海马冷渗漏不同渗流强度下贻贝和鳞虫之间的营养关系:稳定同位素(δ13C 和 δ15N)和 C:N:P 化学计量的启示

IF 2.3 3区 地球科学 Q2 OCEANOGRAPHY
Zhixin Ke , Haochen Huang , Danting Chen , Yehui Tan
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引用次数: 0

摘要

南海海马冷泉深海贻贝(贻贝科:Bathymodiolinae)的贻腔中通常含有一种鳞片蠕虫Branchipolynoe pettiboneae。为了探索它们的环境适应和共生机制,研究了不同甲烷渗流强度下海马鳞虫和伴生鳞虫的稳定同位素(δ13C和δ15N)和C:N:P生态化学计量。在有渗流的情况下,大多数贻贝的套腔中都有一条鳞虫。然而,在停止渗流的情况下,贻贝的生理状态看起来并不健康,体内也没有鳞虫出现。不同贻贝组织的δ13C值差异很大,从-49.7‰到-57.8‰不等。在主动渗流条件下,贻贝组织的δ13C值依次为足部、鳃部和套部,而在停止渗流条件下,贻贝组织的δ13C值变化趋势没有规律可循。鳞虫的δ13C和δ15N相对于其贻贝宿主平均富集了2.9‰和3.2‰,鳞虫与贻贝的营养位分离在渗流活跃时更为显著。在主动渗流条件下,贻贝足的δ13C值(平均-50.8‰)明显高于停止渗流条件下(平均-55.1‰),表明在主动渗流条件下,贻贝可能摄取和同化了更多富含13C的悬浮颗粒有机物(POM)。在贻贝组织中,高 C:N 比值和低δ13C 值应归因于高含量的储能物质。在停止渗流的情况下,随着储能物质的耗尽,地幔的 C:N 比值急剧下降。P 含量的变化在鳃中最为显著,这可能受共生细菌数量的调节。可以推测,鳃中 P 含量的急剧下降是由于高 P 细菌共生体在停止渗流时的损失。鳃组织中的 C:P 和 N:P 比值在停止渗流后都明显增加,这表明鳞虫的食物质量下降。生活在贻贝中的鳞片蠕虫可能会发现食物质量的变化,并放弃饥饿的贻贝宿主。我们的研究结果有助于更好地理解冷渗漏生态系统中渗流强度不稳定时化自养贻贝和鳞虫的环境适应性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Trophic relationship between mussels and scale worms under various seepage intensities in the haima cold seep: Insights from stable isotopes (δ13C and δ15N) and C:N:P stoichiometry

Trophic relationship between mussels and scale worms under various seepage intensities in the haima cold seep: Insights from stable isotopes (δ13C and δ15N) and C:N:P stoichiometry

The deep-sea mussels Gigantidas haimaensis (Mytilidae: Bathymodiolinae) usually contain one scale worm Branchipolynoe pettiboneae in their mantle cavity in the Haima cold seep, South China Sea. To explore their environmental adaptation and coexistence mechanisms, the stable isotopes (δ13C and δ15N) and C:N:P ecological stoichiometry of G. haimaensis and the associated B. pettiboneae were investigated under different methane seepage intensities. In the presence of seepage, most mussels harbored one scale worm in their mantle cavity. However, under seepage cease, the physiological status of mussels looked unhealthy, and no scale worm appeared in their bodies. The variation in δ13C values was great among different mussel tissues, ranging from −49.7‰ to −57.8‰. The δ13C values of mussel tissues followed the order of foot > gill > mantle under active seepage, while no regular trend was found under seepage cease. The δ13C and δ15N of scale worms were averagely enriched by 2.9 ‰ and 3.2 ‰ relative to their mussel hosts, and the trophic niche separation between scale worms and mussels was more significant under active seepage. The δ13C value of mussel foot was significantly higher under active seepage (average −50.8‰) than under seepage cease (average −55.1‰), indicating that mussels might ingest and assimilate more 13C-rich suspended particulate organic matter (POM) under active seepage. In mantle tissues, the high C:N ratio and low δ13C value should be attributed to the high content of energy storage substances. The C:N ratio of mantle dramatically declined with the exhaustion of energy storage materials under seepage cease. The variation of P content was most significant in the gill, which might be regulated by the abundance of symbiotic bacteria. It can be speculated that the dramatic decline of P content in the gill was attributed to the loss of high-P bacterial symbionts under seepage cease. Both the C:P and N:P ratios of gill tissues significantly increased under seepage cease, which suggested the decline of food quality for scale worms. Mussel-dwelling scale worms might detect the change of food quality and abandon their starving mussel host. Our results help to better understand the environmental adaptation of chemoautotrophic mussels and scale worms under unstable seepage intensity in cold seep ecosystems.

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来源期刊
CiteScore
4.60
自引率
4.20%
发文量
144
审稿时长
18.3 weeks
期刊介绍: Deep-Sea Research Part I: Oceanographic Research Papers is devoted to the publication of the results of original scientific research, including theoretical work of evident oceanographic applicability; and the solution of instrumental or methodological problems with evidence of successful use. The journal is distinguished by its interdisciplinary nature and its breadth, covering the geological, physical, chemical and biological aspects of the ocean and its boundaries with the sea floor and the atmosphere. In addition to regular "Research Papers" and "Instruments and Methods" papers, briefer communications may be published as "Notes". Supplemental matter, such as extensive data tables or graphs and multimedia content, may be published as electronic appendices.
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