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首页> 外文期刊>Aquatic Microbial Ecology >Sediment properties and bacterial community in burrows of the ghostshrimp Pestarella tyrrhena (Decapoda: Thalassinidea)
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Sediment properties and bacterial community in burrows of the ghostshrimp Pestarella tyrrhena (Decapoda: Thalassinidea)

机译:鬼虾Pestarella tyrrhena(十足纲:Thalassinidea)的洞穴中的沉积物特征和细菌群落

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Chemical properties of burrow wall sediment from burrows of the thalassinidean shrimp Pestarella (=Callianassa) tyrrhena located at Vravrona Bay (Aegean Sea, Greece) were studied and found to be very different from the sediment surface and ambient anoxic sediment. P. tyrrhena burrow walls had significantly higher amounts of silt and clay, while total organic carbon (TOC) was up to 6 times higher than in surrounding sediment. Chlorophyll a (chl a) accounted for a small fraction of TOC and showed similar values in burrow walls and surface sediment, whereas the low chl a: chl a + phaeopigment ratio indicated the presence of more fresh material in the latter. Biopolymers (carbohydrates, proteins and lipids) were 4 to 11 times higher in burrow walls than in the surrounding sediment, accounting for 47% of TOC. The low protein:carbohydrate ratio indicated that the high TOC in the burrow walls was caused by the presence of aged detritus of low nutritional quality, such as seagrass detritus. The distinct conditions along the burrow wall also affected the bacterial community and resulted in a 10-fold increase of bacterial abundance. Molecular fingerprints of the bacterial communities showed that the bacterial composition of the burrow wall was more similar to the ambient anoxic sediment and showed less seasonal change than the sediment surface. These results suggest that burrow walls have distinct properties and should not be considered merely as a simple extension of the sediment surface.
机译:研究了位于Vravrona湾(希腊爱琴海)的海藻虾虾Pestarella(= Callianassa)tyrrhena的洞穴的洞穴壁沉积物的化学性质,发现其与沉积物表面和周围缺氧沉积物有很大不同。 tyrrhena洞穴壁的泥沙和粘土含量明显较高,而总有机碳(TOC)则比周围沉积物高出6倍。叶绿素a(chl a)占TOC的一小部分,并且在洞穴壁和表面沉积物中显示出相似的值,而较低的chl a:chl a +色素沉着比表明后者中存在更多新鲜物质。洞穴壁中的生物聚合物(碳水化合物,蛋白质和脂质)比周围的沉积物高4至11倍,占TOC的47%。低的蛋白质:碳水化合物比率表明,洞穴壁中的高TOC是由于存在营养质量低下的老化碎屑(例如海草碎屑)引起的。沿洞穴壁的独特条件也影响了细菌群落,并导致细菌丰度增加了10倍。细菌群落的分子指纹显示,洞穴壁的细菌组成与环境缺氧沉积物更相似,并且与沉积物表面相比,季节变化较小。这些结果表明,洞穴壁具有独特的性质,不应仅视为沉积物表面的简单延伸。

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