首页> 外文期刊>Journal of foraminiferal research >MESOCOSM AND MICROCOSM EXPERIMENTS ON THE FEEDING OF TEMPERATE SALT MARSH FORAMINIFERA
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MESOCOSM AND MICROCOSM EXPERIMENTS ON THE FEEDING OF TEMPERATE SALT MARSH FORAMINIFERA

机译:温带盐沼地捕捞的中核和微观微观实验

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摘要

Agglutinated foraminifera dominate in temperate salt marsh sediment, making them key indicators for monitoring sea level and environmental changes. Little is known about the biology of these benthic foraminifera because of difficulties in distinguishing live from dead specimens in laboratory cultures. We present data from 10 years of laboratory experiments using comparisons of the agglutinant trochamminids Trochammina inflata and Entzia macrescens and the mili-olid Miliammina fusca with the calcareous rotalids Helenina anderseni and Elphidium williamsoni. Specimens were taken from a laboratory mesocosm representing Chezzetcook Inlet, a cool-temperate salt marsh in eastern Canada. We determined culture requirements for the agglutinated foraminifera in Petri dishes over 10-12 week periods. Five inexpensive, non-terminal ways of identifying live organisms were developed: spatial movement, detritus-gathering, attachment, clustering, and test opacity. Comparison with rose Bengal staining showed < 10% diversion for calcareous species and T. inflata but M. fusca was over-counted by > 30%. Terminal chambers of Trochammina inflata were examined by transmission electron microscopy to visualise food consumption and identify food in digestive vacuoles, both in specimens from mesocosm and in culture. Bacteria and unidentified detritus in the vacuoles establish that this agglutinated species is a saprophagous and bacterivorous detritivore. The adhesive secretions by these species apparently help them gather and possibly farm food while being relatively immobile in the sediments. Our observations of movement and feeding orientation in the agglutinants suggest links between form and function that underscore their value as ultra high resolution sea-level proxies. Mesocosm biomass and abundance counts show that foraminifera represent > 50% of the meiofaunal biomass, emphasising their importance in the food web and energy-flow dynamics of temperate salt marsh systems.
机译:凝集的foraminifera在温带盐沼泽中占主导地位,使其成为监测海平面和环境变化的关键指标。由于在实验室培养中的死亡标本中区分生活困难,这些底栖火鸡的生物学知之甚少。我们将10年的实验室实验提供数据,使用凝集菌丘脑瘙痒和偏差麦克风和肉体玛丽亚米娜Fusca与钙质罗奈特人和Elhidium Williammsoni的钙质罗西尼亚·米兰·莫里纳菌和伊斯兰·威廉姆西试样从代表Chzzetcook入口的实验室中核糖,是加拿大东部的一种凉爽的温带盐沼。在10-12周内,我们确定了培养皿中凝集的花瓶凝集的花瓶。开发了五种廉价,非终端识别活生物的非终端方式:空间运动,碎屑采集,附着,聚类和测试不透明。与玫瑰孟加拉染色的比较显示,钙质物种和T.涌入10%的转移,但M.Fusca被> 30%的尺寸超过> 30%。通过透射电子显微镜检查Trochammina IntaTata的末端腔室,以使食物消耗可视化并鉴定来自Mesocosm和培养的标本中的消化液泡中的食物。液泡中的细菌和身份不明的碎屑证实,这种凝集物种是一种噬噬菌和诱导的碎屑。这些物种的粘合剂分泌显然有助于它们在沉积物中相对不动的同时聚集和可能的农场食物。我们对凝聚剂中的运动和饲养取向的观察表明了表格和功能之间的链接,其向超高分辨率海平面代理下划线的价值。 Mesocosm生物量和丰度计数表明,对于Meiofaunal生物量的Foraminifera代表了50%,强调了它们在温带盐沼系统的食品网和能量流动动态中的重要性。

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