Stöcklin Jürg, Schweizer Kathrin, Körner Christian
Institute of Botany, University of Basel, Schönbeinstrasse 6, CH-4056 Basel, Switzerland e-mail:
Oecologia. 1998 Aug;116(1-2):50-56. doi: 10.1007/s004420050562.
We investigated the effects of elevated CO (600 μl l vs 350 μl l) and phosphorus supply (1 g P m year vs unfertilized) on intact monoliths from species-rich calcareous grassland in a greenhouse. Aboveground community dry mass remained almost unaffected by elevated CO in the first year (+6%, n.s.), but was significantly stimulated by CO enrichment in year two (+26%, P<0.01). Among functional groups, only graminoids contributed significantly to this increase. The effect of phosphorus alone on community biomass was small in both years and marginally significant only when analyzed with MANOVA (+6% in year one, +9% in year two, 0.1 ≥P > 0.05). Belowground biomass and stubble after two seasons were not different in elevated CO and when P was added. The small initial increase in aboveground community biomass under elevated CO is explained by the fact that some species, in particular Carex flacca, responded very positively right from the beginning, while others, especially the dominant Bromus erectus, responded negatively to CO enrichment. Shifts in community composition towards more responsive species explain the much larger CO response in the second year. These shifts, i.e., a decline in xerophytic elements (B. erectus) and an increase in mesophytic grasses and legumes occurred independently of treatments in all monoliths but were accelerated significantly by elevated CO. The difference in average biomass production at elevated compared to ambient CO was higher when P was supplied (at the community level the CO response was enhanced from 20% to 33% when P was added, in graminoids from 17% to 27%, in legumes from 4% to 60%, and in C. flacca from 120% to 298% by year two). Based on observations in this and similar studies, we suggest that interactions between CO concentration, species presence, and nutrient availability will govern community responses to elevated CO.
我们在温室中研究了高浓度二氧化碳(600 μl l 对比 350 μl l)和磷供应(1 g P m² 年对比未施肥)对物种丰富的钙质草原完整土柱的影响。地上群落干质量在第一年几乎不受高浓度二氧化碳的影响(增加 6%,无显著差异),但在第二年受到二氧化碳富集的显著刺激(增加 26%,P<0.01)。在功能组中,只有禾本科植物对这种增加有显著贡献。单独的磷对群落生物量的影响在两年中都很小,仅在使用多变量方差分析时才略微显著(第一年增加 6%,第二年增加 9%,0.1 ≥P > 0.05)。两个季节后,高浓度二氧化碳处理和添加磷时的地下生物量和残茬没有差异。高浓度二氧化碳下地上群落生物量最初的小幅增加可以解释为,一些物种,特别是软苔草,从一开始就反应非常积极,而其他物种,尤其是优势种直立雀麦,对二氧化碳富集反应消极。群落组成向更敏感物种的转变解释了第二年对二氧化碳的更大反应。这些转变,即旱生元素(直立雀麦)减少,中生禾本科植物和豆科植物增加,在所有土柱中都独立于处理发生,但高浓度二氧化碳显著加速了这种转变。与环境二氧化碳相比,供应磷时高浓度二氧化碳下的平均生物量生产差异更大(在群落水平,添加磷时对二氧化碳的反应从 20%提高到 33%,在禾本科植物中从 17%提高到 27%,在豆科植物中从 4%提高到 60%,在软苔草中到第二年从 120%提高到 298%)。基于本研究及类似研究的观察结果,我们认为二氧化碳浓度、物种存在和养分有效性之间的相互作用将决定群落对高浓度二氧化碳的反应。