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Estimating impacts of lichens and bryophytes on global biogeochemical cycles

机译:估算地衣和苔藓植物对全球生物地球化学循环的影响

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Lichens and bryophytes may significantly affect global biogeochemical cycles by fixation of nitrogen and biotic enhancement of surface weathering rates. Most of the studies suggesting these effects, however, are either conceptual or rely on upscaling of regional estimates to obtain global numbers. Here we use a different method, based on estimates of net carbon uptake, to quantify the impacts of lichens and bryophytes on biogeochemical cycles at the global scale. We focus on three processes, namely, nitrogen fixation, phosphorus uptake, and chemical weathering. Our estimates have the form of potential rates, which means that we quantify the amount of nitrogen and phosphorus needed by the organisms to build up biomass, also accounting for resorption and leaching of nutrients. Subsequently, we use potential phosphorus uptake on bare ground to estimate chemical weathering by the organisms, assuming that they release weathering agents to obtain phosphorus. The predicted requirement for nitrogen ranges from 3.5 to 34 Tg yr~(-1) and for phosphorus it ranges from 0.46 to 4.6 Tg yr~(-1). Estimates of chemical weathering are between 0.058 and 1.1 km~3 yr~(-1) of rock. These values seem to have a realistic order of magnitude, and they support the notion that lichens and bryophytes have the potential to play an important role for biogeochemical cycles.
机译:地衣和苔藓植物可能通过固氮和生物提高表面风化率而严重影响全球生物地球化学循环。但是,大多数表明这些影响的研究要么是概念性的,要么是依靠扩大区域估计数以获得全球数字。在这里,我们使用基于净碳吸收量估算的另一种方法来量化地衣和苔藓植物对全球范围内生物地球化学循环的影响。我们专注于三个过程,即固氮,吸收磷和化学风化。我们的估计采用潜在速率的形式,这意味着我们可以量化生物体建立生物量所需的氮和磷的量,还应考虑营养物的吸收和浸出。随后,假设生物体释放出耐候剂以获得磷,则我们利用裸露在地面上的潜在磷吸收量来估算生物体的化学耐候性。预测的氮需求量为3.5至34 Tg yr〜(-1),磷的需求量为0.46至4.6 Tg yr〜(-1)。化学风化作用的估计值在岩石的0.058至1.1 km〜3 yr〜(-1)之间。这些值似乎具有现实的数量级,并且它们支持地衣和苔藓植物有潜力在生物地球化学循环中发挥重要作用的观点。

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