3 edition of Late Oligocene to Pliocene evolution of the central portion of the south Florida platform found in the catalog.
Late Oligocene to Pliocene evolution of the central portion of the south Florida platform
T. M. Missimer
Includes bibliographical references (p. 167-184).
|Statement||by Thomas M. Missimer.|
|Series||Bulletin,, no. 65, Geological bulletin (Tallahassee, Fla.) ;, no. 65.|
|LC Classifications||QE99.A3 no. 65, QC380.15|
|The Physical Object|
|Pagination||xii, 184 p. :|
|Number of Pages||184|
|LC Control Number||2003505231|
The other trend was mostly confined to South America, which was isolated from North America during the Oligocene epoch (the Central American land bridge would not form for another 20 million years) and hosted a bizarre array of megafauna mammals, including the elephant-like Pyrotherium and the meat-eating marsupial Borhyaena (the marsupials of Oligocene South . Oligocene. The Oligocene epoch (39 to 22 million years ago) is the transition period between the earlier and later Tertiary period (65 to 2 million years ago).. A key feature of evolution is the ripple effect created by geographical changes that influence climate and therefore vegetation and ultimately the ways in which animals develop. The most important geographical event .
The end of the Pleistocene epoch (20, to 12, years ago) was marked by a global ice age, which led to the extinction of many megafauna most people don't know is that this capitalized "Ice Age" was the last of no less than 11 Pleistocene ice ages, interspersed with more temperate intervals called "interglacials.'During these periods, much of . Missimer TM () Late Oligocene to Pliocene evolution of the central portion of the south Florida Platform: Mixing of siliciclastic and carbonate Sediments. Fla Geol Surv Bull 65 Google Scholar Navoy AS () Hydrogeologic data from a 2,foot deep core hole at Polk City, Green Swamp area, central Florida.
Abstract. The fast growing calcareous skeletons of zooxanthellate reef corals (z corals) represent unique environmental proxy archives through. Age indicators in lower part are early to late Oligocene ( to Ma); age indicators for Nocatee are late Oligocene ( to Ma); age indicators for Tampa range from late Oligocene to middle Miocene ( to Ma); and age indicators for upper part range from late Oligocene to middle Miocene ( to Ma). 87Sr/86Sr data from.
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Department of Environmental Protection, is publishing as its Bulle Late Oligocene to Pliocene Evolution of the Central Portion of the South Florida Platform: of Siliciclastic and Carbonate Sediments, by Thomas M.
Missimer. This report summarizes the results of a multi-year investigation of the lithostratigraphy. Late Oligocene to Pliocene evolution of the central portion of the south Florida platform.
Tallahassee, FL: Florida Geological Survey, (OCoLC) Online version: Missimer, T.M. Late Oligocene to Pliocene evolution of the central portion of the south Florida platform. Tallahassee, FL: Florida Geological Survey, (OCoLC) Late Oligocene to Pliocene evolution of the central portion of the south Florida platform.
Tallahassee, FL: Florida Geological Survey, (DLC) (OCoLC) Material Type: Document, Government publication, State or province government publication, Internet resource: Document Type: Internet Resource, Computer File. Therefore, the southern Florida ramp deposited during the late Oligocene to early Pliocene was more similar to a restricted-sea ramp than a wave-dominated ramp.A new chronostratigraphy was developed for the upper Paleogene and Neogene sediments on the central part of the South Florida by: 8.
Late oligocene to pliocene evolution of the central portion of the south Florida platform. By Thomas M Missimer. Abstract (Bibliography) Includes bibliographical references (p. )Series statement: Bulletin - Florida Geological Society ; 65(Statement of Responsibility) by Thomas M.
Missimer Author: Thomas M Missimer. The Pliocene (/ ˈ p l aɪ. ə ˌ s iː n, ˈ p l aɪ. oʊ-/ PLY-ə-seen, PLY-oh-; also Pleiocene) Epoch is the epoch in the geologic timescale that extends from million to million years is the second and youngest epoch of the Neogene Period in the Cenozoic Pliocene follows the Miocene Epoch and is followed by the Pleistocene Epoch.
Prior to the revision of the. Late oligocene to pliocene evolution of the central portion of the south Florida platform: mixing of siliciclastic and carbonate sediments / by Thomas M. Missimer. By T. Missimer. Abstract. xii, p. The hiatal gap along the upper sequence boundary (SB-B), marking the Arcadia Formation overlain by Miocene–Pliocene sediments that vary in age and composition regionally, records the same increase from the central part of the platform (southwest Florida, Arcadia Fm/Peace River Fm, ∼ m.y.) to the south platform edge (lower Florida Keys.
Oligocene Epoch, third and last major worldwide division of the Paleogene Period ( million to 23 million years ago), spanning the interval between million to 23 million years ago.
The Oligocene Epoch is subdivided into two ages and their corresponding rock stages: the Rupelian and the followed the Eocene Epoch and was succeeded by the Miocene Epoch, the. The tectonic and geodynamic evolution of the Pelagian platform and of the Pantelleria Rift System, located in the foreland of the Apennine‐Sicilian‐Maghrebian Belt, from the Late Oligocene onward, is still debated.
Here we present a new interpretation based on structural data collected in the Malta and Gozo islands. The evolution of the horse, a mammal of the family Equidae, occurred over a geologic time scale of 50 million years, transforming the small, dog-sized, forest-dwelling Eohippus into the modern horse.
Paleozoologists have been able to piece together a more complete outline of the evolutionary lineage of the modern horse than of any other animal. Much of this evolution.
a deep-water carbonate platform: the florida margin west florida slope (m.y) ag e 0-~ i0 20 30 40 50 60 70 80 90 i00 i1(~ eustatic curves on ramp mid- to late miocene isthmus of panama closure m~ loop current fntensification late oligocene-- probradatioi mid-miocene ano pelab,c suwannee straits closure~ loop current.
Late Oligocene to Pliocene evolution of the central portion of the south Florida platform: mixing o Thomas M. Missimer Thesis (Ph. D.)--University of Miami, Thomas M.
Scott's 13 research works with citations and reads, including: Geology and hydrology of Lee County, Florida (Boggess Memorial Publication).
Missimer TM () Late Oligocene to Pliocene evolution of the central portion of the South Florida Platform: mixing of siliciclastic and carbonate sediments. Fla Geol Surv Bull 65 Google Scholar Missimser TM Maliva RG () Tectonically induced fracturing, folding and groundwater flow in south Florida.
The size of the exposed portion of the Platform changed dramatically over geologic time as sea level rose and fell (from Hine ; Geologic History of Florida: Major Events That Formed the Sunshine State by Albert C.
Hine. Gainesville: University Press of Florida, Missimer, T.M.,Late Oligocene to Pliocene evolution of the central portion of the South Florida Platform: mixing of siliciclastics and carbonate sediments (Ph.D.
dissertation: Coral Gables, Florida, University of Miami, 2 volumes, and p. Missimer, T.M.,Late Oligocene to Pliocene evolution of the central portion of the South Florida Platform: mixing of siliciclastic and carbonate sediments (Ph.D. dissertation): Coral Gables, Florida, University of Miami, 2 volumes, and p.
The Oligocene Epoch Million Years Ago. Early Oligocene, After a hiatus, carbonate deposition continues as the Suwannee Limestone is laid down and the Florida Platform persists as a subtropical carbonate bank, very similar to the present Bahamas. Massive coral reefs are now prominent.
Late Oligocene. The tropics diminished, giving way to cooler woodlands and grasslands. Although there was a slight warming period in the late Oligocene, the overall cooling trend was to continue, culminating in the Ice Ages of the Pleistocene.
Plant Life. By the Oligocene the major evolution and dispersal of modern types of angiosperms had occurred. From the Early Cretaceous to the Late Eocene, the southern part of the Florida Platform was isolated by the channel to the north and the Florida Straits to the south, which limited deposition on the platform to carbonate sediments, and at times locally evaporites, similar to the modern Bahamas Platform (Hull, ; Puri & Vernon, ; Randazzo & Jones, ).Late oligocene to pliocene evolution of the central portion of the south Florida platform.
Significance of caves in watershed management and protection in Florida. Springs of Florida (FGS: Bulletin 66) Workshop to develop blue prints for the management and protection of Florida .First test: time scale and associated primates and characteristics, some evolution vocab Learn with flashcards, games, and more — for free.