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Impact of Pestarella tyrrhena on benthic metabolism in sediment microcosms enriched with seagrass and macroalgal detritus

机译:葛根粉对富含海草和大型藻类碎屑的沉积物微观底栖生物代谢的影响

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The impact of Pestarella (= Callianasa) tyrrhena (Decapoda: Thalassinidea), a common burrowing shrimp in the Mediterranean Sea on sediment-water fluxes (O_2, TCO_2, NH_4~+ and NO_3~-+ NO_2~-), sediment characteristics (organic matter, chlorophyll a) and porewater solutes (TCO_2, NH_4~+ and NO_3~- + NO_2~-) was investigated in laboratory microcosms over a period of 42 d. Microcosms containing homogenised fine sandy sediment were amended with either dead Posidonia oceanica leaves or fresh Ulva lactuca thalli. Reworking activity by the animal resulted in a rapid burial of surface deposited organic matter into the sediment. Porewater profiles of both TCO_2 and NH_4~+ indicated that P. tyrrhena activities result in a significant flushing of porewater solutes. Total sediment metabolism and carbon mineralisation were enhanced in the presence of P. tyrrhena. Metabolism of P. tyrrhena individuals was approximately 3 times higher in Ulva-amended sediment, probably due to a high activity level when nutritious food sources are in excess. Accordingly, animal respiration explained approximately half of the total enhancement in Ulva-amended sediment, while microbial decomposition of refractory seagrass detritus contributed about 4 times more to the stimulated carbon mineralisation than animal respiration. Despite the higher initial addition of carbon in Posidorna-amended sediment compared to Ulva-amended sediment, the amount of excess carbon mineralised was 4.7 times higher in the latter, indicating that mineralisation processes depend on the degradability rather than the quantity of the organic pool. Although P. tyrrhena excretion constituted only a minor part of the total nitrogen mineralised, macrofaunal activities were the major factor affecting total nitrogen mineralisation, and not the enrichment with organic matter.
机译:地中海常见的穴居虾虾(Pestarella tyrrhena(= Callianasa)tyrrhena(Decapoda:Thalassinidea))对沉积物水通量(O_2,TCO_2,NH_4〜+和NO_3〜-+ NO_2〜-),沉积物特征(有机)的影响在实验室缩影中对物质,叶绿素a)和孔隙水溶质(TCO_2,NH_4〜+和NO_3〜-+ NO_2〜-)进行了为期42天的研究。含有均质细沙质沉积物的缩影可以用死去的波塞冬藻叶子或新鲜的Ulva lactuca thalli进行修饰。动物的返工活动导致表面沉积的有机物快速埋入沉积物中。 TCO_2和NH_4〜+的孔隙水特征表明,痢疾假单胞菌的活动导致孔隙水溶质的大量冲洗。鼠李假单胞菌的存在增加了总沉积物的代谢和碳矿化作用。在被Ulva改良的沉积物中,P。tyrrhena个体的代谢大约高出3倍,这可能是由于营养丰富的食物来源过多时活动水平高所致。因此,动物呼吸作用解释了Ulva改良沉积物中总增强作用的一半,而难降解海草碎屑的微生物分解对受刺激的碳矿化的贡献是动物呼吸作用的约4倍。尽管在Posidorna修正的沉积物中初始碳的添加量比Ulva修正的沉积物中更高,但后者的矿化过量碳量是后者的4.7倍,这表明矿化过程取决于可降解性而不是有机池的数量。尽管tyrrhena排泄物仅占总氮矿化的一小部分,但大型动物活动是影响总氮矿化的主要因素,而不是有机质富集的主要因素。

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