Ecosystem Functional Type

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Fig.1: Ecosystem Functional Types (EFT) of temperate South America based on Moderate Resolution Imaging Spectroradiometer Enhanced Vegetation Index (MODIS-EVI) dynamics (Alcaraz-Segura et al. 2013). The map shows the EFTs of the 2001-2008 period. EFTs.PNG
Fig.1: Ecosystem Functional Types (EFT) of temperate South America based on Moderate Resolution Imaging Spectroradiometer Enhanced Vegetation Index (MODIS-EVI) dynamics (Alcaraz-Segura et al. 2013). The map shows the EFTs of the 2001–2008 period.

Ecosystem Functional Type (EFT) is an ecological concept to characterize ecosystem functioning. Ecosystem Functional Types are defined as groups of ecosystems or patches of the land surface that share similar dynamics of matter and energy exchanges between the biota and the physical environment. [1] [2] [3] The EFT concept is analogous to the Plant Functional Types (PFTs) concept, but defined at a higher level of the biological organization. As plant species can be grouped according to common functional characteristics, ecosystems can be grouped according to their common functional behavior.

Contents

One of the most used approaches to implement this concept has been the identification of EFTs from the satellite-derived dynamics of primary production, [1] [2] an essential and integrative descriptor of ecosystem functioning. [4]

History

In 1992, Soriano and Paruelo [5] proposed the concept of Biozones to identify vegetation units that share ecosystem functional characteristics using time-series of satellite images of spectral vegetation indices. Biozones were later renamed to EFTs by Paruelo et al. (2001), [1] using an equivalent definition and methodology. [6] was one of the first authors that used the term EFT as "aggregated components of ecosystems whose interactions with one another and with the environment produce differences in patterns of ecosystem structure and dynamics". Walker (1997) [7] proposed the use of a similar term, vegetation functional types, for groups of PFTs in sets that constitute the different states of vegetation succession in non-equilibrium ecosystems. The same term was applied by Scholes et al. [8] in a wider sense for those areas having similar ecological attributes, such as PFTs composition, structure, phenology, biomass or productivity. Several studies have applied hierarchy and patch dynamic theories [9] [10] [11] for the definition of ecosystem and landscape functional types at different spatial scales, by scaling-up emergent structural and functional properties from patches to regions. Valentini et al. [12] defined land functional units by focusing on patches of the land surface that are able to exchange mass and energy with the atmosphere and show a coordinated and specific response to environmental factors.

Paruelo et al. (2001) [1] and Alcaraz-Segura et al. (2006, 2013) [2] [3] refined the EFT concept and proposed a remote-sensing based methodology to derive them. Since then, several authors have implemented the idea under the same or similar approaches using NOAA-AVHRR, MODIS and Landsat archives. [2] [3] [13] [14] [15] [16] [17] [18] [19] [20] In brief, all these approaches use the seasonal dynamics of spectral indices related to key functional aspects of ecosystems such as primary production, water exchange, heat exchange and radiative balance.

Identification

The functional classification of EFTs developed by Paruelo et al. (2001) [1] and Alcaraz-Segura et al. (2006, 2013) [2] [3] uses time series of spectral vegetation indexes to capture the carbon gains dynamics, the most integrative indicator of ecosystem functioning. [4] To build EFTs, these authors derive three descriptors or metrics from the seasonal dynamics (annual curve) of spectral vegetation indexes (VI) that capture most of the variance in the time series (Fig.2): [1] [2] [3]

Fig.2: Annual curve of spectral vegetation indexes (VI: Enhanced Vegetation Index (MODIS-EVI) AnualDynamics EVI 3vars.png
Fig.2: Annual curve of spectral vegetation indexes (VI: Enhanced Vegetation Index (MODIS-EVI)

The range of values of each VI metric is divided into four intervals, giving the potential number of 4x4x4=64 EFTs. Each EFT is assigned a code of two letters and a number (three characters). The first letter of the code (capital) corresponds to the VI_Mean level, ranging from A to D for low to high (increasing) VI_Mean or productivity. The second letter (small) shows the seasonal CV, ranging from a to d for high (decreasing) to low VI_sCV or seasonality. The numbers refer to DMAX or phenology and indicate the season of maximum VI (1–4: spring, summer, autumn and winter).

Current known applications

Advantages

Related Research Articles

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References

  1. 1 2 3 4 5 6 7 Paruelo; et al. (2001). "Current distribution of ecosystem functional types in temperate South America". Ecosystems. 4 (7): 683–698. CiteSeerX   10.1.1.660.431 . doi:10.1007/s10021-001-0037-9. S2CID   8173744.
  2. 1 2 3 4 5 6 7 Alcaraz-Segura; et al. (2006). "Identification of current ecosystem functional types in the Iberian Peninsula". Global Ecology and Biogeography. 15 (2): 200–212. doi:10.1111/j.1466-822x.2006.00215.x.
  3. 1 2 3 4 5 6 Alcaraz-Segura; et al. (2013). "Environmental and Human Controls of Ecosystem Functional Diversity in Temperate South America". Remote Sensing. 5 (1): 127–154. Bibcode:2013RemS....5..127A. doi: 10.3390/rs5010127 . hdl: 10835/7381 .
  4. 1 2 Virginia; et al. (2001). "Principles of ecosystem function". Encyclopedia of Biodiversity. Academic Press. pp. 345–352.
  5. Soriano & Paruelo (1992). "Biozones: vegetation units defined by functional characters identifiable with the aid of satellite sensor images". Global Ecology and Biogeography Letters. 2 (3): 82–89. doi:10.2307/2997510. JSTOR   2997510.
  6. Shugart, H.H. (1997). "Plant and ecosystem functional types". In T.M. Smith; H.H. Shugart; F.I. Woodward) (eds.). Plant functional types: their relevance to ecosystem properties and global change. Cambridge University Press. pp. 20–45.
  7. Walker, B.H. (1997). "Functional types in non-equilibrium ecosystems". In T.M. Smith; H.H. Shugart; F.I. Woodward (eds.). Plant functional types: their relevance to ecosystem properties and global change. Cambridge University Press. pp. 91–103.
  8. Scholes; et al. (1997). "Plant functional types in African savannas and grasslands". In T.M. Smith, H.H. Shugart and F.I. Woodward (ed.). Plant functional types: their relevance to ecosystem properties and global change. Cambridge University Press. pp. 255–268.
  9. Aber; et al. (1999). J.D. Tenhunen; P. Kabat (eds.). Group report: hydrological and biogeochemical processes in complex landscapes — what is the role of temporal and spatial ecosystem dynamics?Integrating hydrology, ecosystem dynamics and biogeochemistry in complex landscapes. John Wiley & Sons, Berlin. pp. 335–356.{{cite book}}: CS1 maint: location missing publisher (link)
  10. Reynolds & Wu (1999). J.D. Tenhunen & P. Kabat (eds.). Do landscape structural and functional units exist? Integrating hydrology, ecosystem dynamics and biogeochemistry in complex landscapes. Berlin: John Wiley & Sons. pp. 273–296.
  11. Wu & David (2003). S. Guhathakurta (ed.). Linking land-use change with ecosystem processes: a hierarchical patch dynamic model. Integrated land use and environmental models. Springer, Berlin. pp. 99–119.{{cite book}}: CS1 maint: location missing publisher (link)
  12. Valentini; et al. (1999). J.D. Tenhunen; P. Kabat (eds.). Ecological controls on land–surface atmospheric interactions. Integrating hydrology, ecosystem dynamics and biogeochemistry in complex landscapes. Berlin: John Wiley & Sons. pp. 105–116.
  13. Azzali & Meneti (1999). "Mapping isogrowth zones on continental scale using temporal Fourier analysis of AVHRR-NDVI data". International Journal of Applied Earth Observation and Geoinformation. 1 (1): 9–20. Bibcode:1999IJAEO...1....9A. doi:10.1016/s0303-2434(99)85023-5.
  14. Karlsen; et al. (2006). "Satellite‐based mapping of the growing season and bioclimatic zones in Fennoscandia". Global Ecology and Biogeography. 15 (4): 416–430. doi:10.1111/j.1466-822x.2006.00234.x.
  15. Duro; et al. (2007). "Development of a large area biodiversity monitoring system driven by remote sensing". Progress in Physical Geography. 31 (3): 235–260. doi:10.1177/0309133307079054. S2CID   129809993.
  16. 1 2 Fernández; et al. (2010). "Ecosystem functioning of protected and altered Mediterranean environments: A remote sensing classification in Doñana, Spain". Remote Sensing of Environment. 114 (1): 211–220. Bibcode:2010RSEnv.114..211F. doi:10.1016/j.rse.2009.09.001. hdl: 10261/50225 .
  17. Geerken (2009). "An algorithm to classify and monitor seasonal variations in vegetation phonologies and their inter-annual change". ISPRS Journal of Photogrammetry and Remote Sensing. 64 (4): 422–431. Bibcode:2009JPRS...64..422G. doi:10.1016/j.isprsjprs.2009.03.001.
  18. Ivits; et al. (2013). "Global Biogeographical Pattern of Ecosystem Functional Types Derived From Earth Observation Data". Remote Sensing. 5 (7): 3305–3330. Bibcode:2013RemS....5.3305I. doi: 10.3390/rs5073305 .
  19. Pérez-Hoyos; et al. (2015). "Identification of Ecosystem Functional Types from Coarse Resolution Imagery Using a Self-Organizing Map Approach: A Case Study for Spain". Remote Sensing. 6 (11): 11391–11419. doi: 10.3390/rs61111391 .
  20. Wang & Huang (2015). "Identification and analysis of ecosystem functional types in the west of Songnen Plain". Journal of Applied Remote Sensing. 9 (1): 096096. doi:10.1117/1.jrs.9.096096. S2CID   123090366.
  21. Pettorelli; et al. (2005). "Using the satellite-derived NDVI to assess ecological responses to environmental change". Trends in Ecology and Evolution. 20 (9): 503–510. doi:10.1016/j.tree.2005.05.011. PMID   16701427.
  22. 1 2 3 Alcaraz-Segura; et al. (2009). "Baseline characterization of major Iberian vegetation types based on the NDVI dynamics". Plant Ecology. 202: 13–29. doi:10.1007/s11258-008-9555-2. S2CID   38077489.
  23. Cazorla, B.; et al. (2015). Ecología y conservación de la diversidad funcional de ecosistemas en la transición mediterráneo-desierto-tropical de la Península de Baja California. Universidad de Granada. p.  http://hdl.handle.net/10481/38511.{{cite book}}: CS1 maint: location missing publisher (link)
  24. Cabello; et al. (2008). "Funcionamiento ecosistémico y evaluación de prioridades geográficas en conservación". Ecosistemas. 17 (3): 53–63.
  25. Cabello; et al. (2013). Di Bella; Alcaraz-Segura (eds.). "Ecosystem services assessment of national park networks for functional diversity and carbon conservation strategies using remote sensing". Earth Observation of Ecosystem Services: 179–200.
  26. Paruelo; et al. (2011). El seguimiento del nivel de provisión de los servicios ecosistémicos. Valoración de Servicios Ecosistémicos. Conceptos, herramientas y aplicaciones para el ordenamiento territorial. Buenos Aires, Argentina: Ediciones INTA. pp. 141–162.
  27. Volante; et al. (2012). "Ecosystem functional changes associated with land clearing in NW Argentina". Agriculture, Ecosystems & Environment. 154: 12–22. doi:10.1016/j.agee.2011.08.012. hdl: 11336/81528 .
  28. Oki; et al. (2013). Land Cover and Land Use Changes and Their Impacts on Hydroclimate, Ecosystems and Society. In: Asrar GR, Hurrell JW, Climate Science for Serving Society. Dordrecht: Springer Science+Business Media. pp. 185–203.
  29. Lee; et al. (2013). "The Impact of Ecosystem Functional Type Changes on the La Plata Basin Climate". Advances in Atmospheric Sciences. 30 (5): 1387–1405. Bibcode:2013AdAtS..30.1387L. doi:10.1007/s00376-012-2149-x. S2CID   123806117.
  30. Lee; et al. (2013). "Effect of implementing ecosystem functional type data in a mesoscale climate model". Advances in Atmospheric Sciences. 30 (5): 1373–1386. Bibcode:2013AdAtS..30.1373L. doi:10.1007/s00376-012-2143-3. S2CID   120485640.
  31. Müller; et al. (2014). "Regional model simulations of the 2008 drought in southern South America using a consistent set of land surface properties". Journal of Climate. 27 (17): 6754–6778. Bibcode:2014JCli...27.6754M. doi:10.1175/jcli-d-13-00463.1. hdl: 11336/92811 . S2CID   129315993.
  32. Vitousek (1994). "Beyond global warming: ecology and global change". Ecology. 75 (7): 1861–1876. doi:10.2307/1941591. JSTOR   1941591. S2CID   66138238.
  33. Milchunas & Lauenroth (1995). "Inertia in plant community structure: State changes after cessation of nutrient enrichment stress". Ecology Applied. 5: 1195–2005.
  34. Costanza; et al. (2006). "The value of New Jersey's ecosystem services and natural capital".{{cite journal}}: Cite journal requires |journal= (help)