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地中海贻贝作为环境状况的生物指示物:以亚得里亚海东岸为例。

Mytilus galloprovincialis as a bioindicator of environmental conditions: the case of the eastern coast of the Adriatic Sea.

作者信息

Kanduc Tjasa, Medaković Davorin, Hamer Bojan

机构信息

Jozef Stefan Institute, Ljubljana, Slovenia.

出版信息

Isotopes Environ Health Stud. 2011 Mar;47(1):42-61. doi: 10.1080/10256016.2011.548866.

Abstract

The marine mussel Mytilus galloprovincialis lives attached to the surface of hard substrata, where its exposure and relative immobility allow it to record changes in ambient seawater. It is also found along the eastern coast of the Adriatic Sea. Oxygen and carbon isotopes were analysed for calcite and aragonite in separate shell layers, while major, minor and trace elements in the bulk shell were analysed to evaluate environmental conditions such as the temperature of carbonate deposition, freshwater influence and locations of anthropogenic pollution. We found that, on average, aragonite is enriched by 1.1‰ in (13)C and by 0.2‰ in (18)O compared with calcite. The calculated temperatures for M. galloprovincialis shell growth from the investigated area range from 13.4 to 20.9 °C for calcite and from 16.6 to 23.1 °C for aragonite. According to the δ(18)O and δ(13)C values of shell layers, we can separate the investigated area into three locations: those with more influence of freshwater, those with less influence of freshwater and those with marine environments. The highest concentrations of manganese, barium, boron, arsenic, nickel and chromium were observed in shells from Omis, Bacvice and Zablace (Central Adriatic) and Sv. Ivan (South Adriatic), where chemical and heavy industries are located and where sewage is known to be discharged into coastal areas. The highest concentrations of zinc, lead and copper were measured in samples from Pula, Rijeka and Gruz, where there are also ports in addition to industry.

摘要

地中海贻贝(Mytilus galloprovincialis)附着生活在坚硬基质表面,因其暴露在外且相对固定,能够记录周围海水的变化。它也分布在亚得里亚海的东海岸。对贝壳不同层中的方解石和文石进行了氧和碳同位素分析,同时分析了整个贝壳中的主量、微量和痕量元素,以评估诸如碳酸盐沉积温度、淡水影响和人为污染位置等环境条件。我们发现,平均而言,与方解石相比,文石的碳-13富集1.1‰,氧-18富集0.2‰。根据研究区域内地中海贻贝贝壳生长的计算温度,方解石的温度范围为13.4至20.9℃,文石的温度范围为16.6至23.1℃。根据贝壳层的δ(18)O和δ(13)C值,我们可以将研究区域分为三个位置:受淡水影响较大的区域、受淡水影响较小的区域和海洋环境区域。在奥米斯、巴奇维采和扎布拉斯(亚得里亚海中部)以及圣伊万(亚得里亚海南部)的贝壳中观察到锰、钡、硼、砷、镍和铬的最高浓度,这些地方有化学和重工业,且已知有污水排入沿海地区。在普拉、里耶卡和格鲁兹的样本中测量到锌、铅和铜的最高浓度,这些地方除了有工业外还有港口。

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