Across the globe, species distributions are changing in response to climate change and land use change. In parts of the southeastern United States, climate change is expected to result in the poleward range expansion of black mangroves (Avicennia germinans) at the expense of some salt marsh vegetation. The morphology of A. germinans at its northern range limit is more shrub-like than in tropical climes in part due to the aboveground structural damage and vigorous multi-stem regrowth triggered by extreme winter temperatures. In this study, we developed aboveground allometric equations for freeze-affected black mangroves which can be used to quantify: (1) total aboveground biomass; (2) leaf biomass; (3) stem plus branch biomass; and (4) leaf area. Plant volume (i.e., a combination of crown area and plant height) was selected as the optimal predictor of the four response variables. We expect that our simple measurements and equations can be adapted for use in other mangrove ecosystems located in abiotic settings that result in mangrove individuals with dwarf or shrub-like morphologies including oligotrophic and arid environments. Many important ecological functions and services are affected by changes in coastal wetland plant community structure and productivity including carbon storage, nutrient cycling, coastal protection, recreation, fish and avian habitat, and ecosystem response to sea level rise and extreme climatic events. Coastal scientists in the southeastern United States can use the identified allometric equations, in combination with easily obtained and non-destructive plant volume measurements, to better quantify and monitor ecological change within the dynamic, climate sensitive, and highly-productive mangrove-marsh ecotone.
Citation: Osland MJ, Day RH, Larriviere JC, From AS (2014) Aboveground Allometric Models for Freeze-Affected Black Mangroves (Avicennia germinans): Equations for a Climate Sensitive Mangrove-Marsh Ecotone. PLoS ONE 9(6): e99604. https://doi.org/10.1371/journal.pone.0099604
Editor: Ben Bond-Lamberty, DOE Pacific Northwest National Laboratory, United States of America
Received: February 28, 2014; Accepted: May 15, 2014; Published: June 27, 2014
This is an open-access article, free of all copyright, and may be freely reproduced, distributed, transmitted, modified, built upon, or otherwise used by anyone for any lawful purpose. The work is made available under the Creative Commons CC0 public domain dedication.
Funding: This project was supported by the Department of Interior Southeast Climate Science Center (doi.gov/csc/southeast/index.cfm). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: JCL & ASF are employees of Fiver Rivers Services, LLC, who provide technical support via a contract with the USGS. Via this contract with the USGS, Five Rivers Services personnel “provide technical support in the following areas: biological, ecological, and hydrologic research; environmental chemistry; geography; river studies; geographic information systems and spatial analysis; information technology, and administrative services.” More information about Five Rivers Services and this contract with USGS can be found at this link: http://www.fiveriversservices.com/2011/04/26/five-rivers-services-awarded-us-geological-survey-contract/. There are no patents, products in development or marketed products to declare. This does not alter the authors' adherence to all the PLOS ONE policies on sharing data and materials.
In response to climate change and land use change, species distributions are changing across the globe –. Some of these distributional changes are resulting in comparatively large ecological transformations, especially where traditional ecosystem boundaries (i.e., ecotones) are migrating –. In areas with shifting ecotones, ecologists and environmental managers seek information that will enable them to better understand the ecological implications of ecosystem transformations.
In coastal wetland ecosystems, abrupt ecotones are common and occur across multiple abiotic gradients (e.g., inundation, salinity, and macroclimatic gradients) –. Since tidal wetland ecotones involve foundation plant species, sensu –, with divergent growth forms and functionality (e.g., graminoid plants, microbial mats, succulent plants, and woody mangrove plants), the ecological implications of shifting ecotones in coastal wetlands can be substantial.
In the southeastern United States and other tropical-to-temperate climatic transition zones, the mangrove-salt marsh ecotone is dynamic, visually striking, and highly productive , . Mangroves are woody foundation plant species that are sensitive to extreme winter temperatures and dominant in warmer climates , . In contrast, salt marsh graminoids and salt marsh succulent plant foundation species are dominant in cooler coastal reaches ,  where extreme winter temperature events lead to mangrove mortality and/or limit mangrove forest development, reproduction, and dispersal , , . At the poleward mangrove-marsh ecotone, mangrove abundance and coverage is winter temperature-sensitive in that it increases and decreases in response to the absence or presence of extreme winter events, respectively –. In response to changing climatic conditions, a decrease in the frequency, duration, and/or intensity of extreme winter temperatures is expected which would facilitate poleward mangrove range expansion at the expense of salt marsh vegetation . In the southeastern U.S., the northward expansion of mangroves is expected to occur in Texas, Louisiana, and parts of Florida.
The ecological implications of mangrove expansion are poorly understood. Mangroves and salt marsh ecosystems provide many important ecosystem goods and services including fish and wildlife habitat, carbon storage, nutrient and sediment retention, coastal protection, and maintenance of coastal food webs and fisheries . Although salt marsh and mangrove forest ecosystems are both highly valuable and have many ecosystem goods and services in common, there are structural and functional differences between these two ecosystems as well as differences in the provision of some ecosystem goods and services. Like many other ecotones, structural and functional complexity is higher at the mangrove-marsh ecotone than in adjacent graminoid or mangrove-dominated ecosystems. As a result, it is likely that ecological resilience and the supply of some ecosystem goods and services within the mangrove-marsh ecotone is equivalent to or even greater than in adjacent marsh or mangrove-dominated areas. However, our understanding of the ecosystem goods and services that would be affected by mangrove expansion and replacement of salt marsh is limited, and coastal wetland ecologists seek information and tools that will enable them to better quantify ecological changes associated with mangrove expansion at the expense of salt marshes –. Here, we provide equations that can be used to quantify changes in important aspects of aboveground mangrove structure near and within the dynamic mangrove-marsh ecotone.
Aboveground biomass is an important and fundamental metric for quantifying change in coastal wetland ecosystems. Many important coastal wetland ecological functions and services are affected by changes in aboveground biomass, structure, and productivity, including resilience to sea level rise –, carbon storage , –, coastal protection , , , recreation, and fish and avian habitat , . Allometric equations provide an approach for estimating plant biomass and structural attributes via easily-obtained and non-destructive measurements. Most allometric models for determining mangrove aboveground biomass have been developed in tropical climates in the absence of extreme freeze events . Within the freeze-dependent mangrove-marsh ecotone, traditional metrics for quantifying mangrove forest aboveground biomass are not appropriate because the morphology and architecture of freeze-affected mangrove trees is different than tropical mangrove trees. In the absence of freeze events and where freshwater and nutrient resources are abundant, tropical mangrove plants can develop into comparatively tall and straight trees. In contrast, at the poleward range limit of mangroves, severe freeze events can either lead to total mangrove mortality or cause aboveground structural damage that is followed by vigorous basal resprouting (Figure 1). As a result, mangroves in freeze-prone areas are often shorter, wider, multi-stemmed, and more shrub-like relative to their tropical counterparts growing in resource-rich environments, but see . Tree-focused allometric models for quantifying aboveground biomass (i.e., dbh and/or height-based models) , – are not suitable for freeze-affected and shrubby mangrove individuals.
The upper two photos show the shrub-like morphology. The middle left photo shows the size of the smallest individuals included in the analyses. The middle right photo shows leaf damage from an extreme winter temperature event in January, 2014. The lower two photos show the high stem density of freeze-affected individuals.
Our objective was to develop aboveground allometric models for freeze-affected black mangroves (Avicennia germinans). In the southeastern United States, A. germinans is the most cold-tolerant mangrove species and the most abundant mangrove species at the northern range limit of mangrove forests. Based upon studies from other shrub-dominated ecosystems – and models for stunted mangroves in New Zealand , southern Florida (USA) , , and Iran , we expected that crown area and height measurements could be used to develop allometric models for quantifying total aboveground biomass, leaf area, and leaf biomass for freeze-stunted A. germinans individuals.
Materials and Methods
Allometric equations were developed using mangroves from two tidal wetland sites near Port Fourchon, Louisiana (USA; 29°8′52″N, −90°14′38″W and 29°6′58″N, −90°11′26″W′; Figure 2), which is within the Mississippi River Deltaic Plain. Tidal wetlands in this area are abundant and dominated primarily by Spartina alterniflora (smooth cordgrass) and/or A. germinans. For more information about the study area, see , , –. Port Fourchon is near the northern limit of A. germinans along the Gulf of Mexico coast and is periodically exposed to extreme winter events that can damage or kill A. germinans (see photos in Figure 1), reducing areal coverage and limiting structural development. Historical accounts of A. germinans in the region document freeze-induced mortality during the 1960's  and 1980's . The aerial extent and abundance of A. germinans has expanded and contracted in response to extreme winter events , , , . Although most of the A. germinans stands in the Port Fourchon vicinity were less than 3 m in height at the time of this study, some individuals were between 4.5 and 5 m in height and some stands were in the 3–4 m height range (RHD and MJO, personal observation). This study was conducted, with permission, on private lands owned by The Louisiana Land and Exploration Company LLC (LL&E) and managed by the Conoco Phillips Company/LL&E office in Houma, Louisiana.
In February and May 2013, we selected a total of 56 A. germinans individuals for allometric equation development. We selected 40 individuals in February and 16 individuals in May. For each individual, we measured the height and the basal diameter at 30 cm above the soil surface. We also measured crown diameter in two perpendicular directions, across the widest crown section (CD1) and at the widest section perpendicular to the first section (CD2). The two crown diameter measurements were used to calculate crown area via the equation for an ellipse: crown area = [(CD1)/2)*(CD2)/2)]*π. When an individual had multiple stems, height was measured only on the tallest stem and basal diameter was measured only on the thickest stem. Whereas height was measured to the base of the highest leaf, crown diameter measurements were made to the edge of the most horizontally-distant leaf tips. Crown area and height were integrated into a single estimate of volume via the following equation: volume = crown area*height. Once in situ measurements were recorded, we cut each individual at the soil surface and transported the samples back to the laboratories of the U.S. Geological Survey's National Wetlands Research Center in Lafayette, Louisiana.
In the laboratory, the February and May samples were processed in a slightly different fashion since the May samples were collected explicitly for the development of leaf area and leaf biomass allometric equations. Individuals collected in February were dried to a constant mass at 60°C to determine total aboveground biomass (i.e., leaves were not separated from stems and branches prior to drying and weighing). In contrast, the May samples were separated into leaves and non-leaves (i.e., stem+branch) prior to drying, and the area of fresh leaves was determined using a Li-3000C (Licor, Inc., Lincoln, NE, USA). The separated leaf and non-leaf samples were then dried to a constant mass at 60°C to determine leaf biomass, stem+branch biomass, and total aboveground biomass. The data for this study can be found in Dataset S1.
Linear regression models were developed for the following response variables: (1) total aboveground biomass; (2) leaf biomass; (3) stem plus branch biomass; and (4) leaf area. The independent variables (i.e., crown area, height, volume, and basal diameter) were evaluated alone and in combination via simple and multiple regression analyses. Response and independent variables were natural log transformed prior to analysis. For each equation, we calculated a correction factor (CF) sensu Sprugel , where CF = exp (SEE2/2) and where SEE is the Standard Error of the Estimate. These correction factors are to be applied to the back-transformed estimates of the response variables in order to correct for a small underestimation associated with using log transformed data in the regression analyses , . For example, for an allometric equation of the form ln (y) = a+b * ln (x), y should be calculated as follows: y = CF * (exp [a+b * ln (x)]). Data analyses were conducted in SAS Version 9.3 (SAS Institute, Cary, NC, USA) and Sigma Plot Version 12.5 (Systat Software, Inc., San Jose, CA, USA).
We measured A. germinans individuals within a height range of 31–157 cm, a crown diameter range of 4–180 cm, and an aboveground biomass range of 1–2,452 g (Table 1). For the smallest plants, the measurements of crown diameter were essentially the lengths of two pairs of leaves on a single un-branched stem. In contrast, the largest plants contained multiple stems and branches extending to almost 1 m from a central base (Figure 1). We developed and compared multiple allometric equations using various combinations of predictor and response variables resulting in the selection of those shown in Table 2 and Table S1. The range limits presented in Table 1 identify boundaries for the application of the developed equations and should be used to avoid unwarranted extrapolation. Plant volume was selected as the best predictor of all of the response variables (i.e., leaf area, leaf biomass, stem plus branch biomass, and total above ground biomass) (Table 2, Figure 3, Table S1). Additional models based upon other combinations of measurements were also significant (Table S1). These additional models may be useful for researchers that want to determine biomass using alternative combinations of variables.
The short and long dashed lines show the 95% confidence and prediction bands, respectively. Note the natural log scale on both axes.
In this study, our primary objective was to develop aboveground allometric equations for freeze-affected A. germinans individuals near and within the poleward mangrove-marsh ecotone in the southeastern United States. Allometric equations enable scientists to estimate plant community structural attributes via easily-obtained and non-destructive measurements. Although aboveground allometric models have been developed for mangrove species in different abiotic settings , most of these models are for trees growing in tropical wet climates. At the poleward range limit of mangrove forests, extreme winter temperature events affect the morphology of mangrove plants and result in plants that sometimes resemble shrubs (i.e., short, wide, and multi-stemmed individuals) rather than trees. To our knowledge, our study is the first to develop allometric models for freeze-affected and shrub-like A. germinans individuals at their northern range limit.
Mangrove shrub or dwarf morphologies can result from various abiotic conditions, including drought stress, freeze stress, salinity stress, nutrient limitation, and hydrologic isolation , –. Shrub-based aboveground allometric models have been developed for some mangroves in some of these abiotic conditions. In New Zealand, near the southern latitudinal limit of mangroves and in an area with shrubby mangroves less than 1 m tall, Woodroffe  developed allometric equations that predict A. marina biomass using mean canopy width measurements. In an arid high-latitude mangrove forest in Iran, Parvaresh et al.  developed allometric equations that predict A. marina biomass from measurements of crown diameter. In a south Florida (USA) dwarf mangrove forest located in an irregularly-inundated basin setting, Ross et al.  developed allometric equations that predict A. germinans, Rhizophora mangle, and Laguncularia racemosa biomass from measurements of stem basal diameter and crown volume. In another south Florida dwarf mangrove forest, Coronado-Molina et al.  developed allometric equations that predict Rhizophora mangle biomass from measurements of height, crown diameter, and the number of prop roots. Collectively, these four studies along with our results show that crown area-focused measurements, sometimes in combination with other measurements (e.g., plant height, number of prop roots), can be used to develop allometric equations for estimating aboveground biomass of mangrove individuals with dwarf or shrub morphologies.
How do we envision that these equations will be used? In response to future changing winter temperature regimes and accelerated sea level rise, black mangroves are expected to migrate both poleward  and landward  along the northern Gulf of Mexico coast, in many cases at the expense of salt marshes, tidal freshwater systems, and/or upland forests. At many of these ecotones, ecologists will be challenged to characterize and monitor the structural changes that are already occurring or are expected to occur in the future. To the north and south of these ecotones (i.e., in salt marshes and large mangrove forests, respectively), methods for characterizing aboveground biomass and vegetation structure are well-established. Vegetation methods used in salt marshes are quite different than those used in mangrove forests. For example, whereas ground-layer measurements and vegetation samples (e.g., biomass clip plots and stem measurements from plants less than 2 m in height) are typically taken in small plots (∼1-m2) within marshes, tree-focused measurements (e.g., dbh and/or tree heights) are typically taken in large plots (∼100-m2) within tropical mangrove forests. Vegetation measurements in the freeze-affected and structurally-complex mangrove-marsh ecotone require a hybrid sampling approach that includes measurements tailored for the stunted morphology of freeze-affected mangroves (e.g., crown area and plant height measurements) as well as the multiple other vegetation strata that could be present ranging from graminoid and succulent marsh plants to large (i.e., 2–10 m tall) mangrove forest trees. See Osland et al.  for an example of the multiple plot sizes and stratum-specific measurements required to sample marshes and mangroves within a single study design. Sampling designs within mangrove-marsh ecotones often need to be customized to fit the range of plant species and morphologies present. Where conditions allow multi-stemmed shrubby mangroves to grow into large multi-stemmed trees, traditional tree-focused metrics can be applied to each individual stem contained within a tree .
Our findings and allometric equations provide a foundation for characterizing aboveground structural changes of freeze-affected black mangroves within mangrove-marsh ecotones. In combination with a robust sampling design, these equations can be used to quantify the temporal and spatial changes in plant community structure in response to the presence or lack of extreme climatic events including freeze events, drought, and hurricanes, as well as slower abiotic changes associated with sea level rise. Plant community structural information can be used to investigate the effects of ecosystem transformations and ecotone migration upon important ecosystem functions and services (e.g., sediment trapping, soil elevation change, nutrient cycling, fish and wildlife abundances, wave attenuation, carbon storage). When paired with carbon concentration data and information regarding belowground processes and soil carbon accumulation, our equations can provide a foundation for quantifying the aboveground carbon present in freeze-affected black mangrove forests which is information that can contribute to estimates of carbon sequestration and inform best practices for carbon management and climate change mitigation , . The biomass equations can also be used to evaluate plant community development and functional equivalency after wetland restoration and/or management. The leaf area equations may be incorporated into ecophysiological and/or biogeochemical models, for example , .
In summary, we developed aboveground allometric equations for freeze-affected black mangroves (A. germinans) which can be used to quantify the following: (1) total aboveground biomass; (2) leaf biomass; (3) stem plus branch biomass; and (4) leaf area. Plant volume (i.e., a combination of crown area and plant height), was selected as the optimal predictor of these response variables. Coastal wetland scientists in the southeastern United States can use these equations to better quantify and monitor ecological changes within the dynamic and climate sensitive mangrove-marsh ecotone.
Additional allometric regression equations for freeze-affected black mangrove (Avicennia germinans) individuals.
The data used to develop allometric equations for freeze-affected black mangrove (Avicennia germinans) individuals. An excel file that has two spreadsheets: (1) a data spreadsheet (spreadsheet entitled “data”); and (2) a spreadsheet that includes a description of column names and units contained within the data spreadsheet (spreadsheet entitled “legend”).
We thank Erik Yando for assistance in the field, Ken Krauss for leaf area measurement recommendations, and the ConocoPhillips Company/Louisiana Land and Exploration Company LLC for permission to conduct research on their land. The contents of the manuscript are solely the responsibility of the authors and do not necessarily represent the views of the Southeast Climate Science Center or the USGS. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
Conceived and designed the experiments: MJO RHD JCL ASF. Performed the experiments: MJO RHD JCL ASF. Analyzed the data: MJO RHD. Wrote the paper: MJO RHD JCL ASF.
- 1. Parmesan C, Yohe G (2003) A globally coherent fingerprint of climate change impacts across natural systems. Nature 421: 37–42.
- 2. Millenium Ecosystem Assessment (2005) Ecosystems and human well-being: Synthesis. Washington, D.C.: Island Press. 137 p.
- 3. Chen IC, Hill JK, Ohlemüller R, Roy DB, Thomas CD (2011) Rapid range shifts of species associated with high levels of climate warming. Science 333: 1024–1026.
- 4. Allen CD, Breshears DD (1998) Drought-induced shift of a forest–woodland ecotone: rapid landscape response to climate variation. Proceedings of the National Academy of Sciences 95: 14839–14842.
- 5. Neilson RP (1993) Transient ecotone response to climatic change: some conceptual and modelling approaches. Ecological Applications 385–395.
- 6. Risser PG (1995) The status of the science examining ecotones: A dynamic aspect of landscape is the area of steep gradients between more homogeneous vegetation associations. BioScience 45: 318–325.
- 7. Jiang J, Gao D, DeAngelis DL (2012) Towards a theory of ecotone resilience: Coastal vegetation on a salinity gradient. Theoretical Population Biology 82: 29–37.
- 8. Pennings SC, Bertness MD (2001) Salt marsh communities. In: Bertness MD, Gaines SD, Hay M, editors. Marine Community Ecology. Sunderland: Sinauer Associates. pp. 289–316.
- 9. Marani M, D'Alpaos A, Lanzoni S, Carniello L, Rinaldo A (2010) The importance of being coupled: Stable states and catastrophic shifts in tidal biomorphodynamics. Journal of Geophysical Research: Earth Surface 115: F04004.
- 10. Osland MJ, Enwright N, Day RH, Doyle TW (2013) Winter climate change and coastal wetland foundation species: salt marshes versus mangrove forests in the southeastern U.S. Global Change Biology 19: 1482–1494.
- 11. Ellison AM, Bank MS, Clinton BD, Colburn EA, Elliott K, et al. (2005) Loss of foundation species: consequences for the structure and dynamics of forested ecosystems. Frontiers in Ecology and the Environment 3: 479–486.
- 12. Angelini C, Altieri AH, Silliman BR, Bertness MD (2011) Interactions among foundation species and their consequences for community organization, biodiversity, and conservation. BioScience 61: 782–789.
- 13. Bruno JF, Bertness MD (2001) Habitat modification and facilitation in benthic marine communities. In: Bertness MD, Gaines SD, Hay J, editors. Marine Community Ecology. Sunderland: Sinauer Associates. pp. 201–218.
- 14. Dayton PK (1972) Toward an understanding of community resilience and the potential effects of enrichments to the benthos at McMurdo Sound, Antartica. In: Parker BC, editor. Proceedings of the Colloquium on Conservation Problems in Antartica. Lawrence: Allen Press. pp. 81–96.
- 15. McKee K, Rogers K, Saintilan N (2012) Response of salt marsh and mangrove wetlands to changes in atmospheric CO2, climate, and sea level. In: Middleton BA, editor. Global Change and the Function and Distribution of Wetlands: Global Change Ecology and Wetlands. Dordrecht: Springer. pp. 63–96.
- 16. Saintilan N, Wilson NC, Rogers K, Rajkaran A, Krauss KW (2014) Mangrove expansion and salt marsh decline at mangrove poleward limits. Global Change Biology 20: 147–157.
- 17. Tomlinson PB (1986) The Botany of Mangroves. New York: Cambridge University Press. 413 p.
- 18. Alongi DM (2009) The Energetics of Mangrove Forests. New York: Springer. 216 p.
- 19. Adam P (1990) Saltmarsh Ecology. Cambridge: Cambridge University Press.
- 20. Cavanaugh KC, Kellner JR, Forde AJ, Gruner DS, Parker JD, et al. (2014) Poleward expansion of mangroves is a threshold response to decreased frequency of extreme cold events. Proceedings of the National Academy of Sciences 111: 723–727.
- 21. Pickens CN, Hester MW (2011) Temperature tolerance of early life history stages of black mangrove Avicennia germinans: implications for range expansion. Estuaries and Coasts 34: 824–830.
- 22. Giri C, Long J, Tieszen L (2011) Mapping and monitoring Louisiana's mangroves in the aftermath of the 2010 Gulf of Mexico Oil Spill. Journal of Coastal Research 27: 1059–1064.
- 23. Ross MS, Ruiz PL, Sah JP, Hanan EJ (2009) Chilling damage in a changing climate in coastal landscapes of the subtropical zone: a case study from south Florida. Global Change Biology 15: 1817–1832.
- 24. Woodroffe CD, Grindrod J (1991) Mangrove biogeography: the role of Quaternary environmental and sea-level change. Journal of Biogeography 18: 479–492.
- 25. Barbier EB, Hacker SD, Kennedy C, Koch EW, Stier AC, et al. (2011) The value of estuarine and coastal ecosystem services. Ecological Monographs 81: 169–193.
- 26. Perry CL, Mendelssohn IA (2009) Ecosystem effects of expanding populations of Avicennia germinans in a Louisiana salt marsh. Wetlands 29: 396–406.
- 27. Comeaux RS, Allison MA, Bianchi TS (2012) Mangrove expansion in the Gulf of Mexico with climate change: Implications for wetland health and resistance to rising sea levels. Estuarine, Coastal and Shelf Science 96: 81–95.
- 28. Chavez-Ramirez F, Wehtje W (2012) Potential impact of climate change scenarios on whooping crane life history. Wetlands 32: 11–20.
- 29. Henry KM, Twilley RR (2013) Soil development in a coastal Louisiana wetland during a climate-induced vegetation shift from salt marsh to mangrove. Journal of Coastal Research 29: 1273–1283.
- 30. Lewis DB, Brown JA, Jimenez KL (2014) Effects of flooding and warming on soil organic matter mineralization in Avicennia germinans mangrove forests and Juncus roemerianus salt marshes. Estuarine, Coastal and Shelf Science 139: 11–19.
- 31. Bianchi TS, Allison MA, Zhao J, Li X, Comeaux RS, et al. (2013) Historical reconstruction of mangrove expansion in the Gulf of Mexico: linking climate change with carbon sequestration in coastal wetlands. Estuarine, Coastal and Shelf Science 119: 7–16.
- 32. Krauss KW, McKee KL, Lovelock CE, Cahoon DR, Saintilan N, et al. (2014) How mangrove forests adjust to rising sea level. New Phytologist 202: 19–34.
- 33. Kirwan ML, Megonigal JP (2013) Tidal wetland stability in the face of human impacts and sea-level rise. Nature 504: 53–60.
- 34. Morris JT, Sundareshwar PV, Nietch CT, Kjerfve B, Cahoon D (2002) Responses of coastal wetlands to rising sea level. Ecology 83: 2869–2877.
- 35. Duarte CM, Losada IJ, Hendriks IE, Mazarrasa I, Marbà N (2013) The role of coastal plant communities for climate change mitigation and adaptation. Nature Climate Change 3: 961–968.
- 36. Osland MJ, Spivak AC, Nestlerode JA, Lessmann JM, Almario AE, et al. (2012) Ecosystem development after mangrove wetland creation: plant-soil change across a 20-year chronosequence. Ecosystems 15: 848–866.
- 37. Mcleod E, Chmura GL, Bouillon S, Salm R, Björk M, et al. (2011) A blueprint for blue carbon: toward an improved understanding of the role of vegetated coastal habitats in sequestering CO2. Frontiers in Ecology and the Environment 9: 552–560.
- 38. Gedan KB, Kirwan ML, Wolanski E, Barbier EB, Silliman BR (2011) The present and future role of coastal wetland vegetation in protecting shorelines: answering recent challenges to the paradigm. Climatic Change 106: 7–29.
- 39. Feagin RA, Lozada-Bernard SM, Ravens TM, Möller I, Yeager KM, et al. (2009) Does vegetation prevent wave erosion of salt marsh edges? Proceedings of the National Academy of Sciences 106: 10109–10113.
- 40. Odum WE, McIvor CC, Smith TJ III (1982) The ecology of mangroves of south Florida: a community profile: U.S. Fish and Wildlife Service, Office of Biological Services, Washington, D.C. FWS/OBS-81/24. 144 p.
- 41. Caudill MC (2005) Nekton utilization of black mangrove (Avicennia germinans) and smooth cordgrass (Spartina alterniflora) sites in southwestern Caminada Bay, Louisiana. M.S. Thesis. Louisiana State University, Department of Oceanography and Coastal Sciences, Baton Rouge, LA.
- 42. Komiyama A, Ong JE, Poungparn S (2008) Allometry, biomass, and productivity of mangrove forests: A review. Aquatic Botany 89: 128–137.
- 43. Clough BF, Dixon P, Dalhaus O (1997) Allometric relationships for estimating biomass in multi-stemmed mangrove trees. Australian Journal of Botany 45: 1023–1031.
- 44. Cintrón G, Schaeffer Novelli Y (1984) Methods for studying mangrove structure. In: Snedacker SC, Snedaker JG, editors. The mangrove ecosystem: research methods. Paris: UNESCO. pp. 91–113.
- 45. Smith TJ III, Whelan KR (2006) Development of allometric relations for three mangrove species in South Florida for use in the Greater Everglades Ecosystem restoration. Wetlands Ecology and Management 14: 409–419.
- 46. Day JW, Conner WH, Ley-Lou F, Day RH, Navarro AM (1987) The productivity and composition of mangrove forests, Laguna de Términos, Mexico. Aquatic Botany 27: 267–284.
- 47. Fromard F, Puig H, Mougin E, Marty G, Betoulle JL, et al. (1998) Structure, above-ground biomass and dynamics of mangrove ecosystems: new data from French Guiana. Oecologia 115: 39–53.
- 48. Clough BF, Scott K (1989) Allometric relationships for estimating above-ground biomass in six mangrove species. Forest Ecology and Management 27: 117–127.
- 49. Clough B, Dixon P, Dalhaus O (1997) Allometric relationships for estimating biomass in multi-stemmed mangrove trees. Australian Journal of Botany 45: 1023–1031.
- 50. Cleary MB, Pendall E, Ewers BE (2008) Testing sagebrush allometric relationships across three fire chronosequences in Wyoming, USA. Journal of Arid Environments 72: 285–301.
- 51. Uresk DW, Gilbert RO, Rickard WH (1977) Sampling big sagebrush for phytomass. Journal of Range Management 30: 311–314.
- 52. Northup BK, Zitzer SF, Archer S, McMurtry CR, Boutton TW (2005) Above-ground biomass and carbon and nitrogen content of woody species in a subtropical thornscrub parkland. Journal of Arid Environments 62: 23–43.
- 53. McClaran MP, McMurtry CR, Archer SR (2013) A tool for estimating impacts of woody encroachment in arid grasslands: allometric equations for biomass, carbon and nitrogen content in Prosopis velutina. Journal of Arid Environments 88: 39–42.
- 54. Woodroffe CD (1985) Studies of a mangrove basin, Tuff Crater, New Zealand: I. Mangrove biomass and production of detritus. Estuarine, Coastal and Shelf Science 20: 265–280.
- 55. Ross MS, Ruiz PL, Telesnicki GJ, Meeder JF (2001) Estimating above-ground biomass and production in mangrove communities of Biscayne National Park, Florida (USA). Wetlands Ecology and Management 9: 27–37.
- 56. Coronado-Molina C, Day JW, Reyes E, Perez BC (2004) Standing crop and aboveground biomass partitioning of a dwarf mangrove forest in Taylor River Slough, Florida. Wetlands Ecology and Management 12: 157–164.
- 57. Parvaresh H, Parvaresh E, Zahedi G (2012) Establishing allometric relationship using crown diameter for the estimation of above-ground biomass of grey mangrove, Avicennia Marina (Forsk) Vierh in mangrove forests of Sirik, Iran. Journal of Basic and Applied Scientific Research 2: 1763–1769.
- 58. Patterson S, McKee KL, Mendelssohn IA (1997) Effects of tidal inundation and predation on Avicennia germinans seedling establishment and survival in a sub-tropical mangal/salt marsh community. Mangroves and Salt Marshes 1: 103–111.
- 59. Stagg CL, Mendelssohn IA (2011) Controls on resilience and stability in a sediment-subsidized salt marsh. Ecological Applications 21: 1731–1744.
- 60. Krauss KW, McKee KL, Hester MW (2014) Water use characteristics of black mangrove (Avicennia germinans) communities along an ecotone with marsh at a northern geographical limit. Ecohydrology 7: 354–365.
- 61. Alleman LK, Hester MW (2011) Refinement of the fundamental niche of black mangrove (Avicennia germinans) seedlings in Louisiana: applications for restoration. Wetlands Ecology and Management 19: 47–60.
- 62. McKee KL, Rooth JE (2008) Where temperate meets tropical: multi-factorial effects of elevated CO2, nitrogen enrichment, and competition on a mangrove-salt marsh community. Global Change Biology 14: 971–984.
- 63. West RC (1977) Tidal salt-marsh and mangal formations of Middle and South America. In: Chapman VJ, editor. Wet coastal ecosystems. Amsterdam: Elsevier. pp. 193–213.
- 64. Michot TC, Day RH, Wells CJ (2010) Increase in black mangrove abundance in coastal Louisiana. Lousiana Natural Resource News. Newsletter of the Lousiana Association of Professional Biologists January 2010: 4–5.
- 65. Sprugel D (1983) Correcting for bias in log-transformed allometric equations. Ecology 64: 209–210.
- 66. Beauchamp JJ, Olson JS (1973) Corrections for bias in regression estimates after logarithmic transformation. Ecology 54: 1403–1407.
- 67. Lugo AE, Snedaker SC (1974) The ecology of mangroves. Annual Review of Ecology and Systematics 5: 39–64.
- 68. Pool DJ, Snedaker SC, Lugo AE (1977) Structure of mangrove forests in Florida, Puerto Rico, Mexico, and Costa Rica. Biotropica 9: 195–212.
- 69. Feller IC, McKee KL, Whigham DF, O'Neill JP (2003) Nitrogen vs. phosphorus limitation across an ecotonal gradient in a mangrove forest. Biogeochemistry 62: 145–175.
- 70. Castañeda-Moya E, Twilley RR, Rivera-Monroy VH (2013) Allocation of biomass and net primary productivity of mangrove forests along environmental gradients in the Florida Coastal Everglades, USA. Forest Ecology and Management 307: 226–241.
- 71. Cintrón G, Lugo AE, Pool DJ, Morris G (1978) Mangroves of arid environments in Puerto Rico and adjacent islands. Biotropica 10: 110–121.
- 72. Doyle TW, Krauss KW, Conner WH, From AS (2010) Predicting the retreat and migration of tidal forests along the northern Gulf of Mexico under sea-level rise. Forest Ecology and Management 259: 770–777.
- 73. Lovelock CE, Ball MC, Choat B, Engelbrecht BM, Holbrook NM, et al. (2006) Linking physiological processes with mangrove forest structure: phosphorus deficiency limits canopy development, hydraulic conductivity and photosynthetic carbon gain in dwarf Rhizophora mangle. Plant, cell & environment 29: 793–802.