Earth: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.

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.

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.

EFTs 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)
  • Annual mean of VI (VI_Mean): estimator of annual primary production, one of the most essential and integrative descriptors of ecosystem functioning.
  • Intra-annual coefficient of variation of VI (VI_sCV): descriptor of seasonality or differences in carbon gains between the growing and non growing seasons.
  • Date of maximum VI value (VI_DMAX): phenological indicator of when in the year does the growing season take place.[21][22]

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 EFTs applications

  • To characterize the spatial and temporal heterogeneity of ecosystem functioning at the local and regional scales.[16][22]
  • To describe the biogeographical patterns of functional diversity at the ecosystem level.[2]
  • To assess the functional diversity at the ecosystem level by determining the EFTs richness and equity in the landscape.[23]
  • To evaluate the environmental and human controls of ecosystem functional diversity.[3]
  • To identify priorities for Biodiversity Conservation.[24]
  • To assess the representativeness of protected area networks to capture the functional diversity at the ecosystem level.[25]
  • To quantify and monitor the level of provision of intermediate support ecosystem services.[26][27]
  • To assess the effects of land-use changes on ecosystem functioning.[28][29]
  • To improve weather forecast models by introducing the effects of inter-annual changes in ecosystem biophysical properties into land-surface and general circulation atmospheric models.[30][31]

Pros of EFTs

  • Functional classifications provide a useful framework for understanding the large-scale ecological changes.[22]
  • Environmental changes are particularly noticeable at the ecosystem level.[32]
  • Ecosystem functional attributes, such as the exchange of energy and matter of an ecosystem, have shorter time response to environmental changes than structural or compositional attributes, such as species composition or vegetation physiognomy.[33]
  • Ecosystem functioning can be more easily monitored than structural attributes by using remote sensing at different spatial scales, over large extents, and utilizing a common protocol in space and time.[1]
  • Functional attributes allow the qualitative and quantitative evaluation of ecosystem services.[34]

References

  1. ↑ 1.0 1.1 1.2 1.3 1.4 1.5 1.6 Paruelo (2001). "Current distribution of ecosystem functional types in temperate South America.". Ecosystems 4 (7): 683–698. doi:10.1007/s10021-001-0037-9. 
  2. ↑ 2.0 2.1 2.2 2.3 2.4 2.5 2.6 Alcaraz-Segura (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. ↑ 3.0 3.1 3.2 3.3 3.4 3.5 Alcaraz-Segura (2013). "Environmental and Human Controls of Ecosystem Functional Diversity in Temperate South America". Remote Sensing 5 (1): 127–154. doi:10.3390/rs5010127. Bibcode: 2013RemS....5..127A. 
  4. ↑ 4.0 4.1 Virginia (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. 
  6. ↑ Shugart, H.H. (1997). "Plant and ecosystem functional types". in T.M. Smith. 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. Plant functional types: their relevance to ecosystem properties and global change. Cambridge University Press. pp. 91–103. 
  8. ↑ Scholes (1997). "Plant functional types in African savannas and grasslands". in T.M. Smith, H.H. Shugart and F.I. Woodward. Plant functional types: their relevance to ecosystem properties and global change. Cambridge University Press. pp. 255–268. 
  9. ↑ Aber (1999). J.D. Tenhunen. ed. 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. 
  10. ↑ Reynolds; Wu (1999). J.D. Tenhunen. ed. 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. 
  12. ↑ Valentini (1999). J.D. Tenhunen. ed. 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. doi:10.1016/s0303-2434(99)85023-5. Bibcode: 1999IJAEO...1....9A. 
  14. ↑ Karlsen (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 (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. 
  16. ↑ 16.0 16.1 Fernández (2010). "Ecosystem functioning of protected and altered Mediterranean environments: A remote sensing classification in Doñana, Spain.". Remote Sensing of Environment 114 (1): 211–220. doi:10.1016/j.rse.2009.09.001. Bibcode: 2010RSEnv.114..211F. 
  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. doi:10.1016/j.isprsjprs.2009.03.001. Bibcode: 2009JPRS...64..422G. 
  18. ↑ Ivits (2013). "Global Biogeographical Pattern of Ecosystem Functional Types Derived From Earth Observation Data.". Remote Sensing 5 (7): 3305–3330. doi:10.3390/rs5073305. Bibcode: 2013RemS....5.3305I. 
  19. ↑ Pérez-Hoyos (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. 
  21. ↑ Pettorelli (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. ↑ 22.0 22.1 22.2 Alcaraz-Segura (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. 
  23. ↑ Cazorla, B. (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. 
  24. ↑ Cabello (2008). "Funcionamiento ecosistémico y evaluación de prioridades geográficas en conservación". Ecosistemas 17 (3): 53–63. 
  25. ↑ Cabello (2013). Di Bella. ed. "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 (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 (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. 
  28. ↑ Oki (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 (2013). "The Impact of Ecosystem Functional Type Changes on the La Plata Basin Climate". Advances in Atmospheric Sciences 30 (5): 1387–1405. doi:10.1007/s00376-012-2149-x. Bibcode: 2013AdAtS..30.1387L. 
  30. ↑ Lee (2013). "Effect of implementing ecosystem functional type data in a mesoscale climate model". Advances in Atmospheric Sciences 30 (5): 1373–1386. doi:10.1007/s00376-012-2143-3. Bibcode: 2013AdAtS..30.1373L. 
  31. ↑ Müller (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. doi:10.1175/jcli-d-13-00463.1. Bibcode: 2014JCli...27.6754M. 
  32. ↑ Vitousek (1994). "Beyond global warming: ecology and global change.". Ecology 75 (7): 1861–1876. doi:10.2307/1941591. 
  33. ↑ Milchunas; Lauenroth (1995). "Inertia in plant community structure: State changes after cessation of nutrient enrichment stress". Ecology Applied 5: 1195–2005. 
  34. ↑ Costanza (2006). The value of New Jersey's ecosystem services and natural capital. 



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