Climatic signatures in shallow-water carbonates: high-resolution stratigraphic markers in structurally controlled carbonate buildups (Late Miocene, southern Spain)

2001 ◽  
Vol 175 (1-4) ◽  
pp. 211-237 ◽  
Author(s):  
Thomas C Brachert ◽  
Nadja Hultzsch ◽  
Andrea C Knoerich ◽  
Uwe M.R Krautworst ◽  
Oliver M Stückrad
Keyword(s):  
High Resolution ◽  
Shallow Water ◽  
Late Miocene ◽  
Southern Spain ◽  
Carbonate Buildups

HIGH RESOLUTION CHRONOLOGY USING ROCK MAGNETIC CYCLOSTRATIGRAPHY IN THE BAZA BASIN, SOUTHERN SPAIN

2020 ◽  
Author(s):  
Monica C. Powers ◽  
◽  
David Anastasio ◽  
Josep M. Pares ◽  
M. Duval ◽  
...  
Keyword(s):  
High Resolution ◽  
Southern Spain

scholarly journals Shallow water seagrass observed by high resolution full waveform bathymetric LiDAR

2014 ◽  
Author(s):  
Zhigang Pan ◽  
Juan Carlos Fernandez-Diaz ◽  
Craig L. Glennie ◽  
Michael Starek
Keyword(s):  
High Resolution ◽  
Shallow Water ◽  
Full Waveform

Rich shallow-water benthic ecosystem in Late Miocene East Antarctica (Fisher Bench Fm, Prince Charles Mountains)

2017 ◽  
Vol 133 ◽  
pp. 40-49 ◽  
Author(s):  
Wojciech Majewski ◽  
Andrzej Tatur ◽  
Jakub Witkowski ◽  
Andrzej Gaździcki
Keyword(s):  
Shallow Water ◽  
Late Miocene ◽  
East Antarctica

scholarly journals The distribution of <i>Triebelina raripila</i> and <i>Carinocythereis carinata</i> (Ostracoda) from the Middle Miocene of the Central Paratethys and their palaeogeographic implications

1998 ◽  
Vol 17 (2) ◽  
pp. 125-130 ◽  
Author(s):  
J. Szczechura
Keyword(s):  
Shallow Water ◽  
Late Miocene ◽  
Middle Miocene ◽  
Early Miocene ◽  
Central Paratethys ◽  
Eastern Paratethys ◽  
Main Species ◽  
Late Middle Miocene ◽  
The Mediterranean

Abstract. Late Middle Miocene (Upper Badenian) strata of the Fore-Carpathian Depression of Poland yield a shallow-water ostracod fauna which contains the species Triebelina raripila (G. W. Müller, 1894) and Carinocythereis carinata (Roemer, 1838). The palaeobiogeographic distribution of the two main species suggests, that in the late Middle Miocene, Central Paratethys was still connected to the Mediterranean, although still separated from the Eastern Paratethys and from southeastern Eurasia. The continuous occurrence of Triebelina raripila and Carinocythereis carinata in the Mediterranean basins, from the Early Miocene to Recent, indicates that marine conditions existed throughout, thereby allowing them to survive the Late Miocene salinity crisis.

Deep-sea panoramas: Progress and remaining challenges in late Miocene stratigraphy and climate

2021 ◽  
Author(s):  
Anna Joy Drury ◽  
Thomas Westerhold ◽  
David A. Hodell ◽  
Mitchell Lyle ◽  
Cédric M. John ◽  
...  
Keyword(s):  
High Resolution ◽  
Ocean Circulation ◽  
Late Miocene ◽  
Deep Sea ◽  
Deep Ocean ◽  
High Resolution Data ◽  
Ongoing Work ◽  
Climate Evolution ◽  
Deep Ocean Circulation ◽  
Geological Timescale

&lt;p&gt;During the late Miocene, meridional sea surface temperature gradients, deep ocean circulation patterns, and continental configurations evolved to a state similar to modern day. Deep-sea benthic foraminiferal stable oxygen (&amp;#948;&lt;sup&gt;18&lt;/sup&gt;O) and carbon (&amp;#948;&lt;sup&gt;13&lt;/sup&gt;C) isotope stratigraphy remains a fundamental tool for providing accurate chronologies and global correlations, both of which can be used to assess late Miocene climate dynamics. Until recently, late Miocene benthic &amp;#948;&lt;sup&gt;18&lt;/sup&gt;O and &amp;#948;&lt;sup&gt;13&lt;/sup&gt;C stratigraphies remained poorly constrained, due to relatively poor global high-resolution data coverage.&lt;/p&gt;&lt;p&gt;Here, I present ongoing work that uses high-resolution deep-sea foraminiferal stable isotope records to improve late Miocene (chrono)stratigraphy. Although challenges remain, the coverage of late Miocene benthic &amp;#948;&lt;sup&gt;18&lt;/sup&gt;O and &amp;#948;&lt;sup&gt;13&lt;/sup&gt;C stratigraphies has drastically improved in recent years, with high-resolution records now available across the Atlantic and Pacific Oceans. The recovery of these deep-sea records, including the first astronomically tuned, deep-sea integrated magneto-chemostratigraphy, has also helped to improve the late Miocene geological timescale. Finally, I will briefly touch upon how our understanding of late Miocene climate evolution has improved, based on the high-resolution deep-sea archives that are now available.&lt;/p&gt;

High-resolution sequence biostratigraphy of a lowstand prograding deltaic wedge: Oso Field (late Miocene), Nigeria

1999 ◽  
Vol 152 (1) ◽  
pp. 259-290 ◽  
Author(s):  
J. M. Armentrout ◽  
L. B. Fearn ◽  
K. Rodgers ◽  
S. Root ◽  
W. D. Lyle ◽  
...  
Keyword(s):  
High Resolution ◽  
Late Miocene
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