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Expanded Florida reef development during the mid-Pliocene warm period

机译:在上新世中期暖期,佛罗里达的珊瑚礁发展得到扩大

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The coral fauna of the Tamiami Formation documents a northern expansion of reef development along the Florida Peninsula during the mid-Pliocene warm period (MPWP). Radiometric dating (U-Pb) of Solenastrea bournoni produced an age of 2.99 +/- 0.11 Ma, constraining reef development to the MPWP and the peak of Plio-Pleistocene faunal turnover; subsequent to the final closure of the Central American Seaway (CAS) but prior to major Northern Hemisphere Glaciation (NHG). Coral faunal analyses are based on a total of 1614 coral specimens collected along a 165 km stretch of the west Florida coast, and included rarefaction and detrended correspondence analysis (DCA). A total of 60 coral species occur within the Tamiami Formation, with faunal assemblages ranging from 42 to 87% extinct taxa. The Tamiami collections can be split into a southem "reef" assemblage with high diversity of stenotopic taxa and a northern "non-reef" assemblage with lower diversity eurytopic taxa. The southem reef assemblage contains framework buildups of the dominant tropical taxa Stylophora affinis, Orbicella annularis, and Acropora cervicornis. We interpret enhanced west Florida reef development during the middle Pliocene to be a product of more equitable sea surface temperatures, and reduced salinity fluctuations associated with higher sea levels. While mean sea surface temperature estimates based on oxygen isotopic analysis of the coral Solenastrea bournoni (253 degrees C) are similar to present day values (26 degrees C), a completely flooded southern Florida Platform in the Pliocene would be less prone to salinity fluctuations associated with coastal runoff and extreme cold-water events during winter storms. While higher latitude range shifts of tropical reef corals associated with current global climate change have been documented elsewhere in the world, we do not foresee the West Florida Shelf being conducive to significant range shifts in tropical coral taxa or reef development within the coming century. 2017 Elsevier B.V. All rights reserved.
机译:Tamiami组的珊瑚动物群记录了在上新世中期(MPWP)中佛罗里达半岛沿礁的北部扩展。 Solenastrea bournoni的放射性测年(U-Pb)年龄为2.99 +/- 0.11 Ma,这限制了珊瑚礁向MPWP的发育和上新世更新世动物区系转换的高峰。在中美洲航道(CAS)最终关闭之后,但在北半球主要冰川(NHG)之前。珊瑚动物区系分析是基于在佛罗里达州西部海岸165公里处采集的总共1614个珊瑚标本进行的,其中包括稀疏性和去趋势对应分析(DCA)。 Tamiami组内共有60种珊瑚物种,其动物群落范围从42%至87%的灭绝生物群中不等。 Tamiami集合可分为具有多样化的狭窄主题类群的南部“珊瑚礁”组合和具有较低多样性的主题性分类类的北部“非礁石”组合。南部礁石组合包含主要热带类群Stylophora affinis,Orbicella ringis和Acropora cervicornis的构架。我们将上新世中期中佛罗里达州西部礁石开发的增强解释为海平面温度更加平衡,以及与较高海平面相关的盐度波动减少的产物。虽然基于珊瑚Solenastrea bournoni(253摄氏度)的氧同位素分析得出的平均海面温度估算值与当前值(26摄氏度)相似,但在上新世佛罗里达南部完全被洪水淹没的平台不太容易出现盐度波动冬季暴风雨期间沿海径流和极端冷水事件。尽管在世界其他地方已经记录了与当前全球气候变化相关的热带珊瑚礁更高纬度范围的变化,但我们不认为西佛罗里达大陆架会在未来一个世纪内有利于热带珊瑚类群或礁石发展的显着范围变化。 2017 Elsevier B.V.保留所有权利。

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