Y. Nakanishi, Tatsuma Matsutani, K. Hinokidani, T. Nagai, Mami Irie
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引用次数: 2
摘要
铁在红树林土壤中的增溶作用与枯叶凋落物中浸出的多酚有关,可以提高铁的生物利用度。在这种情况下,红树林蟹的脱叶过程会增加红树林叶片中多酚与土壤中铁的反应频率。在本研究中,我们研究了脱叶蟹(Neosarmatium smithi)在铁溶解过程中的生态作用。当落叶被螃蟹带到它们的洞穴并被它们吃掉后,多酚可能会留在它们的粪便中。如果是这样,粪便中的多酚类物质与红树林土壤的接触可以促进土壤中溶解铁的析出。为了证明这一假设,我们首先调查了蟹洞中黑色部分的出现比例,并测量了史密斯黑斑蟹粪便和黑色部分土壤中的总酚含量。在此基础上,研究了蟹粪对红树林土壤中溶解铁的影响。结果表明,洞中黑色部分的出现率为67%,洞中粪便、黑色部分和黄色部分的酚含量分别为9.93、0.49和0.12 mg g−1。土壤+粪便水提物溶液中溶解铁的含量为0.65 μ g g−1,是土壤+蒸馏水溶液的4.5倍。我们认为,粪便中残留的多酚通过铁还原和螯合特性影响了不溶性铁的溶解。
A role of a herbivorous crab, Neosarmatium smithi, in dissolved iron elution from mangrove ecosystems
Iron solubilization in mangrove soils associated with polyphenols leached out from leaf-litter can improve iron bioavailability. In this context, the leaf-removing process by mangrove crabs would increase reacting frequency of the polyphenols in mangrove leaves with iron in the soils. In this study, we investigated ecological roles of a leaf-removing crab, Neosarmatium smithi , on the iron solubilization process. After the fallen leaves carried by the crabs to their burrows and eaten by them, polyphenols may be remained in their feces. If so, contact of polyphenols in the feces with mangrove soils could promote elution of dissolved iron from the soils. In order to demonstrate this hypothesis, we firstly surveyed the appearance ratio of the black part in crab burrows and measured total phenolic content in feces of N. smithi as well as in the black part soil. Then, we examined influences of the crab feces on dissolved iron elution from mangrove soils. As the results, the appearance ratio of the black part in the burrow was 67 % and the phenolic content in the feces, the black part, and the yellow part in crab burrows were 9.93, 0.49, and 0.12 mg g − 1 , respectively. Dissolved iron content in the solution (soil + water extract from feces) was 0.65 μ g g − 1 and this content was 4.5 times higher than the control (soil + distilled water). We suggest that the polyphenols remained in the feces affect to solubilize insoluble forms of iron by iron reduction and chelating properties.