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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Bioerosion rates on coral reefs: interactions between macroborers, microborers and grazers (Moorea, French Polynesia)
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Bioerosion rates on coral reefs: interactions between macroborers, microborers and grazers (Moorea, French Polynesia)

机译:珊瑚礁的生物侵蚀率:大钻,微钻和放牧者之间的相互作用(莫雷阿岛,法属波利尼西亚)

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摘要

A two-year experimental study of bioerosion at Moorea Island, French Polynesia, clearly demonstrated the importance of microborers in the initial stages of the establishment of infaunal boring communities. Rates of erosion by micro- and macroborers and by grazers were estimated from measurements of carbonate removal from experimental substrates, using Image Analysis. The studied substrates have been exposed for 2, 6, 12 and 24 months. After 2 months of exposure, the only borers present in the substrates were cyanobacteria and one chlorophyte (Phaeophila sp.) and their bioerosion rate was estimated at 0.6 kg CaCO_3 m~(-2)yr~(-1). In the course of the 2 years of exposure, recruitment of macroborers occurred and their estimated rates of erosion increased during this period from 2.15 to 90g CaCO_3 m~(-2)yr~(-1). Carbonate removal by grazers was the dominant agent of erosion, responsible for 89% of the total bioerosion: 2.6 kg CaCO_3 m~(-2)yr~(-1), as recorded in substrates exposed for 2 years. The measurable rates of bioerosion by microborers apparently decreased with the time of exposure from 0.6 to 0.2 kg m~(-2) yr~(-1), but these values are underestimations which need to be corrected by including the intensity of microboring in substrate layers removed by grazing. Bioerosion is dependent on numerous environmental factors such as depth, light availability, and nutrient supply. A good knowledge of bioerosional processes in modern environments could highlight bioerosion significance in the fossil record.
机译:在法属波利尼西亚的莫雷阿岛进行的为期两年的生物侵蚀实验研究清楚地表明,微孔虫在建立无聊的无性群落的初始阶段非常重要。使用图像分析,通过测量从实验基质去除碳酸盐的方法,估算了微型钻孔器和大型钻孔器以及放牧者的侵蚀速率。所研究的基材已暴露2、6、12和24个月。暴露2个月后,基质中仅有的蛀虫为蓝细菌和一种绿藻(Phaeophila sp。),其生物侵蚀速率估计为0.6 kg CaCO_3 m〜(-2)yr〜(-1)。在这两年的暴露过程中,发生了大型钻孔器的招募,其侵蚀速率在此期间从2.15增加到90g CaCO_3 m〜(-2)yr〜(-1)。放牧者清除碳酸盐是侵蚀的主要因素,占总生物侵蚀的89%:2.6 kg CaCO_3 m〜(-2)yr〜(-1),暴露于暴露2年的底物中。随着暴露时间的延长,可测量的微孔虫的生物侵蚀率明显降低,从0.6降低至0.2 kg m〜(-2)yr〜(-1),但是这些值被低估了,需要通过将底物中的微孔强度包括在内来进行校正。通过放牧去除层。生物侵蚀取决于许多环境因素,例如深度,光线可用性和养分供应。对现代环境中生物侵蚀过程的深入了解可能会突出化石记录中生物侵蚀的重要性。

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