Department of Biology, Norwegian University of Science and Technology, N-7491 Trondheim, Norway.
Department of Biology, Norwegian University of Science and Technology, N-7491 Trondheim, Norway.
Sci Total Environ. 2014 Mar 1;473-474:262-74. doi: 10.1016/j.scitotenv.2013.12.028. Epub 2013 Dec 27.
The objective of this study was to quantify chemical and biological responses to an experimentally increased nutrient input to an open coastal planktonic ecosystem and to contribute to a scientific concept and credible indicators for managing nutrient supply to coastal waters. Data were derived in a 5 year fertilisation experiment of a tidal driven coastal lagoon at the outer coast off Central Norway (63°36' N, 9°33' E), with a surface area of 275.000 m(2), volume of 5.5 mill m(3), mean depth of 22 m and a water exchange rate of 0.19 day(-1). The lagoon was fertilised in the summer season 1998 and 1999, while summer seasons 1996-97 and 2000 and inflowing water were used as unfertilised references. Most measured chemical and biological variables showed linear responses with an increasing loading rate of inorganic N and P (LN and LP, respectively). PON, POP and POC (< 200 μm) responded significantly (P<0.05) as did chlorophyll a and phytoplankton C. DIN and DIP remained, however, constant and independent of LN and LP, respectively (P>0.05) as did heterotrophic biomass (P>0.05). We evaluate the response variables assuming a stepwise incorporation process of nutrients in the planktonic ecosystem and how that will interact with biological response times and water dilution rates. We suggest that PON is a credible indicator of both chemical and ecological states of the planktonic ecosystem and that natural background and upper critical concentrations are 46 and 88 mg PON m(-3), respectively. The study was supported by data from mesocosms. We discuss the scientific relevance of our suggestions, how results can be extrapolated to a broader geographical scale, and we propose a science-based concept for the management of nutrient emission to open coastal waters.
本研究旨在量化向开阔海岸浮游生态系统中人为增加营养物质输入所产生的化学和生物响应,并为管理沿海水域营养物质供应提供科学概念和可靠指标。数据来自于挪威中部外海(63°36' N,9°33' E)潮汐驱动沿海泻湖的 5 年施肥实验,泻湖面积 275000 平方米,体积 5500000 立方米,平均水深 22 米,水交换率为 0.19 天-1。泻湖于 1998 年和 1999 年夏季进行施肥,而 1996-97 年和 2000 年夏季以及流入水则作为未施肥的对照。大多数测量的化学和生物变量均表现出与无机氮和磷负荷率(LN 和 LP)呈线性响应的特征。PON、POP 和 POC(<200 μm)显著响应(P<0.05),叶绿素 a 和浮游植物 C 也是如此。然而,DIN 和 DIP 保持不变,且分别独立于 LN 和 LP(P>0.05),异养生物量也是如此(P>0.05)。我们假设营养物质在浮游生态系统中的逐步同化过程以及该过程如何与生物响应时间和水稀释率相互作用,对响应变量进行评估。我们认为 PON 是浮游生态系统化学和生态状态的可靠指标,其自然背景和上限临界浓度分别为 46 和 88 mg PON m-3。该研究得到了中观模型数据的支持。我们讨论了我们建议的科学相关性,以及如何将结果外推到更广泛的地理范围,并提出了一个基于科学的概念,用于管理向开阔沿海水域的营养物质排放。