Multiphase Chemistry Department, Max Planck Institute for Chemistry, Hahn-Meitner-Weg 1, 55128 Mainz, Germany.
Öko-Log Freilandforschung, Hauptstrasse 181, 67705 Trippstadt, Germany.
Sci Total Environ. 2017 May 15;586:1287-1297. doi: 10.1016/j.scitotenv.2017.02.141. Epub 2017 Feb 21.
Dryland vegetation developed morphological and physiological strategies to cope with drought. However, as aridity increases, vascular plant coverage gets sparse and microbially-dominated surface communities (MSC), comprising cyanobacteria, algae, lichens and bryophytes together with heterotropic bacteria, archaea and fungi, gain relevance. Nevertheless, the relevance of MSC net primary productivity has only rarely been considered in ecosystem scale studies, and detailed information on their contribution to the total photosynthetic biomass reservoir is largely missing. In this study, we mapped the spatial distribution of two different MSC (biological soil crusts and quartz fields hosting hypolithic crusts) at two different sites within the South African Succulent Karoo (Soebatsfontein and Knersvlakte). Then we characterized both types of MSC in terms of chlorophyll content, and combining these data with the biocrust and quartz field maps, we estimated total biomass values of MSCs and their spatial patterns within the two different ecosystems. Our results revealed that MSC are important vegetation components of the South African Karoo biome, revealing clear differences between the two sites. At Soebatsfontein, MSC occurred as biological soil crusts (biocrusts), which covered about one third of the landscape reaching an overall biomass value of ~480gha of chlorophyll a+b at the landscape scale. In the Knersvlakte, which is characterized by harsher environmental conditions (i.e. higher solar radiation and potential evapotranspiration), MSC occurred as biocrusts, but also formed hypolithic crusts growing on the lower soil-immersed parts of translucent quartz pebbles. Whereas chlorophyll concentrations of biocrusts and hypolithic crusts where insignificantly lower in the Knersvlakte, the overall MSC biomass reservoir was by far larger with ~780gha of chlorophyll a+b. Thus, the complementary microbially-dominated surface communities promoted biomass formation within the environmentally harsh Knersvlakte ecosystem.
旱地植被发展了形态和生理策略来应对干旱。然而,随着干旱程度的增加,维管束植物的覆盖率变得稀疏,微生物主导的表面群落(MSC)变得更加重要,包括蓝细菌、藻类、地衣和苔藓,以及异养细菌、古菌和真菌。然而,在生态系统尺度的研究中,很少考虑 MSC 的净初级生产力的相关性,并且关于它们对总光合生物量库的贡献的详细信息在很大程度上是缺失的。在这项研究中,我们在南非肉质喀拉哈里的两个不同地点(Soebatsfontein 和 Knersvlakte)绘制了两种不同 MSC(生物土壤结皮和含有隐花结皮的石英地)的空间分布。然后,我们根据叶绿素含量对这两种类型的 MSC 进行了特征描述,并将这些数据与生物结皮和石英地的地图结合起来,我们估计了 MSC 的总生物量值及其在两个不同生态系统中的空间模式。我们的结果表明,MSC 是南非喀拉哈里生物群落的重要植被组成部分,这两个地点之间存在明显的差异。在 Soebatsfontein,MSC 表现为生物土壤结皮(biocrusts),覆盖了大约三分之一的景观,在景观尺度上达到了约 480gha 的叶绿素 a+b 的总生物量值。在 Knersvlakte,环境条件更为恶劣(即更高的太阳辐射和潜在蒸散量),MSC 表现为生物结皮,但也形成了在半透明石英卵石的下部土壤淹没部分生长的隐花结皮。虽然 Knersvlakte 中生物结皮和隐花结皮的叶绿素浓度没有显著降低,但 MSC 的总生物量库要大得多,约为 780gha 的叶绿素 a+b。因此,互补的微生物主导的表面群落促进了环境恶劣的 Knersvlakte 生态系统中生物量的形成。