Department of Biology, Research Group of Plant and Vegetation Ecology, University of Antwerp, Belgium.
Ecology. 2011 Mar;92(3):633-44. doi: 10.1890/10-0822.1.
The Arctic experiences a high-radiation environment in the summer with 24-hour daylight for more than two months. Damage to plants and ecosystem metabolism can be muted by overcast conditions common in much of the Arctic. However, with climate change, extreme dry years and clearer skies could lead to the risk of increased photoxidation and photoinhibition in Arctic primary producers. Mosses, which often exceed the NPP of vascular plants in Arctic areas, are often understudied. As a result, the effect of specific environmental factors, including light, on these growth forms is poorly understood. Here, we investigated net ecosystem exchange (NEE) at the ecosystem scale, net Sphagnum CO2 exchange (NSE), and photoinhibition to better understand the impact of light on carbon exchange from a moss-dominated coastal tundra ecosystem during the summer season 2006. Sphagnum photosynthesis showed photoinhibition early in the season coupled with low ecosystem NEE. However, later in the season, Sphagnum maintained a significant CO2 uptake, probably for the development of subsurface moss layers protected from strong radiation. We suggest that the compact canopy structure of Sphagnum reduces light penetration to the subsurface layers of the moss mat and thereby protects the active photosynthetic tissues from damage. This stress avoidance mechanism allowed Sphagnum to constitute a significant percentage (up to 60%) of the ecosystem net daytime CO2 uptake at the end of the growing season despite the high levels of radiation experienced.
北极地区在夏季有长达两个月的 24 小时白昼,辐射水平很高。云层覆盖的情况在北极地区很常见,这可以减轻对植物和生态系统代谢的破坏。然而,随着气候变化,极端干旱年份和更晴朗的天空可能会导致北极初级生产者的光氧化和光抑制风险增加。苔藓通常在北极地区的植被净初级生产力(NPP)中占很大比重,但它们的研究却相对较少。因此,包括光在内的特定环境因素对这些生长形式的影响知之甚少。在这里,我们研究了生态系统尺度上的净生态系统交换(NEE)、净泥炭 CO2 交换(NSE)和光抑制,以更好地了解在 2006 年夏季,光照对以苔藓为主的沿海冻原生态系统中碳交换的影响。在季节早期,泥炭光合作用就表现出了光抑制,同时生态系统 NEE 也很低。然而,在季节后期,泥炭仍然保持着显著的 CO2 吸收量,这可能是由于下面苔藓层的发育,从而免受强烈辐射的影响。我们认为,泥炭的紧密树冠结构减少了光的穿透深度,到达苔藓垫的下层,从而保护了活跃的光合组织免受损害。这种避免胁迫的机制使得泥炭在生长季节结束时,尽管经历了高辐射水平,但仍能构成生态系统净白天 CO2 吸收的重要部分(高达 60%)。