DOI: 10.1016/j.gloplacha.2017.02.001
论文题名: Expanded Florida reef development during the mid-Pliocene warm period
作者: Klaus J.S. ; Meeder J.F. ; McNeill D.F. ; Woodhead J.F. ; Swart P.K.
刊名: Global and Planetary Change
ISSN: 0921-8181
出版年: 2017
卷: 152 起始页码: 27
结束页码: 37
语种: 英语
英文关键词: Coral reefs
; Florida
; Mid Pliocene warm period
; Sea level
; Tamiami formation
Scopus关键词: Atmospheric temperature
; Climate change
; Glacial geology
; Oceanography
; Sea level
; Storms
; Submarine geophysics
; Surface properties
; Surface waters
; Tropics
; Coral reef
; Detrended correspondence analysis
; Florida
; Global climate changes
; Mid-Pliocene
; Northern hemisphere glaciations
; Sea surface temperature (SST)
; Tamiami formation
; Reefs
; Acropora cervicornis
; Anthozoa
; Solenastrea bournoni
; Stylophora (coral)
英文摘要: 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 southern “reef” assemblage with high diversity of stenotopic taxa and a northern “non-reef” assemblage with lower diversity eurytopic taxa. The southern 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 (25.3 °C) are similar to present day values (26 °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. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-85014467429&doi=10.1016%2fj.gloplacha.2017.02.001&partnerID=40&md5=c9a807f4552f9b1fa85d6ea0c8880bd1
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/11735
Appears in Collections: 全球变化的国际研究计划 气候变化与战略
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作者单位: Department of Marine Geosciences, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL, United States
Recommended Citation:
Klaus J.S.,Meeder J.F.,McNeill D.F.,et al. Expanded Florida reef development during the mid-Pliocene warm period[J]. Global and Planetary Change,2017-01-01,152.