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根据现场脉冲追踪实验推断深渊大型底栖动物的摄食偏好。

Feeding preferences of abyssal macrofauna inferred from in situ pulse chase experiments.

机构信息

School of Environmental Sciences, University of Liverpool, Liverpool, Merseyside, United Kingdom.

出版信息

PLoS One. 2013 Nov 26;8(11):e80510. doi: 10.1371/journal.pone.0080510. eCollection 2013.

Abstract

Climatic fluctuations may significantly alter the taxonomic and biochemical composition of phytoplankton blooms and subsequently phytodetritus, the food source for the majority of deep-sea communities. To examine the response of abyssal benthic communities to different food resources we simulated a food sedimentation event containing diatoms and coccolithophorids at Station M in the NE Pacific. In one set of experiments we measured incorporation of diatomC and coccoN into the macrofauna using isotopically enriched (13)C-diatoms and (15)N-coccolithophores. In a second experiment we measured incorporation of C and N from dual-labelled ((13)C and (15)N) diatoms. The second experiment was repeated 2 months later to assess the effect of seasonality. The simulated food pulses represented additions of 650 - 800 mg C m(-2) and 120 mg N m(-2) to the seafloor. In all cases rapid incorporation of tracer was observed within 4 days, with between 20% and 52% of the macrofauna displaying evidence of enrichment. However, incorporation levels of both diatomC and coccoN were low (<0.05% and 0.005% of the added C and N). Incorporation of labelled diatoms was similar during both June and September suggesting that the community was not food limited during either period. We found no evidence for selective ingestion of the different food types in the metazoan fauna suggesting that macrofauna do not have strong preferences for diatom vs. coccolithophore dominated phytodetrital pulses. C∶N ratios from both experiments suggest that the metazoan macrofauna community appear to have higher C demands and/or assimilation efficiencies compared to N. Concomitantly, the foraminifera preferentially selected for diatomN over coccoN, and we suggest that this may be related to foraminiferal requirements for intracellular nitrate. These experiments provide evidence that abyssal faunal feeding strategies are in part driven by an organism's internal stoichiometric budgets and biochemical requirements.

摘要

气候变化可能会显著改变浮游植物大量繁殖的分类和生化组成,进而影响浮游植物碎屑,而后者是大多数深海生物群落的食物来源。为了研究深海海底生物群落对不同食物资源的响应,我们在北太平洋的 M 站模拟了一次含有硅藻和颗石藻的食物沉降事件。在一组实验中,我们使用同位素标记的(13)C-硅藻和(15)N-颗石藻来测量大型动物对硅藻 C 和 coccoN 的吸收。在第二项实验中,我们测量了来自双标记(13C 和 15N)硅藻的 C 和 N 的吸收。第二项实验在两个月后重复进行,以评估季节性的影响。模拟的食物脉冲代表向海底添加了 650-800mg C m(-2) 和 120mg N m(-2)。在所有情况下,示踪剂的快速吸收在 4 天内观察到,有 20%-52%的大型动物显示出富集的证据。然而,硅藻 C 和 coccoN 的吸收水平都很低(添加的 C 和 N 的 0.05%和 0.005%以下)。6 月和 9 月的标记硅藻吸收情况相似,这表明在这两个时期,群落都没有受到食物的限制。我们没有发现后生动物区系对不同食物类型有选择性摄食的证据,这表明大型动物对硅藻与颗石藻为主的浮游植物碎屑脉冲没有强烈的偏好。两个实验的 C∶N 比值表明,后生动物大型动物群落的 C 需求和/或同化效率似乎高于 N。同时,有孔虫优先选择硅藻 N 而不是 coccoN,我们认为这可能与有孔虫对细胞内硝酸盐的需求有关。这些实验提供的证据表明,深海动物的摄食策略部分是由生物体内部化学计量预算和生化需求驱动的。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2829/3841197/33e0f6daa25d/pone.0080510.g001.jpg

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