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Spatial variation in potential photosynthesis in Northern European bogs

机译:北欧沼泽中潜在光合作用的空间变化

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QuestionMeasurements of ecosystem carbon (C) exchange are usually labour-intensive and expensive. In peatlands, these temporally and spatially limited measurements are often up-scaled over comparable ecosystems, such as ombrotrophic bogs, to provide an estimate for ecosystem level carbon dioxide (CO2) fluxes. Peatlands typically have moisture variations reflected in the presence of microforms (e.g. hummocks and hollows), each with characteristic plant life forms. However, so far the applicability of peatland type (e.g. bog, fen) or microforms for up-scaling has not been assessed. Does the vegetation composition or function of associated species differ so greatly between the same types of peatland that up-scaling is impossible?
机译:问题对生态系统碳交换的测量通常是劳动密集型的且昂贵的。在泥炭地,这些时间和空间有限的测量值通常在可比生态系统(如营养营养沼泽)上进行了放大,以估算生态系统水平的二氧化碳(CO2)通量。泥炭地的水分变化通常反映在微形态的存在下(例如,山岗和空心),每种形态都有独特的植物生命形式。但是,到目前为止,尚未评估泥炭地类型(例如沼泽,芬)或微缩模型在扩大规模方面的适用性。同一类型的泥炭地之间的植被组成或相关物种的功能差异是否如此之大,以至于无法扩大规模?

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