The consequences of precipitation seasonality for Mediterranean-ecosystem vegetation of South Africa
| dc.contributor.author | Cramer, Michael D | en_ZA |
| dc.contributor.author | Hoffman, M Timm | en_ZA |
| dc.date.accessioned | 2015-12-20T16:08:29Z | |
| dc.date.available | 2015-12-20T16:08:29Z | |
| dc.date.issued | 2015 | en_ZA |
| dc.description.abstract | Globally, mediterranean-climate ecosystem vegetation has converged on an evergreen, sclerophyllous and shrubby growth form. The particular aspects of mediterranean-climate regions that contribute to this convergence include summer droughts and relatively nutrient-poor soils. We hypothesised that winter-precipitation implies stressful summer droughts and leaches soils due to greater water availability (i.e. balance between precipitation and potential evapotranspiration; P-PET) during cold periods. We conducted a comparative analysis of normalised difference vegetation indices (NDVI) and edaphic and climate properties across the biomes of South Africa. NDVI was strongly correlated with both precipitation and P-PET (r 2 = 0.8). There was no evidence, however, that winter-precipitation reduces NDVI in comparison to similar amounts of summer-precipitation. Base saturation (BS), a measure of soil leaching was, however, negatively related to P-PET (r 2 = 0.64). This led to an interaction between P-PET and BS in determining NDVI, indicating the existence of a trade-off between water availability and soil nutrients that enables NDVI to increase with precipitation, despite negative consequences for soil nutrient availability. The mechanism of this trade-off is suggested to be that water increases nutrient accessibility. This implies that along with nutrient-depauperate geologies and long periods of time since glaciation, the winter-precipitation may have contributed to the highly leached status of the soils. Since many of the ecophysiological characteristics of mediterranean-ecosystem flora are associated with low nutrient availabilities (e.g. evergreen foliage, sclerophylly, cluster roots), we conclude that mediterranean-climates promote convergence of growth-forms in these regions through high leaching capacity. | en_ZA |
| dc.identifier.apacitation | Cramer, M. D., & Hoffman, M. T. (2015). The consequences of precipitation seasonality for Mediterranean-ecosystem vegetation of South Africa. <i>PLoS One</i>, http://hdl.handle.net/11427/15932 | en_ZA |
| dc.identifier.chicagocitation | Cramer, Michael D, and M Timm Hoffman "The consequences of precipitation seasonality for Mediterranean-ecosystem vegetation of South Africa." <i>PLoS One</i> (2015) http://hdl.handle.net/11427/15932 | en_ZA |
| dc.identifier.citation | Cramer, M. D., & Hoffman, M. T. (2015). The consequences of precipitation seasonality for Mediterranean-ecosystem vegetation of South Africa. PloS one, 10(12). doi:10.1371/journal.pone.0144512 | en_ZA |
| dc.identifier.ris | TY - Journal Article AU - Cramer, Michael D AU - Hoffman, M Timm AB - Globally, mediterranean-climate ecosystem vegetation has converged on an evergreen, sclerophyllous and shrubby growth form. The particular aspects of mediterranean-climate regions that contribute to this convergence include summer droughts and relatively nutrient-poor soils. We hypothesised that winter-precipitation implies stressful summer droughts and leaches soils due to greater water availability (i.e. balance between precipitation and potential evapotranspiration; P-PET) during cold periods. We conducted a comparative analysis of normalised difference vegetation indices (NDVI) and edaphic and climate properties across the biomes of South Africa. NDVI was strongly correlated with both precipitation and P-PET (r 2 = 0.8). There was no evidence, however, that winter-precipitation reduces NDVI in comparison to similar amounts of summer-precipitation. Base saturation (BS), a measure of soil leaching was, however, negatively related to P-PET (r 2 = 0.64). This led to an interaction between P-PET and BS in determining NDVI, indicating the existence of a trade-off between water availability and soil nutrients that enables NDVI to increase with precipitation, despite negative consequences for soil nutrient availability. The mechanism of this trade-off is suggested to be that water increases nutrient accessibility. This implies that along with nutrient-depauperate geologies and long periods of time since glaciation, the winter-precipitation may have contributed to the highly leached status of the soils. Since many of the ecophysiological characteristics of mediterranean-ecosystem flora are associated with low nutrient availabilities (e.g. evergreen foliage, sclerophylly, cluster roots), we conclude that mediterranean-climates promote convergence of growth-forms in these regions through high leaching capacity. DA - 2015 DB - OpenUCT DO - 10.1371/journal.pone.0144512 DP - University of Cape Town J1 - PLoS One LK - https://open.uct.ac.za PB - University of Cape Town PY - 2015 T1 - The consequences of precipitation seasonality for Mediterranean-ecosystem vegetation of South Africa TI - The consequences of precipitation seasonality for Mediterranean-ecosystem vegetation of South Africa UR - http://hdl.handle.net/11427/15932 ER - | en_ZA |
| dc.identifier.uri | http://hdl.handle.net/11427/15932 | |
| dc.identifier.uri | http://dx.doi.org/10.1371/journal.pone.0144512 | |
| dc.identifier.vancouvercitation | Cramer MD, Hoffman MT. The consequences of precipitation seasonality for Mediterranean-ecosystem vegetation of South Africa. PLoS One. 2015; http://hdl.handle.net/11427/15932. | en_ZA |
| dc.language.iso | eng | en_ZA |
| dc.publisher | Public Library of Science | en_ZA |
| dc.publisher.department | Department of Biological Sciences | en_ZA |
| dc.publisher.faculty | Faculty of Science | en_ZA |
| dc.publisher.institution | University of Cape Town | |
| dc.rights | This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. | en_ZA |
| dc.rights.holder | © 2015 Cramer, Hoffman | en_ZA |
| dc.rights.uri | http://creativecommons.org/licenses/by/4.0 | en_ZA |
| dc.source | PLoS One | en_ZA |
| dc.source.uri | http://journals.plos.org/plosone | en_ZA |
| dc.subject.other | Ecosystems | en_ZA |
| dc.subject.other | Grasslands | en_ZA |
| dc.subject.other | Rain | en_ZA |
| dc.subject.other | South Africa | en_ZA |
| dc.subject.other | Summer | en_ZA |
| dc.subject.other | Winter | en_ZA |
| dc.subject.other | Cation exchange capacity | en_ZA |
| dc.subject.other | Water resources | en_ZA |
| dc.title | The consequences of precipitation seasonality for Mediterranean-ecosystem vegetation of South Africa | en_ZA |
| dc.type | Journal Article | en_ZA |
| uct.type.filetype | Text | |
| uct.type.filetype | Image | |
| uct.type.publication | Research | en_ZA |
| uct.type.resource | Article | en_ZA |
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