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受近期冰川消退影响的南极浅水环境生态系统中的底栖生物营养相互作用

Benthic Trophic Interactions in an Antarctic Shallow Water Ecosystem Affected by Recent Glacier Retreat.

作者信息

Pasotti Francesca, Saravia Leonardo Ariel, De Troch Marleen, Tarantelli Maria Soledad, Sahade Ricardo, Vanreusel Ann

机构信息

Marine Biology Laboratory, Ghent University, Krijgslaan 281/S8, B-9000, Ghent, Belgium.

Institute of Sciences, National University of General Sarmiento, Juan María Gutierrez 1150, C.P.1613, Los Polvorines, Buenos Aires, Argentina.

出版信息

PLoS One. 2015 Nov 11;10(11):e0141742. doi: 10.1371/journal.pone.0141742. eCollection 2015.

Abstract

The western Antarctic Peninsula is experiencing strong environmental changes as a consequence of ongoing regional warming. Glaciers in the area are retreating rapidly and increased sediment-laden meltwater runoff threatens the benthic biodiversity at shallow depths. We identified three sites with a distinct glacier-retreat related history and different levels of glacial influence in the inner part of Potter Cove (King George Island, South Shetland Islands), a fjord-like embayment impacted since the 1950s by a tidewater glacier retreat. We compared the soft sediment meio- and macrofauna isotopic niche widths (δ13C and δ15N stable isotope analysis) at the three sites to investigate possible glacier retreat-related influences on benthic trophic interactions. The isotopic niches were locally shaped by the different degrees of glacier retreat-related disturbance within the Cove. Wider isotopic niche widths were found at the site that has become ice-free most recently, and narrower niches at the older ice-free sites. At an intermediate state of glacier retreat-related disturbance (e.g. via ice-growler scouring) species with different strategies could settle. The site at the earliest stage of post-retreat development was characterized by an assemblage with lower trophic redundancy. Generally, the isotopic niche widths increased with increasing size spectra of organisms within the community, excepting the youngest assemblage, where the pioneer colonizer meiofauna size class displayed the highest isotopic niche width. Meiofauna at all sites generally occupied positions in the isotopic space that suggested a detrital-pool food source and/or the presence of predatory taxa. In general ice scour and glacial impact appeared to play a two-fold role within the Cove: i) either stimulating trophic diversity by allowing continuous re-colonization of meiofaunal species or, ii) over time driving the benthic assemblages into a more compact trophic structure with increased connectedness and resource recycling.

摘要

由于持续的区域变暖,南极半岛西部正经历着强烈的环境变化。该地区的冰川正在迅速消退,携带沉积物的融水径流增加,威胁着浅水区的底栖生物多样性。我们在波特湾(南设得兰群岛乔治王岛)内部确定了三个具有不同冰川消退相关历史和不同冰川影响程度的地点,自20世纪50年代以来,这个峡湾状的海湾受到了潮水冰川消退的影响。我们比较了这三个地点软沉积物中小型和大型底栖动物的同位素生态位宽度(δ13C和δ15N稳定同位素分析),以研究冰川消退可能对底栖生物营养相互作用产生的影响。海湾内不同程度的与冰川消退相关的干扰在局部塑造了同位素生态位。在最近才无冰的地点发现了更宽的同位素生态位宽度,而在较早无冰的地点则较窄。在与冰川消退相关的干扰处于中间状态时(例如通过冰砾擦蚀),具有不同策略的物种可以定居。消退后发育最早阶段的地点以营养冗余较低的群落为特征。一般来说,同位素生态位宽度随着群落中生物个体大小谱的增加而增加,但最年轻的群落除外,在该群落中,先锋定居的小型底栖动物大小类群显示出最高的同位素生态位宽度。所有地点的小型底栖动物在同位素空间中通常占据表明以碎屑库为食物来源和/或存在捕食性类群的位置。总体而言,冰蚀和冰川影响在海湾内似乎起到了双重作用:i)通过允许小型底栖动物物种的持续重新定殖来刺激营养多样性,或者ii)随着时间的推移,将底栖生物群落驱动到一个更紧凑的营养结构,增加连通性和资源循环。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ee85/4641631/f9a92977ef62/pone.0141742.g001.jpg

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