Tamilselvi S M, Thiyagarajan Chitdeshwari, Uthandi Sivakumar
Biocatalysts Lab, Department of Agricultural Microbiology, Tamil Nadu Agricultural University Coimbatore, India.
Department of Soil Science and Agricultural Chemistry, Tamil Nadu Agricultural University Coimbatore, India.
Front Plant Sci. 2016 Dec 8;7:1828. doi: 10.3389/fpls.2016.01828. eCollection 2016.
Assessing the ability of soil microorganisms to dissolute poorly soluble native calcite to supply Ca is a new area to be explored in reclaiming sodic soils by supplying adequate Ca and reducing the recurrent sodicity. Hence, the present study aimed to isolate a calcite dissolving bacteria (CDB) from calcareous sodic soils and to understand the mechanism of calcite dissolution. Of the 33 CDB isolates recovered from the calcareous sodic soils of Tamil Nadu (Coimbatore, Ramnad, and Trichy), 11 isolates were screened for calcite dissolution based on titratable acidity. 16S rRNA gene sequence analysis of the three best isolates ., SORI09, SOTI05, and SOTI06 revealed 99% similarity to , 100% to , and 93% to sp., respectively. Among them, sp. SOTI06 released more Ca (3.6 g.l) by dissolving 18.6% of the native calcite. The spectral data of FTIR also showed reduction in the intensity of calcite (55.36-41.27) by the isolate at a wave number of 1636 cm which confirmed the dissolution. Besides producing organic acids (gluconic acid and acetic acid), sp. SOTI06 also produced siderophore (91.6%) and extracellular polysaccharides (EPS, 13.3 μg. ml) which might have enhanced the calcite dissolution.
评估土壤微生物溶解难溶性天然方解石以供应钙的能力,是在通过供应充足的钙和降低反复出现的碱化度来改良苏打土壤方面有待探索的新领域。因此,本研究旨在从石灰性苏打土壤中分离出一种方解石溶解细菌(CDB),并了解方解石溶解的机制。从泰米尔纳德邦(哥印拜陀、拉马纳德和蒂鲁吉拉伯利)的石灰性苏打土壤中回收的33株CDB分离株中,基于可滴定酸度筛选了11株分离株对方解石的溶解情况。对三株最佳分离株SORI09、SOTI05和SOTI06进行的16S rRNA基因序列分析显示,它们分别与 、 和 sp.的相似性为99%、100%和93%。其中,SOTI06菌株通过溶解18.6%的天然方解石释放了更多的钙(3.6 g·l)。傅里叶变换红外光谱(FTIR)的光谱数据也显示,该分离株在1636 cm波数处使方解石的强度(55.36 - 41.27)降低,这证实了溶解过程。除了产生有机酸(葡萄糖酸和乙酸)外,SOTI06菌株还产生了铁载体(91.6%)和细胞外多糖(EPS,13.3 μg·ml),这可能增强了方解石的溶解。