Vegetation influence on CO2 and CH4 exchange in a temperate salt marsh ecosystem

Date
2021
Journal Title
Journal ISSN
Volume Title
Publisher
University of Delaware
Abstract
Salt marshes are one of the most productive ecosystems in the world with the capacity to store large amounts of carbon per unit area, referred as Blue Carbon. This carbon can remain in the ecosystem, be emitted to the atmosphere as carbon dioxide (CO2) or methane (CH4), or laterally exported by the tidal exchange of water. The influence of vegetation on the CO2 and CH4 exchange between salt marsh ecosystems and the atmosphere is uncertain, as a response to the high temporal and spatial variability in these ecosystems. This information is needed for a better understanding of the role of salt marsh ecosystems into the global carbon cycle. In this PhD study, I aim to understand the influence of the salt marsh vegetation on the exchange of carbon between a temperate salt marsh and the atmosphere. I describe and quantify the influence of different plant phenological phases on the CO2 and CH4 exchange, as well as their influence on the Gross Primary Productivity (GPP) at the ecosystem and canopy scale (i.e., canopy photosynthesis by each dominant salt marsh species; FA). For that, I use proximal canopy sensing (PCS; PhenoCam, hyperspectral reflectance data and spectral vegetation indices) to measure and monitor the temporal and spatial variability of the exchange of carbon. This study was performed on the East Coast of the United States, within the Mid-Atlantic in the State of Delaware. The study site is a temperate tidal salt marsh dominated by grasses (i.e., Spartina alterniflora and S. cynosuroides). My main results show that contrasting biophysical factors influence Net Ecosystem Exchange (NEE) of CO2 and CH4 exchange across the diel cycle and plant phenological phases (i.e., Greenup, Maturity, Senescence, Dormancy). I find that plant phenological phases have a substantial influence on the exchange of carbon, being Senescence and Dormancy the phases where this salt marsh ecosystem is emitting more CO2 and CH4 to the atmosphere. (Chapter 2). My results show that plant phenological phases also have an influence on the daily GPP variability, and that PCS is also able to model and predict this variability across the annual cycle and during the beginning of the growing season, but challenges remain for the rest of the plant phenological phases, as a response to changes in the salt marsh vegetation and exposition of soils. I find that vegetation indices used to explain changes in the chlorophyll/carotenoid ratio were more useful to model GPP variability, in contrast to some indices used to explain changes on the greenness condition of the vegetation. My results also show that the use of hyperspectral data from the visible and infrared sregion (VIS-IR) coupled with the partial least square regression (PLSR) approach, is more useful to model and predict daily GPP than specific areas of the electromagnetic region such as the Sun Induced Fluorescence (SIF), red edge (RedEdge) and infrared (IR) (Chapter 3). I find that the spatial heterogeneity in salt marshes influences the relationship between canopy photosynthesis (FA) and leaf nutrients for the most dominant species of vegetation. Nitrogen leaf nutrient (N) has an influence on the FA of S. cynosuroides but not on the FA of S. alterniflora, as a response of the availability of vegetation to uptake this nutrient from soils under lower redox conditions. Leaf nutrients such as phosphorus (P), potassium (K) and sodium (Na) are related with FA for the most dominant salt marsh species in this ecosystem. My results show the promising application of hyperspectral PCS and PLSR approach for linking information of leaf nutrients with FA in canopy salt marshes (Chapter 4). My PhD results are useful to better understand and monitor the carbon cycle in temperate salt marshes, to reduce the uncertainty on the carbon exchanged within the atmosphere and to improve estimations and models of blue carbon in coastal wetlands.
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Keywords
Blue carbon, CO2, CH4, Gross primary productivity, Hyperspectral, Leaf nutrients, Salt marshes
Citation