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A relic coral fauna threatened by global changes and human activities, Eastern Brazil

机译:巴西东部,受全球变化和人类活动威胁的遗迹珊瑚动物区系

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Coral species composition of drilled cores from emergent bank reefs, and coral cover of the surface of old and living reefs located along the coast of the state of Bahia, Eastern Brazil, revealed that there is a marked change in the occurrence of the major building coral species in different time intervals of the reef structure, as well as in the living surface of reefs located in two different geographical sites. Holocene core sections from two reef areas (12° 40′S-38° 00′W and 18° 00′S-39° 00′W) have as major reef builders, on its topmost core interval (3 to 4 ky old), the endemic coral Mussismilia braziliensis Verrill, 1868, which also dominate on the 2.5-3.5 ky old surfaces of truncated reef tops. At the base of the cores (the 2 m lower interval, older than 4 ky BP), another endemic coral Mussismilia harttii Verrill, 1868 is the dominant reef component. The relative abundance of M. braziliensis on the living surfaces of shallow reefs from both areas, shows that in the southern area, it is up to 98% on reefs located 60 km off the coast, in depths between 3 and 4 m, but do not exceed 1.3% on the surface of the northern reefs located 1-2 km off the coast in depths 4-5 m. The Holocene falling sea level that occurred along the coast of Brazil since 5.1 ky BP, causes an increasing runoff into the area of coastal reefs. This phenomenon may have affected the nearshore reef building fauna, replacing a more susceptive coral fauna with one better adapted to low light levels and higher sediment influx. The high turbidity associated with early Holocene shelf flooding, should also be responsible for the absence of M. braziliensis during the initial stages of reef buildup in Brazil. At the present time, the rapidly increasing human pressure, due to changes in land uses of the coastal zone (increasing sedimentation rate, nutrification of coastal waters, industrial pollution) and underwater practices, such as overfishing and an intense tourism, is aggravating the recovery capacity of this already naturally threatened coral community. If this situation coupled with increasing sea surface temperature persists, modern coral reef growth, in Brazil cannot be maintained and the major reef building coral species of the reefs in Bahia, a remnant endemic coral fauna will very soon appear in the list of endangered species.
机译:来自巴西东部巴伊亚州沿海沿岸的新兴礁石上钻出的岩心的珊瑚物种组成以及旧礁石和活礁石的珊瑚覆盖表明,主要建筑物珊瑚的发生发生了显着变化物种在不同时间间隔的珊瑚礁结构中,以及在两个不同地理位置的珊瑚礁活动表面中。来自两个珊瑚礁区域(12°40′S-38°00′W和18°00′S-39°00′W)的全新世岩心部分在其最高岩心区间(3至4 ky old)具有主要的造礁作用。 ,特有的珊瑚Mussismilia braziliensis Verrill,1868年,它在截断的礁顶的2.5-3.5 ky旧表面上也占主导地位。在岩心的底部(低2 m的间隔,大于4 ky BP),另一种地方性珊瑚Mussismilia harttii Verrill,1868年是主要的礁石成分。在这两个地区的浅礁生物活动表面上,巴西僵尸藻的相对丰度表明,在南部地区,位于距海岸60公里,深度3至4 m之间的礁石上,其含量高达98%。在距离海岸1-2公里,深度4-5 m的北部珊瑚礁表面上,不超过1.3%。自从5.1 ky BP以来沿巴西海岸发生的全新世海平面下降导致流入沿海礁石区域的径流增加。这种现象可能已经影响了近岸礁石建造动物群,用更适合低照度和较高泥沙涌入的珊瑚群代替了更具敏感性的珊瑚群。与早期全新世陆架洪水有关的高浊度,也应归因于巴西礁石形成初期的巴西分枝杆菌缺乏。目前,由于沿海地区土地用途的变化(沉积率增加,沿海水域营养化,工业污染)和水下作业(如过度捕鱼和密集的旅游业)而导致的人类压力迅速增加,加剧了恢复这个已经自然受到威胁的珊瑚群落的能力。如果这种情况再加上持续增加的海面温度,就无法维持巴西现代珊瑚礁的生长,并且巴伊亚礁石上主要的珊瑚礁造礁珊瑚物种将很快成为一种濒临灭绝的地方性珊瑚群落。

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