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首页> 外文期刊>Aquatic Microbial Ecology >Carbon release and cycling within epilithic biofilms in two contrasting headwater streams
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Carbon release and cycling within epilithic biofilms in two contrasting headwater streams

机译:两种截然不同的源头水流中的表层生物膜中的碳释放和循环

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摘要

This study investigates the release of dissolved organic carbon (DOC) from epilithic biofilms and how the exchange of C between epilithic algae and bacteria varies between 2 contrasting headwater streams, During 3 seasons, light and dark enclosures were incubated in situ with rock substrate and stream water amended with C-13-labeled bicarbonate to follow newly fixed carbon into DOC, epilithic biofilm, and biofilm phospholipid fatty acids (PLFAs). Net release of DOC only occurred in the light enclosures and was significantly affected by net primary production (NPP). However, the net release of DOC as a proportion of NPP increased with light availability and decreased with dissolved inorganic nitrogen in Huey Hollow, the nutrient-deplete stream, and decreased with dissolved inorganic phosphorus (DIP) in Moore Creek, the nutrient-replete stream. Newly-fixed C, released as DOC, decreased with DIP but represented a greater proportion of net DOC release in Moore Creek (6 to 15 %) relative to that in Huey Hollow (0.7 to 2 %). Congruently, the quantity of newly-fixed C retained in the bulk biofilm and the bacterial PLFA ia15:0 increased together with DIP. Further, the proportion of NPP incorporated into bacterial PLFA in Huey Hollow was 4 times that in the Moore Creek biofilms, suggesting that bacteria accessed relatively more NPP in the low nutrient stream biofilms. Our data indicate that C-cycling differed between the contrasting streams in 2 significant ways. A larger proportion of DOC released from biofilms in the nutrient-rich stream was derived from new photosynthates, reducing the availability of this source of NPP to biofilm bacteria. Concurrently, a greater proportion of NPP was retained in heterotrophic bacterial PLFAs in the more nutrient-deplete stream biofilms. These results suggest that nutrient levels can greatly affect the source and processing of DOC, and emphasize the need to understand the mechanisms responsible for varied DOC cycling and transport in streams.
机译:这项研究调查了表层生物膜中溶解有机碳(DOC)的释放以及表层藻类和细菌之间的C交换如何在2条相反的源水之间变化。在3个季节中,将浅色和深色围墙与岩石基质和溪流进行原位保温将水用C-13标记的碳酸氢盐修正,以将新固定的碳跟随到DOC,上层生物膜和生物膜磷脂脂肪酸(PLFA)中。 DOC的净释放仅发生在灯罩中,并且受到净初级生产(NPP)的显着影响。然而,DOC的净释放量与NPP的比例随着光的可用性而增加,并随着养分流Huey Hollow中的溶解性无机氮而降低,而随着养分流Moore Creek中的溶解性无机磷(DIP)降低。 。新固定的C以DOC的形式释放,随DIP的增加而降低,但相对于Huey Hollow的净DOC释放量(0.7%到2%),在Moore Creek中净释放的DOC所占比例更大(6%到15%)。一致地,保留在主体生物膜和细菌PLFA ia15:0中的新固定C的数量与DIP一起增加。此外,在Huey Hollow的细菌PLFA中掺入的NPP比例是Moore Creek生物膜的4倍,这表明细菌在低养分流生物膜中获得的NPP相对较多。我们的数据表明,对比流之间的C循环在2个重要方面有所不同。在营养丰富的流中,从生物膜释放的DOC的大部分来自新的光合产物,从而减少了这种NPP来源对生物膜细菌的利用。同时,更多养分流生物膜中的异养细菌PLFA中保留了更大比例的NPP。这些结果表明,营养水平可以极大地影响DOC的来源和加工,并强调需要了解导致DOC循环变化和流中运输的机理。

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