Component-specific dynamics of riverine mangrove CO2 efflux in the Florida coastal Everglades

被引:36
|
作者
Troxler, Tiffany G. [1 ]
Barr, Jordan G. [2 ]
Fuentes, Jose D. [3 ]
Engel, Victor [4 ]
Anderson, Gordon [4 ]
Sanchez, Christopher [5 ]
Lagomasino, David [6 ]
Price, Rene [7 ,8 ]
Davis, Stephen E. [9 ]
机构
[1] Florida Int Univ, Southeast Environm Res Ctr, Miami, FL 33199 USA
[2] Everglades Natl Pk, South Florida Nat Res Ctr, Homestead, FL 33034 USA
[3] Penn State Univ, Dept Meteorol, University Pk, PA 16802 USA
[4] US Geol Survey, Southeast Ecol Sci Ctr, Gainesville, FL 32606 USA
[5] Univ Miami, Abbess Ctr Ecosyst Sci & Policy, Coral Gables, FL 33146 USA
[6] NASA, Goddard Space Flight Ctr, Univ Space Res Assoc, Greenbelt, MD 20771 USA
[7] Florida Int Univ, Dept Earth & Environm, Miami, FL 33199 USA
[8] Florida Int Univ, Southeast Environm Res Ctr, Miami, FL 33199 USA
[9] Everglades Fdn, Palmetto Bay, FL 33157 USA
基金
美国国家科学基金会;
关键词
pCO(2); Pneumatophore; Course woody debris; Carbon; Budget; Peat; COARSE WOODY DEBRIS; ORGANIC-CARBON; SPATIAL VARIATION; SOIL RESPIRATION; GAS-EXCHANGE; WATERS; FORESTS; FLUX; ALLOCATION; DIOXIDE;
D O I
10.1016/j.agrformet.2014.12.012
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Carbon cycling in mangrove forests represents a significant portion of the coastal wetland carbon (C) budget across the latitudes of the tropics and subtropics. Previous research suggests fluctuations in tidal inundation, temperature and salinity can influence forest metabolism and C cycling. Carbon dioxide (CO2) from respiration that occurs from below the canopy is contributed from different components. In this study, we investigated variation in CO2 flux among different below-canopy components (soil, leaf litter, course woody debris, soil including pneumatophores, prop roots, and surface water) in a riverine mangrove forest of Shark River Slough estuary, Everglades National Park (Florida, USA). The range in CO2 flux from different components exceeded that measured among sites along the oligohaline-saline gradient. Black mangrove (Avicennia germinans) pneumatophores contributed the largest average CO2 flux. Over a narrow range of estuarine salinity (25-35 practical salinity units (PSU)), increased salinity resulted in lower CO2 flux to the atmosphere. Tidal inundation reduced soil CO2 flux overall but increased the partial pressure of CO2 (pCO(2)) observed in the overlying surface water upon flooding. Higher pCO(2) in surface water is then subject to tidally driven export, largely as HCO3. Integration and scaling of CO2 flux rates to forest scale allowed for improved understanding of the relative contribution of different below-canopy components to mangrove forest ecosystem respiration (ER). Summing component CO2 fluxes suggests a more significant contribution of below-canopy respiration to ER than previously considered. An understanding of below-canopy CO2 component fluxes and their contributions to ER can help to elucidate how C cycling will change with discrete disturbance events (e.g., hurricanes) and long-term change, including sea-level rise, and potential impact mangrove forests. As such, key controls on below-canopy ER must be taken into consideration when developing and modeling mangrove forest C budgets. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:273 / 282
页数:10
相关论文
共 50 条
  • [1] Flux of organic carbon in a riverine mangrove wetland in the Florida Coastal Everglades
    Romigh, Melissa M.
    Davis, Stephen E., III
    Rivera-Monroy, Victor H.
    Twilley, Robert R.
    HYDROBIOLOGIA, 2006, 569 (1) : 505 - 516
  • [2] Flux of organic carbon in a riverine mangrove wetland in the Florida Coastal Everglades
    Melissa M. Romigh
    Stephen E. Davis
    Victor H. Rivera-Monroy
    Robert R. Twilley
    Hydrobiologia, 2006, 569 : 505 - 516
  • [3] Patterns of Root Dynamics in Mangrove Forests Along Environmental Gradients in the Florida Coastal Everglades, USA
    Castaneda-Moya, Edward
    Twilley, Robert R.
    Rivera-Monroy, Victor H.
    Marx, Brian D.
    Coronado-Molina, Carlos
    Ewe, Sharon M. L.
    ECOSYSTEMS, 2011, 14 (07) : 1178 - 1195
  • [4] Patterns of Root Dynamics in Mangrove Forests Along Environmental Gradients in the Florida Coastal Everglades, USA
    Edward Castañeda-Moya
    Robert R. Twilley
    Victor H. Rivera-Monroy
    Brian D. Marx
    Carlos Coronado-Molina
    Sharon M. L. Ewe
    Ecosystems, 2011, 14 : 1178 - 1195
  • [5] Hurricane disturbance and recovery of energy balance, CO2 fluxes and canopy structure in a mangrove forest of the Florida Everglades
    Barr, Jordan G.
    Engel, Vic
    Smith, Thomas J.
    Fuentes, Jose D.
    AGRICULTURAL AND FOREST METEOROLOGY, 2012, 153 : 54 - 66
  • [6] CO2 Efflux from Cleared Mangrove Peat
    Lovelock, Catherine E.
    Ruess, Roger W.
    Feller, Ilka C.
    PLOS ONE, 2011, 6 (06):
  • [7] Seasonal differences in the CO2 exchange of a short-hydroperiod Florida Everglades marsh
    Schedlbauer, Jessica L.
    Oberbauer, Steven F.
    Starr, Gregory
    Jimenez, Kristine L.
    AGRICULTURAL AND FOREST METEOROLOGY, 2010, 150 (7-8) : 994 - 1006
  • [8] Seasonal and temporal CO2 dynamics in three tropical mangrove creeks - A revision of global mangrove CO2 emissions
    Rosentreter, Judith A.
    Maher, D. T.
    Erler, D. V.
    Murray, R.
    Eyre, B. D.
    GEOCHIMICA ET COSMOCHIMICA ACTA, 2018, 222 : 729 - 745
  • [9] Sediment properties and CO2 efflux from intact and cleared temperate mangrove forests
    Bulmer, R. H.
    Lundquist, C. J.
    Schwendenmann, L.
    BIOGEOSCIENCES, 2015, 12 (20) : 6169 - 6180
  • [10] Soil CO2 efflux and its spatial variation in a Florida slash pine plantation
    Fang, C
    Moncrieff, JB
    Gholz, HL
    Clark, KL
    PLANT AND SOIL, 1998, 205 (02) : 135 - 146