渗漏和喷口生物的稳定同位素分配:化学和生态学意义

M.C. Kennicutt II , R.A. Burke Jr. , I.R. MacDonald , J.M. Brooks , G.J. Denoux , S.A. Macko
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引用次数: 114

摘要

汇编和解释了7年来在渗漏点和喷口处获得的数百个稳定同位素比率(C、N和S)。来源于碳的化学合成固定的组织的稳定同位素组成反映了化学和生物过程之间复杂的相互作用。利用还原硫的双壳类生物的稳定同位素组成表明,海水和/或排气水溶无机碳(DIC)是它们化学合成过程中的主要碳来源。所有研究的硫营养型双壳类动物似乎都具有类似的硫化物氧化代谢。甲烷营养贻贝组织的δ13C值与利用甲烷的δ13C值接近。显然,与甲烷化有关的动力学同位素分馏很少在宿主组织中表达。Vestimentiferan碳同位素组成反映了碳限制和利用底物的同位素组成。排放口组δ 13c值受碳限制的影响较大,而渗漏组δ 13c值则反映了孔隙水DIC同位素组成的变化。稳定的氮同位素组成与氮(N2)固定一致,但负责固氮的酶——固氮酶的存在尚未得到最终证实。各种氮源[N2, NH4+, PON(颗粒有机氮),DON(溶解有机氮)和NO4−]可以被喷口和渗漏生物利用。然而,δ15N数据表明,氮代谢机制不是物种或共生体类型的功能。硫是喷口和渗漏环境中的关键元素,硫营养是主要的化学合成活动。硫的来源在数量和同位素组成上变化很大,但几乎总是与细菌活动有关,要么是自由生活的,要么是共生的。氮和硫的营养需求似乎来源于各种各样的来源。来自异养和化学自养的营养的相对重要性取决于化学环境和动物生理。稳定的同位素组成提供了对这些不同代谢策略的见解;然而,要解决基本的生态问题,需要对无机和有机底物的浓度和同位素组成进行完整的清查,并进行支持的生化、酶和观察研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Stable isotope partitioning in seep and vent organisms: chemical and ecological significance

Several hundred stable isotopic ratios (C, N and S) acquired over seven years of investigations at both seep and vent locations are compiled and interpreted. The stable isotopic compositions of tissues derived from the chemosynthetic fixation of carbon reflect a complex interaction between chemical and biological processes. The stable isotopic composition of bivalves that utilize reduced sulfur suggests that seawater-and/or vent water-dissolved inorganic carbon (DIC) is their primary source of carbon during chemosynthesis. All thiotrophic bivalves studied appear to possess a similar sulfide oxidation metabolism. The δ13C-values of tissues from methanotrophic mussels are close to the δ13C of the methane utilized. Apparently, little of the kinetic isotope fractionation associated with methanotrophy is expressed in the host's tissue. Vestimentiferan carbon isotopic composition reflects both carbon limitation and the isotopic composition of the substrate utilized. The δ13C-values of vent vestimentiferans tend to be affected by carbon limitation, whereas those of seep vestimentiferans reflect the variable isotopic composition of pore-water DIC. Stable nitrogen isotopic compositions are consistent with nitrogen (N2) fixation, but the presence of the enzyme responsible for nitrogen fixation, nitrogenase, has not been conclusively demonstrated. A variety of nitrogen sources [N2, NH4+, PON (particulate organic nitrogen), DON (dissolved organic nitrogen) and NO4] may be utilized by vent and seep organisms. However, the δ15N data suggest that the mechanism of nitrogen metabolism is not a function of the species or the symbiont type. Sulfur is a key element in vent and seep environments and thiotrophy is the major chemosynthetic activity. The sources of sulfur are highly variable in quantity and isotopic composition but are almost always linked to bacterial activity,l either free-living and/or symbiont. Nitrogen and sulfur nutritional requirements appear to be derived from a wide variety of sources. The relative importance of nutrition derived from heterotrophy and chemoautotrophy depends on the chemical environment and animal physiology. Stable isotope compositions provide insight into these diverse metabolic strategies; however, a complete inventory of the concentration and isotopic composition of inorganic and organic substrates, as well as supporting biochemical, enzymatic and observational studies, are needed to resolve fundamental ecological questions.

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