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描述东南极半岛拉森 B 地区新近无冰架环境下冷泉处线虫群落特征。

Characterisation of the nematode community of a low-activity cold seep in the recently ice-shelf free Larsen B area, Eastern Antarctic Peninsula.

机构信息

Marine Biology Section, Ghent University, Ghent, Belgium.

出版信息

PLoS One. 2011;6(7):e22240. doi: 10.1371/journal.pone.0022240. Epub 2011 Jul 20.

Abstract

BACKGROUND

Recent climate-induced ice-shelf disintegration in the Larsen A (1995) and B (2002) areas along the Eastern Antarctic Peninsula formed a unique opportunity to assess sub-ice-shelf benthic community structure and led to the discovery of unexplored habitats, including a low-activity methane seep beneath the former Larsen B ice shelf. Since both limited particle sedimentation under previously permanent ice coverage and reduced cold-seep activity are likely to influence benthic meiofauna communities, we characterised the nematode assemblage of this low-activity cold seep and compared it with other, now seasonally ice-free, Larsen A and B stations and other Antarctic shelf areas (Weddell Sea and Drake Passage), as well as cold-seep ecosystems world-wide.

PRINCIPAL FINDINGS

The nematode community at the Larsen B seep site differed significantly from other Antarctic sites in terms of dominant genera, diversity and abundance. Densities in the seep samples were high (>2000 individuals per 10 cm(2)) and showed below-surface maxima at a sediment depth of 2-3 cm in three out of four replicates. All samples were dominated by one species of the family Monhysteridae, which was identified as a Halomonhystera species that comprised between 80 and 86% of the total community. The combination of high densities, deeper density maxima and dominance of one species is shared by many cold-seep ecosystems world-wide and suggested a possible dependence upon a chemosynthetic food source. Yet stable (13)C isotopic signals (ranging between -21.97±0.86‰ and -24.85±1.89‰) were indicative of a phytoplankton-derived food source.

CONCLUSION

The recent ice-shelf collapse and enhanced food input from surface phytoplankton blooms were responsible for the shift from oligotrophic pre-collapse conditions to a phytodetritus-based community with high densities and low diversity. The parthenogenetic reproduction of the highly dominant Halomonhystera species is rather unusual for marine nematodes and may be responsible for the successful colonisation by this single species.

摘要

背景

近年来,南极洲东部拉森 A(1995 年)和 B(2002 年)冰架因气候原因崩解,为评估冰架下底层生物群落结构提供了独特的机会,并发现了以前未被探索的栖息地,包括前拉森 B 冰架下一个低活性甲烷渗漏区。由于以前永久冰盖下的有限颗粒沉降和冷泉活动减少都可能影响底层后生动物群落,我们对这个低活性冷泉的线虫组合进行了描述,并将其与其他现在季节性无冰的拉森 A 和 B 站点以及其他南极大陆架地区(威德尔海和德雷克海峡)以及全球范围内的冷泉生态系统进行了比较。

主要发现

拉森 B 冷泉区的线虫群落与其他南极地区在优势属、多样性和丰度方面有显著差异。在四个重复中有三个重复中,冷泉样本中的线虫密度很高(>2000 条/10cm2),并在 2-3cm 的沉积物深处达到表面下最大值。所有样本均由一科 Monhysteridae 的一个种主导,该种被鉴定为 Halomonhystera 种,占总群落的 80-86%。高密度、更深的密度最大值和一个物种的优势,是全球许多冷泉生态系统的共同特征,表明可能依赖于化能合成食物源。然而,稳定的(13)C 同位素信号(范围在-21.97±0.86‰和-24.85±1.89‰之间)表明存在源自浮游植物的食物源。

结论

最近的冰架崩解和从表面浮游植物大量繁殖而来的增强的食物输入,导致从崩解前贫营养条件转变为以浮游植物碎屑为基础的高密度、低多样性群落。高度占优势的 Halomonhystera 种的孤雌生殖对于海洋线虫来说相当罕见,这可能是该单一物种成功定植的原因。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9509/3140504/84940c1d5715/pone.0022240.g001.jpg

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