Fluctuations of the oxygen minimum zone at the end of Oceanic Anoxic Event 2 in the Gulf of Mexico and the response of ammonites

2015 ◽  
Vol 134 (2) ◽  
pp. 217-225 ◽  
Author(s):  
Christina Ifrim
Geology ◽  
2011 ◽  
Vol 39 (11) ◽  
pp. 1043-1046 ◽  
Author(s):  
Christina Ifrim ◽  
Stefan Götz ◽  
Wolfgang Stinnesbeck

2019 ◽  
Vol 517 ◽  
pp. 50-60 ◽  
Author(s):  
Florian Scholz ◽  
Sebastian Beil ◽  
Sascha Flögel ◽  
Moritz F. Lehmann ◽  
Ann Holbourn ◽  
...  

2010 ◽  
Vol 61 (2) ◽  
pp. 111-120 ◽  
Author(s):  
Mohamed Soua

Time series analysis (orbital cycles) of the uppermost Cenomanian-Lower Turonian sequence on the southern Tethyan margin using foraminiferaTime series analysis has been performed for the first time on the Cenomanian-Turonian sequence in Central Tunisia in order to shed light on its Milankovitch-like cyclicity. This analysis was applied to two foraminiferal genera: the biserialHeterohelix, an oxygen-minimum zone (OMZ) dweller, and the triserialGuembelitria, a eutrophic surface dweller. Average sedimentary rates and the duration of the oceanic anoxic event (OAE2) in each studied section were estimated. The fluctuations in abundance of these two opportunistic species can be related mainly to both precessional (ca. 20 kyr) and eccentricity (100 and 400 kyr) cyclicity suggesting that changes in surface water fertility were linked to climate changes in the Milankovitch frequency band.


2014 ◽  
Vol 73 (1) ◽  
pp. 51-67 ◽  
Author(s):  
A Jain ◽  
M Bandekar ◽  
J Gomes ◽  
D Shenoy ◽  
RM Meena ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document