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Rainfall, Soil Type, and Plant Species Functional Types

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Rainfall, Soil Type, and Plant Species Functional Types South African Journal for Science and Technology ISSN: (Online) 2222-4173, (Print) 0254-3486 Page Page 1 ofi of 15 ii InhoudsopgaweOorspronklike Navorsing Key determinants of long-term compositional variation of the herbaceous layer in a semi-arid African savanna: Rainfall, soil type, and plant species functional types Authors: Management of the grazing resource in semi-arid savanna is dependent on inter-annual Bezuidenhout H1&5, Botha variation in available moisture, which is determined by rainfall, soil type and woody 2 3 J , Ramaswiela T and biomass. Grazing and fire may further influence trends. Understanding the effect of rainfall O’Connor T4 variability requires study over an 18-year quasi-cycle of rainfall with frequent measurement, Affiliations: a constraint which few southern African studies have met. The herbaceous layer and woody 1 South African National vegetation on deep (> 0.6 m) well-drained sands, moderately deep (0.3–0.6 m) well-drained Parks, Scientific Services, Kimberley Office, PO Box sands, moderately deep poorly drained clays, and shallow (< 0.3 m) rocky moderately 110040, Hadison Park, drained sandy loams in the deproclaimed Vaalbos National Park, South Africa, were Kimberley, 8306, South monitored from 1993 to 2015. Woody density and structure differed conspicuously across Africa soil types, but there were no trends noticed over time for the park or for any individual soil 5 Applied Behavioural type. There was also no change in the number of woody species or frequency distribution Ecology and Ecosystem over this survey period. Different functional groups responded differently to rainfall or to Research Unit, UNISA, Private Bag X6, Florida, soil water storage capacity of the soil profile. Palatable and unpalatable perennial grasses 1717, South Africa both responded to rainfall of the current and previous season but in different ways. The 2 South African National decline of palatable perennial grasses in response to increasing rainfall was influenced in Parks, Private Bag X402, part by use of relative rather than absolute abundance. This indicates that in wet years Skukuza, 1350 3 annual grasses proliferated between perennial grass tufts and were therefore measured as South African closest to point of sampling. This influence of annual grasses obscures whether perennial Environmental Observation Network, Arid Lands Node, grasses changed in absolute terms. Constraints around a lack of personnel, time and budget PO Box 110040, Hadison often determine the type of monitoring that it is feasible to conduct – a concern and probably Park, Kimberley, 8306, the reason why so many monitoring datasets and results are not published. South Africa 4 South African Keywords: long-term vegetation monitoring, statistics, semi-arid region, different soil Environmental Observation types, herbaceous layer Network, PO Box 2600, Pretoria 0001 Corresponding author: Bezuidenhout H Karakteristieke van langtermyn saamgestelde variasie van die kruidstratum in ’n semi-ariede Afrika savanna: Reënval, grondtipe enplantspesies funksionele groepe Die Dates: Received: 10/05/2018 bestuur van weidingsbronne in semi-ariede savanna is afhanklik van beskikbare water, wat Accepted: 30/08/2018 weer op sy beurt afhanklik is van reënval, grondtipe en houtagtige biomassa. Beweiding Published: en vuur kan bydraende faktore wees wat die bestuur beinvloed. Om die effek van reënval How to cite this article: veranderlikheid op plantegroei te verstaan is langtermyn studies nodig, ten minste ’n 18 Bezuidenhout H, jaar “quasi” reënvalsiklus. Die gebrek aan langtermyn data veroorsaak dat baie min van Botha J, Ramaswiela T hierdie tipe studies gepubliseer word. Die monitering van die kruidstratum en houtagtige and O’Connor T, Key plantegroei op diep (>0.6m), goed gedreineerde sanderige grond, matige diep (0.3-0.6m) goed determinants of long-term gedreineerde sande en swak gedreineerde klei-gronde en dan vlak (<0.3m) klipperige matige compositional variation of gedreineerde sandleemgrond in die gedeproklameerde Vaalbos Nasionale Park, Suid Afrika, the herbaceous layer in a semi-arid African savanna: is van 1993 tot 2015 gedoen. Hoewel houtagtige digtheid en struktuur opvallend verskillend rainfall, soil type, and plant is oor die verskillende grondtipes, kon daar geen statisties-verantwoordbare tendense oor species functional types, die tydperk in die park of in ’n spesifieke grondtipe waargeneem word nie. Daar is ook geen Suid-Afrikaanse Tydskrif betekenisvolle veranderinge in die aantal houtagtige plantspesies of die frekwensie daarvan vir Natuurwetenskap en oor die studietydperk waargeneem nie. Die verskillende funksionele plantegroeigroepe het Tegnologie 37(1) (2018) verskillend teenoor reënval of grondwaterhouvermoë gereageer. Smaaklike en onsmaaklike ’n Afrikaanse vertaling van meerjarige grasspesies het beide op huidige en vorige reënvalhoeveelhede op verskillende die manuskrip is aanlyn maniere gereageer. Die afname van smaaklike meerjarige grasse met toename in reënval beskikbaar by http://www. word gedeeltelik verklaar deurdat die relatiewe waardes teenoor die absolute waardes satnt.ac.za/index.php/satnt/ article/view/674 gebruik is. In die natter reënvaljare het die eenjarige grasse se toename daartoe gelei dat teenwoordigheid tussen die meerjarige grasse en die punt van versameling voorgekom het. Copyright: Gevolglik is baie meer van die eenjariges aangeteken. Dit terwyl die meerjarige grasse wel © 2018. Authors. Licensee: Die Suid- nog teenwoordig in die persele was. Dit maak die gevolgtrekking oor wat met die meerjarige Afrikaanse Akademie vir grasse gebeur het in absolute terme baie moeilik. Die tekorte aan personeel, tyd en begroting Wetenskap en Kuns. This het ongelukkig ’n groot impak op die manier van monitering. Dit is heel moontlik die rede work is licensed under waarom so min moniteringsdatastelle bestaan en nog minder gepubliseer word. the Creative Commons Attibution License. Sleutelwoorde: Plantegroei monitering, statistiese ontleding, lang termyn datastel, semi- ariede gebiede, kruidstratum. http://www.satnt.ac.za 1 Open Access Page 2 of 15 Oorspronklike Navorsing of such a combination of factors may persist for decades, Introduction as witnessed for bush encroachment and densification Savanna covers about 40% of Africa’s land surface (Cole in southern Africa following the 1960s drought or the 1986) and is used primarily for support of livestock or withdrawal of fire during high rainfall years suitable for wildlife based on indigenous vegetation (Barnes 1982). woody recruitment (O’Connor et al. 2014). Such increases Dominant plant growth forms of this biome include woody in woody cover further affect the herbaceous sward (Dye & plants (trees, shrubs), dwarf shrubs, graminoids, non- Spear 1982; Belsky et al. 1989; Smit 2004). graminoid monocotyledons and herbaceous dicotyledons (Mucina & Rutherford 2006), but herbaceous biomass is The herbaceous layer exhibits a wide range of life history dominated by grasses (Zietsman & Bezuidenhout 1999; types including long-lived perennials, biennials, and Parr et al. 2014). As a consequence, savanna functioning annuals, whose pattern of dynamics is intrinsically is determined largely by the relation between trees and different (Harper 1977). Success of annual species in semi- grasses (Sankaran et al. 2004) with, to date, the role of a arid southern African savanna is considered to depend conspicuous richness of forbs largely unrecognised (Clegg on receiving adequate rainfall during the early part of & O’Connor 2017). Effective use and management of the rainfall season so that there is sufficient time to attain this vegetation resource therefore requires an improved reproductive status; seeds may therefore be cued not to understanding of the influences which determine the germinate in the late rainy season (Veenendaal et al. 1996a, composition, structure, and dynamics of each. b). Species are also intrinsically different in their tolerance or response to specific environmental conditions. A species The primary determinants of savanna organisation are growing near its climatic optimum would not be expected water and nutrient availability (Frost et al. 1986; Wiegand to respond to inter-annual rainfall variability in the same et al. 1998). Water availability is a function of rainfall manner as one growing near the margin of its distribution. and water storage in soil profile determined by its depth Herbaceous species and functional groups, including and texture (Ritchie 1981). Nutrient availability is also dwarf shrubs, differ in their response to drought (O’Connor determined by soil texture, such that the dual effects 2015) and to variation in intra-seasonal pattern of rainfall of water and nutrient availability are confounded and (O’Connor & Roux 1995; Swemmer et al. 2007). Herbaceous cannot be separated (Foth 1990). Secondary determinants species respond differently to grazing, exemplified by their of savanna vegetation are fire and herbivory (Smit et al. increaser-decreaser classification and to fire (Tainton 1999). 2013), both grazing (Tainton 1999) and browsing (Belsky In summary, individualistic species responses should be 1984; Augustine & McNaughton 2004; Moe et al. 2009). expected to the many constellations of environmental Fire can potentially transform savanna structure because influences which may arise. of its effect on trees and shrubs (Van der Walt & Le Riche 1984; Seymour & Huyser 2008) but can also transform This paper addresses the influence of inter-annual herbaceous composition
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