Arid
DOI10.1016/j.envexpbot.2017.02.014
Sulfur accumulation in gypsum-forming thiophores has its roots firmly in calcium
Robson, Thomas1; Stevens, Jason2,3; Dixon, Kingsley4; Reid, Nathan1
通讯作者Robson, Thomas
来源期刊ENVIRONMENTAL AND EXPERIMENTAL BOTANY
ISSN0098-8472
EISSN1873-7307
出版年2017
卷号137页码:208-219
英文摘要

Recent studies suggest sulfur-accumulators (thiophores and gypsophiles) produce foliar gypsum (CaSO4 center dot 2H(2)O) as a novel biomineralogical tolerance mechanism against sulfate salinity and excess soluble calcium (e.g. gypsic soil). However, little is known of the geochemical and ecophysiological aspects of foliar gypsum. The compositional, developmental (biomass, root development) and functional responses (photosystem performance and water relations), to soils with contrasting relative SO42- and Ca2+ pore-water concentrations (incl. a gypsum treatment), were examined in two gypsum-forming desert thiophores (Acacia bivenosa L. and A. ligulata A.Cunn. ex Benth.) and a sympatric non-thiophore comparator (A. ancistrocarpa Maiden & Blakely). Sulfur and calcium were accreted broadly as a function of the relative abundance of Ca2+ and SO42- ions in soil solution, and interspecific responses revealed thiophores are preferentially Ca accumulators, tending to maximise Ca uptake for the given conditions and scaling sulfate accumulation in relation to Ca, a co-regulation behaviour absent in the comparator. The thiophores were also sensitive to sulfur limitation, and these observations are consistent with cytosolic Ca2+ and SO42- regulation through gypsum precipitation. However, the gypsum-forming species were not comparatively tolerant to the gypsum treatment, most likely due to a lack of tolerance to limited P bioavailability resulting from the formation of sparingly-soluble calcium-phosphate soil minerals. The outcomes indicate that the capacity for gypsum biomineralisation does not, by itself, confer tolerance to the full suite of geochemical stress factors presented by gypsic soils (e.g. constrained P bioavailability). The findings steer future research towards testing alternative hypothesis pertaining to the ecophysiological basis of gypsum formation (e.g. osmoregulation) as well as examining whether obligate gypsophiles, which are also challenged by constrained P bioavailability, benefit by forming gypsum biominerals. (C) 2017 Elsevier B.V. All rights reserved.


英文关键词Biomineralisation Element accumulator Gypsum Gypsophile Thiophore Sulfur Phytoremediation
类型Article
语种英语
国家Australia
收录类别SCI-E
WOS记录号WOS:000398752400018
WOS关键词SULFATE ASSIMILATION ; SOIL ; PHOSPHORUS ; PLANTS ; GROWTH ; DEFICIENCY ; NUTRITION ; NITROGEN ; NITRATE ; INDICATORS
WOS类目Plant Sciences ; Environmental Sciences
WOS研究方向Plant Sciences ; Environmental Sciences & Ecology
来源机构Commonwealth Scientific and Industrial Research Organisation ; University of Western Australia
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/198628
作者单位1.CSIRO Mineral Resources, 26 Dick Perry Ave, Kensington, NSW 6101, Australia;
2.Bot Gardens & Pk Author, Biodivers & Conservat Ctr, Fraser Ave, Kings Pk, WA 6005, Australia;
3.Univ Western Australia, Sch Plant Biol, Stirling Highway, Crawley, WA 6009, Australia;
4.Curtin Univ, Sch Sci, Dept Environm & Agr, GPO Box U1987, Perth, WA, Australia
推荐引用方式
GB/T 7714
Robson, Thomas,Stevens, Jason,Dixon, Kingsley,et al. Sulfur accumulation in gypsum-forming thiophores has its roots firmly in calcium[J]. Commonwealth Scientific and Industrial Research Organisation, University of Western Australia,2017,137:208-219.
APA Robson, Thomas,Stevens, Jason,Dixon, Kingsley,&Reid, Nathan.(2017).Sulfur accumulation in gypsum-forming thiophores has its roots firmly in calcium.ENVIRONMENTAL AND EXPERIMENTAL BOTANY,137,208-219.
MLA Robson, Thomas,et al."Sulfur accumulation in gypsum-forming thiophores has its roots firmly in calcium".ENVIRONMENTAL AND EXPERIMENTAL BOTANY 137(2017):208-219.
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