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深海棘皮动物耗氧率与海星纲、海百合纲、海胆纲、海参纲和蛇尾纲代谢率的类间比较。

Deep-sea echinoderm oxygen consumption rates and an interclass comparison of metabolic rates in Asteroidea, Crinoidea, Echinoidea, Holothuroidea and Ophiuroidea.

机构信息

School of Ocean and Earth Science, University of Southampton, National Oceanography Centre, European Way, Southampton SO14 3HZ, UK.

出版信息

J Exp Biol. 2011 Aug 1;214(Pt 15):2512-21. doi: 10.1242/jeb.055954.

Abstract

Echinoderms are important components of deep-sea communities because of their abundance and the fact that their activities contribute to carbon cycling. Estimating the echinoderm contribution to food webs and carbon cycling is important to our understanding of the functioning of the deep-sea environment and how this may alter in the future as climatic changes take place. Metabolic rate data from deep-sea echinoderm species are, however, scarce. To obtain such data from abyssal echinoderms, a novel in situ respirometer system, the benthic incubation chamber system (BICS), was deployed by remotely operated vehicle (ROV) at depths ranging from 2200 to 3600 m. Oxygen consumption rates were obtained in situ from four species of abyssal echinoderm (Ophiuroidea and Holothuroidea). The design and operation of two versions of BICS are presented here, together with the in situ respirometry measurements. These results were then incorporated into a larger echinoderm metabolic rate data set, which included the metabolic rates of 84 echinoderm species from all five classes (Asteroidea, Crinoidea, Echinoidea, Holothuroidea and Ophiuroidea). The allometric scaling relationships between metabolic rate and body mass derived in this study for each echinoderm class were found to vary. Analysis of the data set indicated no change in echinoderm metabolic rate with depth (by class or phylum). The allometric scaling relationships presented here provide updated information for mass-dependent deep-sea echinoderm metabolic rate for use in ecosystem models, which will contribute to the study of both shallow water and deep-sea ecosystem functioning and biogeochemistry.

摘要

棘皮动物是深海生物群落的重要组成部分,因为它们的丰富度以及它们的活动有助于碳循环。估计棘皮动物对食物网和碳循环的贡献对于我们理解深海环境的功能以及随着气候变化的发生,这种功能将来可能会如何变化非常重要。然而,深海棘皮动物的代谢率数据却很少。为了从深海棘皮动物中获得这些数据,使用遥控潜水器(ROV)在 2200 至 3600 米的深度部署了一种新的原位呼吸计系统,即底栖孵育室系统(BICS)。从四种深海棘皮动物(蛇尾纲和海参纲)原位获得了耗氧量。本文介绍了两种 BICS 版本的设计和操作,以及原位呼吸计测量结果。然后将这些结果纳入到更大的棘皮动物代谢率数据集,其中包括来自五个纲(海星纲、海百合纲、海胆纲、海参纲和蛇尾纲)的 84 种棘皮动物的代谢率。本研究中,每个棘皮动物类群的代谢率与体重之间的异速缩放关系各不相同。对数据集的分析表明,棘皮动物的代谢率没有随深度(按类或门)而变化。本文提出的异速缩放关系为基于质量的深海棘皮动物代谢率提供了更新的信息,可用于生态系统模型,这将有助于研究浅海和深海生态系统的功能和生物地球化学。

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