Sorochkina Kira, Strauss Sarah L, Inglett Patrick W
Department of Soil and Water Sciences, University of Florida, Gainesville, FL, United States.
Southwest Florida Research and Education Center, University of Florida, Immokalee, FL, United States.
Front Microbiol. 2022 Aug 3;13:892266. doi: 10.3389/fmicb.2022.892266. eCollection 2022.
Biocrusts are communities of microorganisms within the top centimeter of soil, often dominated by phototrophic dinitrogen-fixing (N-fixing) organisms. They are common globally in arid ecosystems and have recently been identified in agroecosystems. However, unlike natural ecosystem biocrusts, agroecosystem biocrusts receive regular fertilizer and irrigation inputs. These inputs could influence seasonal biocrust N-fixation and their relationship with soil nutrients in perennial agroecosystems, which is of particular interest given crop management requirements. In this study, biocrust and adjacent bare soil N-fixation activity was measured in the field during the summer, fall, spring, and winter seasons in a Florida citrus orchard and vineyard using both acetylene reduction assays and N incubations. Samples were analyzed for microbial and extractable carbon (MBC, EC), nitrogen (MBN, EN), and phosphorus (MBP, EP). In both agroecosystems, biocrusts had greater microbial biomass and extractable nutrients compared to bare soil. The citrus and grape biocrusts were both actively fixing N, despite crop fertilization, with rates similar to those found in natural arid and mesic systems, from 0.1 to 142 nmol of CH g of biocrust dry weight h (equivalent to 1-401 μmol mh). Lower soil temperatures and higher EC:EN ratios were associated with higher N-fixation rates in citrus biocrusts, while higher soil moisture and higher EP were associated with higher N-fixation rates in grape biocrusts. The N-fixation activity of these agroecosystem biocrusts indicates the possibility of biocrusts to enhance N cycling in perennial agroecosystems, with potential benefits for crop production.
生物结皮是土壤表层一厘米内的微生物群落,通常以光合固氮生物为主。它们在全球干旱生态系统中很常见,最近在农业生态系统中也被发现。然而,与自然生态系统生物结皮不同,农业生态系统生物结皮会定期接受肥料和灌溉投入。这些投入可能会影响多年生农业生态系统中生物结皮的季节性固氮作用及其与土壤养分的关系,鉴于作物管理要求,这一点尤为重要。在本研究中,利用乙炔还原法和氮培养法,在佛罗里达州一个柑橘园和葡萄园的夏季、秋季、春季和冬季实地测量了生物结皮和相邻裸土的固氮活性。对样品进行了微生物和可提取碳(MBC、EC)、氮(MBN、EN)和磷(MBP、EP)的分析。在这两种农业生态系统中,与裸土相比,生物结皮具有更高的微生物生物量和可提取养分。尽管作物施肥,但柑橘和葡萄生物结皮都在积极固氮,其速率与自然干旱和半湿润系统中的速率相似,为每克生物结皮干重每小时0.1至142纳摩尔的CH(相当于1 - 401微摩尔每小时)。较低的土壤温度和较高的EC:EN比值与柑橘生物结皮较高的固氮率相关,而较高的土壤湿度和较高的EP与葡萄生物结皮较高的固氮率相关。这些农业生态系统生物结皮的固氮活性表明,生物结皮有可能增强多年生农业生态系统中的氮循环,对作物生产具有潜在益处。