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钻孔海绵对珊瑚礁的化学与机械生物侵蚀——来自近拟粗壮多孔海绵(Pione cf. vastifica)的启示

Chemical versus mechanical bioerosion of coral reefs by boring sponges--lessons from Pione cf. vastifica.

作者信息

Zundelevich A, Lazar B, Ilan M

机构信息

Department of Zoology, Tel Aviv University, Tel Aviv 69978, Israel.

出版信息

J Exp Biol. 2007 Jan;210(Pt 1):91-6. doi: 10.1242/jeb.02627.

Abstract

Bioerosion by boring sponges is an important mechanism shaping the structure of coral reefs all around the world. To determine the excavation rate by boring sponges, we developed a system in which chemical and mechanical boring rates [calcium carbonate (CaCO(3)) dissolution and chip production, respectively] were measured simultaneously in experimental tanks containing reefal rock inhabited by a boring sponge. Pione cf. vastifica (Hancock 1849) was chosen as a model species to study the erosion rate of boring sponges. It is an abundant species in the coral reefs of the Nature Reserve Reef, Elat, Gulf of Aqaba, northern Red Sea, reaching maximum abundance at 25-30 m. The rate of chemical bioerosion was determined from the increase in tank-seawater alkalinity over time, and the mechanical bioerosion rate was estimated from the total amount of CaCO(3) chips produced over the same time interval. The measured bioerosion rate of P. cf. vastifica was 2.3 g m(-2) sponge day(-1), showing seasonal but not diurnal variations, suggesting that the zooxanthellae harboring the sponge have no effect on its boring rate. The experiments indicated clearly that per each mass of chips that P. cf. vastifica produces during its boring activity, it dissolves three masses of reef CaCO(3) framework. Assuming that some additional boring sponges can use a similar strategy of bioerosion, these findings suggest that chips, the most obvious erosion products of boring sponges, represent only a small fraction of boring sponge bioerosion capacity.

摘要

钻孔海绵造成的生物侵蚀是塑造全球珊瑚礁结构的重要机制。为了确定钻孔海绵的挖掘速率,我们开发了一个系统,在装有栖息有钻孔海绵的礁岩的实验水槽中,同时测量化学和机械钻孔速率(分别为碳酸钙溶解和碎屑产生速率)。选择了近似阔口矶海绵(Pione cf. vastifica, Hancock 1849)作为研究钻孔海绵侵蚀速率的模式物种。它是红海北部亚喀巴湾埃拉特自然保护区珊瑚礁中的常见物种,在25 - 30米深处数量最多。化学生物侵蚀速率通过水槽海水碱度随时间的增加来确定,机械生物侵蚀速率则根据同一时间间隔内产生的碳酸钙碎屑总量来估算。测得的近似阔口矶海绵的生物侵蚀速率为2.3克每平方米海绵每天,呈现季节性变化而非昼夜变化,这表明共生有虫黄藻的海绵对其钻孔速率没有影响。实验清楚地表明,近似阔口矶海绵在钻孔活动中每产生一定质量的碎屑,就会溶解三倍质量的珊瑚礁碳酸钙框架。假设其他一些钻孔海绵也能采用类似的生物侵蚀策略,这些发现表明,碎屑作为钻孔海绵最明显的侵蚀产物,仅占钻孔海绵生物侵蚀能力的一小部分。

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