Eocene climate record of a high southern latitude continental shelf: Seymour Island, Antarctica

2008 ◽  
Vol 120 (5-6) ◽  
pp. 659-678 ◽  
Author(s):  
L. C. Ivany ◽  
K. C. Lohmann ◽  
F. Hasiuk ◽  
D. B. Blake ◽  
A. Glass ◽  
...  
GFF ◽  
2000 ◽  
Vol 122 (1) ◽  
pp. 43-43
Author(s):  
Andrea L. Dutton ◽  
Kyger C Lohmann ◽  
William J. Zinsmeister

PLoS ONE ◽  
2012 ◽  
Vol 7 (7) ◽  
pp. e41672 ◽  
Author(s):  
Rachel V. Downey ◽  
Huw J. Griffiths ◽  
Katrin Linse ◽  
Dorte Janussen

2009 ◽  
Vol 10 (1) ◽  
pp. n/a-n/a ◽  
Author(s):  
K. P. Lawrence ◽  
L. Tauxe ◽  
H. Staudigel ◽  
C. G. Constable ◽  
A. Koppers ◽  
...  

2018 ◽  
Vol 176 ◽  
pp. 05038 ◽  
Author(s):  
Boris Barja ◽  
Felix Zamorano ◽  
Pablo Ristori ◽  
Lidia Otero ◽  
Eduardo Quel ◽  
...  

A tropospheric lidar system was installed in Punta Arenas, Chile (53.13°S, 70.88°W) in September 2016 under the collaboration project SAVERNET (Chile, Japan and Argentina) to monitor the atmosphere. Statistical analyses of the clouds and aerosols behavior and some cases of dust detected with lidar, at these high southern latitude and cold environment regions during three months (austral spring) are discussed using information from satellite, modelling and solar radiation ground measurements.


2012 ◽  
Vol 86 (1) ◽  
pp. 126-128
Author(s):  
Rodney M. Feldmann ◽  
Jeffrey D. Stilwell

Recognition of a fossil previously identified as a “large Cretaceous beetle” as a glypheid lobster permits the definition of a new species, Glyphea wiffenae. The specimen was collected from the richly fossiliferous, Upper Cretaceous Maungataniwa Sandstone in eastern North Island, New Zealand. Several other fossil decapods with high southern latitude affinities have been described previously from the unit, supporting the placement of the Zealandia region within the Weddellian Biotic Province. This is only the fourth glypheid known from New Zealand and the first Cretaceous occurrence of the genus in the country.


2018 ◽  
Author(s):  
James Witts ◽  
Vanessa C. Bowman ◽  
Paul Wignall ◽  
J. Alistair Crame ◽  
Jane Francis ◽  
...  

One of the most expanded records to contain the final fortunes of ammonoid cephalopods is within the López de Bertodano Formation of Seymour Island, James Ross Basin, Antarctica. Located at ~65º South now, and during the Cretaceous, this sequence is the highest southern latitude onshore outcrop containing the Cretaceous–Paleogene (K–Pg) transition. We present comprehensive new biostratigraphic range data for 14 ammonite and one nautiloid species based on the collection of >700 macrofossils from high-resolution sampling of parallel sedimentary sections, dated Maastrichtian to earliest Danian in age, across southern Seymour Island. We find evidence for only a single, abrupt pulse of cephalopod extinction at the end of the Cretaceous when the final seven ammonite species disappeared, consistent with most evidence globally. In the lead up to the K–Pg extinction in the James Ross Basin, starting during the Campanian, ammonite diversity decreased overall, but the number of endemic taxa belonging to the family Kossmaticeratidae actually increased. This pattern continued into the Maastrichtian and may be facies controlled, linked to changes in sea level and seawater temperature. During the early Maastrichtian, ammonite diversity dropped significantly with only two species recorded from the basal López de Bertodano Formation on Seymour Island. The subsequent diversification of endemic taxa and reappearance of long-ranging, widespread species into the basin resulted in an increase in ammonite diversity and abundance during the mid-Maastrichtian. This was coincident with an apparent period of warming temperatures and sea level rise interpreted from palynology and sedimentology, perhaps reflecting a high latitude expression of the Mid-Maastrichtian Event. Late Maastrichtian diversity levels remained stable despite reported climatic and environmental variation. Ammonite diversity patterns during the Maastrichtian parallel those of microfossil species such as nannofossil and planktonic foraminifera, suggesting that dynamic climatic and environmental changes affected many planktonic and nektonic organisms during the latest Cretaceous. However, we suggest that these perturbations had a minimal effect on overall diversity prior to the catastrophic extinction event at the K–Pg boundary.


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