Nava Héctor, Carballo José Luis
Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México (UNAM), Avenida Joel Montes Camarena, s/n. apartado postal 811, 82000 Mazatlán, México.
J Exp Biol. 2008 Sep;211(Pt 17):2827-31. doi: 10.1242/jeb.019216.
Species richness (S) and frequency of invasion (IF) by boring sponges on living colonies of Pocillopora spp. from National Park Isla Isabel (México, East Pacific Ocean) are presented. Twelve species belonging to the genera Aka, Cliona, Pione, Thoosa and Spheciospongia were found, and 56% of coral colonies were invaded by boring sponges, with Cliona vermifera Hancock 1867 being the most abundant species (30%). Carbonate dissolution rate and sediment production were quantified for C. vermifera and Cliona flavifodina Rützler 1974. Both species exhibited similar rates of calcium carbonate (CaCO3) dissolution (1.2+/-0.4 and 0.5+/-0.2 kg CaCO3 m(-2) year(-1), respectively, mean +/- s.e.m.), and sediment production (3.3+/-0.6 and 4.6+/-0.5 kg CaCO3 m(-2) year(-1)), resulting in mean bioerosion rates of 4.5+/-0.9 and 5.1+/-0.5 kg CaCO3 m(-2) year(-1), respectively. These bioerosion rates are close to previous records of coral calcification per unit of area, suggesting that sponge bioerosion alone can promote disequilibrium in the reef accretion/destruction ratio in localities that are heavily invaded by boring sponges. The proportion of dissolved material by C. vermifera and C. flavifodina (27 and 10.2%, respectively) confirms that chemical bioerosion plays an important role in sponge bioerosion and in the CaCO3 cycle in coral reefs.
本文展示了墨西哥东太平洋伊莎贝尔岛国家公园内,波氏鹿角珊瑚(Pocillopora spp.)活群体上钻孔海绵的物种丰富度(S)和入侵频率(IF)。研究发现了属于阿卡属(Aka)、凿贝海绵属(Cliona)、先驱海绵属(Pione)、索萨海绵属(Thoosa)和球海绵属(Spheciospongia)的12个物种,56%的珊瑚群体被钻孔海绵入侵,其中汉考克氏凿贝海绵(Cliona vermifera Hancock 1867)是最丰富的物种(占30%)。对汉考克氏凿贝海绵和黄褐凿贝海绵(Cliona flavifodina Rützler 1974)的碳酸盐溶解速率和沉积物产量进行了量化。这两个物种的碳酸钙(CaCO₃)溶解速率相似(分别为1.2±0.4和0.5±0.2 kg CaCO₃ m⁻² 年⁻¹,平均值±标准误),沉积物产量也相似(分别为3.3±0.6和4.6±0.5 kg CaCO₃ m⁻² 年⁻¹),导致平均生物侵蚀速率分别为4.5±0.9和5.1±0.5 kg CaCO₃ m⁻² 年⁻¹。这些生物侵蚀速率接近先前每单位面积珊瑚钙化的记录,表明在钻孔海绵大量入侵的地区,仅海绵生物侵蚀就能促进珊瑚礁堆积/破坏比率的失衡。汉考克氏凿贝海绵和黄褐凿贝海绵溶解物质的比例(分别为27%和10.2%)证实,化学生物侵蚀在海绵生物侵蚀和珊瑚礁碳酸钙循环中起着重要作用。