Abstract
Original language | English |
---|---|
Pages (from-to) | 35951 |
Journal | Scientific Reports |
Volume | 6 |
Early online date | 24 Oct 2016 |
DOIs | |
Publication status | E-pub ahead of print - 24 Oct 2016 |
Keywords
- Palaeontology
- tectonics
- wetlands ecology
- remote sensing
- time-series
- NDVI
- Okavango
- MODIS
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In: Scientific Reports, Vol. 6, 24.10.2016, p. 35951.
Research output: Contribution to journal › Article (journal) › peer-review
TY - JOUR
T1 - Environmental hydro-refugia demonstrated by vegetation vigour in the Okavango Delta, Botswana
AU - Reynolds, Sally C
AU - Marston, Christopher G
AU - Hassani, Hossein
AU - King, Geoff C P
AU - Bennett, Matthew R
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D. & Ellery, W. N. Seasonal flooding in the Okavango Delta, Botswana-Recent history and future prospects. S. Afr. J. Sci. 96, 25–33 (2000). 8. Gumbricht, T., McCarthy, J. & McCarthy, T. S. Channels, wetlands and islands in the Okavango Delta, Botswana, and their relation to hydrological and sedimentological processes. Earth Surf. Proc. Land. 29, 15–29 (2004). 9. Burrough, S. L., Thomas, D. S. & Bailey, R. M. Mega-Lake in the Kalahari: a Late Pleistocene record of the Palaeolake Makgadikgadi system. Quaternary Sci. Rev. 28(15), 1392–1411 (2009). 10. Moore, A. E., Cotterill, F. P. D. & Eckhardt, F. D. The evolution and ages of Makgadikgadi palaeo-lakes: Consilient evidence from Kalahari drainage evolution South-Central Africa. S. Afr. J. Geol. 115(3), 385–413 (2012). 11. Riedel, F. et al. Dynamics of a Kalahari long-lived mega-lake system: hydromorphological and limnological changes in the Makgadikgadi Basin (Botswana) during the terminal 50 ka. Hydrobiologica 739, 25–53 (2014). 12. Podgorski, J. E. et al. Paleo-megalake and paleo-megafan in southern Africa.Geology 41(11), 1155–1158 (2013). 13. Modisi, M. P. Fault system at the southeastern boundary of the Okavango Rift, Botswana. J. Afr. Earth Sci. 30(3), 569–578 (2000). 14. Kinabo, B. D. et al. Early structural development of the Okavango rift zone, NW Botswana. J. Afr. Earth Sci. 48(2), 125–136 (2007). 15. Haddon, L. G. Isopach map of the Kalahari Group. Council for Geoscience, Pretoria 1999. 16. Gumbricht, T., McCarthy, T. S. & Merry, C. L. The topography of the Okavango Delta, Botswana, and its tectonic and sedimentological implications. S. Afr. J. Geol. 104(3), 243–264 (2001). 17. McCarthy, T. S., Smith, N. D., Ellery, W. N. & Gumbricht, T. The Okavango delta–semiarid alluvial-fan sedimentation related to incipient rifting. Sedimentation in continental rifts, SEPM Special publication 73, 179–193 (2002). 18. McCarthy, T. S., McIver, J. R. & Verhagen, B. T. Groundwater evolution, chemical sedimentation and carbonate brine formation on an island in the Okavango Delta swamp, Botswana. Appl. Geochem. 6(6), 577–595 (1991). 19. McCarthy, T. S. & Ellery, W. N. The Okavango Delta. T. Roy. Soc. S Afr. 53(2), 157–182 (1998). 20. McCarthy, T. S. Groundwater in the wetlands of the Okavango Delta, Botswana, and its contribution to the structure and function of the ecosystem. J Hydrol. 320(3), 264–282 (2006). 21. Wayant, N. M. et al. Correlation between normalized difference vegetation index and malaria in a subtropical rain forest undergoing rapid anthropogenic alteration. Geospatial Health 4(2), 179–190 (2010). 22. Hassani, H., Heravi, S. & Zhigljavsky, A. Forecasting UK Industrial Production with Multivariate Singular Spectrum Analysis. J. Forecasting 32(5) (2013) 395–408 (2013). 23. Hassani, H. Singular Spectrum Analysis: Methodology and Comparison. J. Data Sci. 5(2), 239–257 (2007). 24. Sanei, S. & Hassani, H. Singular Spectrum Analysis of Biomedical Signals CRC Press: United States (2015). 25. Hassani, H. & Silva, E. S. A Kolmogorov-Smirnov Based Test for Comparing the Predictive Accuracy of Two Sets of Forecasts. Econometrics 3(3), (2015) 590–609 (2015). 26. Ellery, W. N. et al. Vegetation, hydrology and sedimentation processes as determinants of channel form and dynamics in the northeastern Okavango Delta, Botswana. Afr. J. Ecol. 31(1), 10–25 (1993). 27. Thito, K., Wolski, P. & Murray-Hudson, M. Spectral reflectance of floodplain vegetation communities of the Okavango Delta. Wetlands Ecology and Management 23(4), pp.637–648 (2015). 28. Ringrose, S., Vanderpost, C. & Matheson, W. Mapping ecological conditions in the Okavango delta, Botswana using fine and coarse resolution systems including simulated SPOT vegetation imagery. Intern. J. Rem. Sens. 24, 1029–1052 (2003). 29. Gröngröft, A., Luther-Mosebach, J., Landschreiber, L. & Eschenbach, A. Cusseque-Soils.–In: Oldeland, J., Erb, C., Finckh, M., Jürgens, N. (Eds.): Environmental Assessments in the Okavango Region. –Biodiversity & Ecology 5, 51–54 (2013). 30. Wolski, P. & Murray-Hudson, M. Flooding dynamics in a large low-gradient alluvial fan, the Okavango Delta, Botswana, from analysis and interpretation of a 30-year hydrometric record. Hydrol. Earth Syst. Sci. Discussions 10(1), pp.127–137 (2006). 31. Wolski, P., Todd, M. C., Murray-Hudson, M. A. & Tadross, M. Multi-decadal oscillations in the hydro-climate of the Okavango River system during the past and under a changing climate. J. Hydrol. 475, pp.294–305 (2012). 32. Mazvimavi, D. & Wolski, P. Long-term variations of annual flows of the Okavango and Zambezi Rivers. Phys. Chem. Earth, Parts A/B/C 31(15), pp.944–951 (2006). 33. Hurrell, J. W. Decadal trends in the North Atlantic Oscillation: regional temperatures and precipitation. Science 269(5224), pp.676–679 (1995). 34. Mantua, N. J. et al. A Pacific interdecadal climate oscillation with impacts on salmon production. B. Am. Meteorol. Soc. 78(6), pp.1069–1079 (1997). 35. Jury, M. R. 2010. Ethiopian decadal climate variability. Theor. Appl. Climatol. 101(1–2), 29–40 (2010). 36. Dincer, T., Child, S. & Khupe, B. A simple mathematical model of a complex hydrologic system-Okavango Swamp, Botswana. J. Hydrol. 93(1–2), 41–65 (1987). 37. Snowy Mountains Engineering Corporation. Southern Okavango Integrated Water Development Project. Gaborone, Botswana, Department of Water Affairs (1990). 38. Gieske, A. Modelling outflow from the Jao/Boro River system in the Okavango Delta, Botswana. J. Hydrol. 193, 214–239 (1997). 39. Wolski, P. & Savenije, H. Dynamics of surface and groundwater interactions in the floodplain system of the Okavango Delta, Botswana. J. Hydrol. 320, 283–301 (2006). 40. Wolski, P., Savenije, H. H. G., Murray-Hudson, M. & Gumbricht, T. Modelling of the flooding in the Okavango Delta, Botswana, using a hybrid reservoir-GIS model. J. Hydrol. 331(1), 58–72 (2006). 41. Kinabo, B. D. et al., Early structural development of the Okavango rift zone, NW Botswana. J. Afr. Earth Sci. 48(2), 125–136 (2007). 42. Burrough, S. L. Thomas, D. S. & Singarayer, J. S. Late Quaternary hydrological dynamics in the Middle Kalahari: forcing and feedbacks. Earth-Sci. Rev. 96(4), 313–326 (2009). 43. Tooth, S. & McCarthy, T. S. Wetlands in drylands: geomorphological and sedimentological characteristics, with emphasis on examples from southern Africa. Prog. Phys. Geog. 31(1), 3–41 (2007). 44. Ramberg, L. et al. Species diversity of the Okavango delta, Botswana. Aquat. Sci. 68(3), 310–337 (2006). 45. Robinson, T. J. et al. Phylogeny and vicariant speciation of the Grey Rhebok, Pelea capreolus. Heredity, 112(3), 325–332 (2014). 46. Sepulchre, P. et al. Tectonic uplift and Eastern Africa aridification. Science 313(5792), 1419–1423 (2006). 47. Bailey, G. N., Reynolds, S. C. & King, G. C. P. Landscapes of human evolution: models and methods of tectonic geomorphology and the reconstruction of hominin landscapes. J. Hum. Evol. 60, 257–280 (2011). 48. Bennett, C. E., Marshall, J. D. & Stanistreet, I. G. Carbonate horizons, paleosols, and lake flooding cycles: Beds I and II of Olduvai Gorge, Tanzania. J. Hum Evol. 63(2), 328–341 (2012). 49. Ashley, G. M. et al. Paleoenvironmental and paleoecological reconstruction of a freshwater oasis in savannah grassland at FLK North, Olduvai Gorge, Tanzania. Quaternary Res. 74(3), 333–343 (2010). 50. Ashley, G. M. et al. Sedimentary geology and human origins: a fresh look at Olduvai Gorge, Tanzania. J. Sediment. Res. 80(8), 703–709 (2010).
PY - 2016/10/24
Y1 - 2016/10/24
N2 - Climate shifts at decadal scales can have environmental consequences, and therefore, identifying areas that act as environmental refugia is valuable in understanding future climate variability. Here we illustrate how, given appropriate geohydrology, a rift basin and its catchment can buffer vegetation response to climate signals on decadal time-scales, therefore exerting strong local environmental control. We use time-series data derived from Normalised Difference Vegetation Index (NDVI) residuals that record vegetation vigour, extracted from a decadal span of MODIS images, to demonstrate hydrogeological buffering. While this has been described previously it has never been demonstrated via remote sensing and results in relative stability in vegetation vigour inside the delta, compared to that outside. As such the Delta acts as a regional hydro-refugium. This provides insight, not only to the potential impact of future climate in the region, but also demonstrates why similar basins are attractive to fauna, including our ancestors, in regions like eastern Africa. Although vertebrate evolution operates on time scales longer than decades, the sensitivity of rift wetlands to climate change has been stressed by some authors, and this work demonstrates another example of the unique properties that such basins can afford, given the right hydrological conditions.
AB - Climate shifts at decadal scales can have environmental consequences, and therefore, identifying areas that act as environmental refugia is valuable in understanding future climate variability. Here we illustrate how, given appropriate geohydrology, a rift basin and its catchment can buffer vegetation response to climate signals on decadal time-scales, therefore exerting strong local environmental control. We use time-series data derived from Normalised Difference Vegetation Index (NDVI) residuals that record vegetation vigour, extracted from a decadal span of MODIS images, to demonstrate hydrogeological buffering. While this has been described previously it has never been demonstrated via remote sensing and results in relative stability in vegetation vigour inside the delta, compared to that outside. As such the Delta acts as a regional hydro-refugium. This provides insight, not only to the potential impact of future climate in the region, but also demonstrates why similar basins are attractive to fauna, including our ancestors, in regions like eastern Africa. Although vertebrate evolution operates on time scales longer than decades, the sensitivity of rift wetlands to climate change has been stressed by some authors, and this work demonstrates another example of the unique properties that such basins can afford, given the right hydrological conditions.
KW - Palaeontology
KW - tectonics
KW - wetlands ecology
KW - remote sensing
KW - time-series
KW - NDVI
KW - Okavango
KW - MODIS
U2 - 10.1038/srep35951
DO - 10.1038/srep35951
M3 - Article (journal)
SN - 2045-2322
VL - 6
SP - 35951
JO - Scientific Reports
JF - Scientific Reports
ER -