a significant regional redistribution of terrestrial C and exerts important controls on aquatic productivity in downstream waterbodies.

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