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觅食的蜜蜂带来的无机氮可能对它们所访问的植物具有适应性益处。

Inorganic nitrogen derived from foraging honey bees could have adaptive benefits for the plants they visit.

机构信息

Department of Crop & Soil Sciences, the University of Georgia, Athens, Georgia, United States of America.

出版信息

PLoS One. 2013 Jul 29;8(7):e70591. doi: 10.1371/journal.pone.0070591. Print 2013.

DOI:10.1371/journal.pone.0070591
PMID:23923006
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3726636/
Abstract

In most terrestrial ecosystems, nitrogen (N) is the most limiting nutrient for plant growth. Honey bees may help alleviate this limitation because their feces (frass) have high concentration of organic nitrogen that may decompose in soil and provide inorganic N to plants. However, information on soil N processes associated with bee frass is not available. The objectives of this work were to 1) estimate the amount of bee frass produced by a honey bee colony and 2) evaluate nitrogen mineralization and ammonia volatilization from bee frass when surface applied or incorporated into soil. Two cage studies were conducted to estimate the amount of frass produced by a 5000-bee colony, and three laboratory studies were carried out in which bee frass, surface-applied or incorporated into soil, was incubated at 25(o)C for 15 to 45 days. The average rate of bee frass production by a 5,000-bee colony was estimated at 2.27 to 2.69 g N month(-1). Nitrogen mineralization from bee frass during 30 days released 20% of the organic N when bee frass was surface applied and 34% when frass was incorporated into the soil. Volatilized NH3 corresponded to 1% or less of total N. The potential amount of inorganic N released to the soil by a typical colony of 20,000 bees foraging in an area similar to that of the experimental cages (3.24 m(2)) was estimated at 0.62 to 0.74 g N m(-2) month(-1) which may be significant at a community scale in terms of soil microbial activity and plant growth. Thus, the deposition of available N by foraging bees could have adaptive benefits for the plants they visit, a collateral benefit deriving from the primary activity of pollination.

摘要

在大多数陆地生态系统中,氮(N)是限制植物生长的最主要营养物质。蜜蜂可能有助于缓解这种限制,因为它们的粪便(蜂蜡)含有高浓度的有机氮,这些氮可能在土壤中分解,并为植物提供无机氮。然而,有关与蜜蜂蜂蜡相关的土壤氮过程的信息尚不清楚。本研究的目的是:1)估计一个蜜蜂群体产生的蜜蜂蜂蜡量;2)评估蜜蜂蜂蜡表面施用到土壤或掺入土壤后氮的矿化和氨挥发。进行了两项笼养研究来估计一个 5000 只蜜蜂群体产生的蜂蜡量,进行了三项实验室研究,其中将蜜蜂蜂蜡表面施用到土壤或掺入土壤中,在 25°C 下孵育 15 至 45 天。一个 5000 只蜜蜂群体的蜜蜂蜂蜡平均产生速率估计为 2.27 至 2.69 g N 月(-1)。在 30 天内,当蜂蜡表面施用时,20%的有机氮从蜂蜡中矿化,当蜂蜡掺入土壤时,34%的有机氮矿化。挥发的 NH3 相当于总氮的 1%或更少。在实验笼类似的区域(3.24 m(2))觅食的 20000 只蜜蜂典型群体向土壤释放的无机 N 量估计为 0.62 至 0.74 g N m(-2)月(-1),就土壤微生物活性和植物生长而言,这在群落尺度上可能具有重要意义。因此,觅食蜜蜂沉积的可用氮可能对它们所访问的植物具有适应性益处,这是传粉这一主要活动的附带好处。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4714/3726636/d5ff36bec157/pone.0070591.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4714/3726636/d5ff36bec157/pone.0070591.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4714/3726636/d5ff36bec157/pone.0070591.g001.jpg

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