Banaszak Anastazia T, Ayala-Schiaffino B Natalia, Rodríguez-Román Aimé, Enríquez Susana, Iglesias-Prieto Roberto
Unidad Académica Puerto Morelos, Apartado Postal 1152, Cancún 77500, México.
Rev Biol Trop. 2003 Jun;51 Suppl 4:57-66.
Two naturally occurring colonies of Millepora alcicornis were monitored during 1997 and 1998, both years in which this species bleached in the Mexican Caribbean. One colony (HL) was naturally exposed to a high light environment and another nearby colony (LL) was exposed to 5.9 times lower light levels due to shadowing by a pier. For 10 days in August 1997, seawater temperatures in the surrounding reef lagoon rose up to 1.5 degrees C above the 6-year August average. The HL colony bleached to white during this period, whereas, the LL colony remained dark-brown colored. The HL colony recovered its normal dark-brown coloration (reversible bleaching) within several weeks, during which time the seawater temperatures returned to average. The following year, for 10 days, seawater temperatures rose up to 3 degrees C above the 7-year August average and both colonies bleached to white and neither colony recovered (irreversible bleaching). Both colonies were rapidly overgrown by algae and hydroids and, as of June 2003, no recovery has taken place. Prior to the 1997 bleaching, experiments using solar radiation showed that the quantum yield of photosystem II charge separation of branches from HL and LL colonies were affected for several hours by exposure to ultraviolet radiation (UVR, 280 to 400 nm), but recovered by the same evening, suggesting that UVR does not have long-term effects on photochemistry in M. alcicornis. In situ effective quantum yield of photosystem II charge separation (deltaF/Fm') measurements before the 1998 bleaching event indicate that both colonies were healthy in terms of the physiological status of their endosymbionts. During and after the 1998 bleaching event, both colonies showed a reduction in deltaF/Fm' and consequently an increase in excitation pressure on photosystem II. The data suggest that temperature is not the only factor that causes bleaching and that solar radiation may play an important role in coral bleaching.
1997年和1998年期间,对两个自然形成的多孔鹿角珊瑚群体进行了监测,这两年该物种在墨西哥加勒比海出现了白化现象。一个群体(HL)自然暴露于高光环境,附近的另一个群体(LL)由于被一个码头遮挡,光照水平低5.9倍。1997年8月,周围珊瑚礁泻湖的海水温度连续10天比6年8月平均温度高出1.5摄氏度。在此期间,HL群体白化至白色,而LL群体仍为深褐色。HL群体在几周内恢复了正常的深褐色(可逆白化),在此期间海水温度恢复到平均水平。次年,海水温度连续10天比7年8月平均温度高出3摄氏度,两个群体均白化至白色,且均未恢复(不可逆白化)。两个群体均迅速被藻类和水螅体覆盖,截至2003年6月,仍未恢复。在1997年白化之前,利用太阳辐射进行的实验表明,HL和LL群体的分支中光系统II电荷分离的量子产率在暴露于紫外线辐射(UVR,280至400纳米)下数小时会受到影响,但在当晚恢复,这表明UVR对多孔鹿角珊瑚的光化学没有长期影响。1998年白化事件之前的光系统II电荷分离原位有效量子产率(deltaF/Fm')测量表明,就其共生体的生理状态而言,两个群体均健康。在1998年白化事件期间及之后,两个群体的deltaF/Fm'均降低,因此光系统II上的激发压力增加。数据表明,温度不是导致白化的唯一因素,太阳辐射可能在珊瑚白化中起重要作用。