In situ occurrence of a gall midge (Insecta, Diptera, Cecidomyiidae) on fossilized angiosperm leaf cuticle fragments from the Pliocene sediments of eastern India

2020 ◽  
Vol 23 (3) ◽  
pp. 762-771
Author(s):  
Manoshi Hazra ◽  
Taposhi Hazra ◽  
Robert A. Spicer ◽  
Subhankar Kumar Sarkar ◽  
Teresa E.V. Spicer ◽  
...  
2018 ◽  
Vol 137 (1-2) ◽  
pp. 399-416 ◽  
Author(s):  
Parth Sarathi Mahapatra ◽  
Rajesh Kumar ◽  
Chinmay Mallik ◽  
Subhasmita Panda ◽  
S. C. Sahu ◽  
...  

1999 ◽  
Vol 11 (2) ◽  
pp. 239-255 ◽  
Author(s):  
E.M. Truswell ◽  
M.E. Dettmann ◽  
P.E. O'Brien

Gravity cores taken from five sites in the Nielsen basin, a sinuous trough on the Mac. Robertson shelf of the East Antarctic continental margin, have yielded non-marine palynofloras of late Early Jurassic to Early Cretaceous age. The palynomorphs occur in glacimarine muds and are thus not in situ, but the composition of the samples indicates that no mixing of individual assemblages has occurred, and that the sediments were deposited very close to outcrop of the source of the palynomorphs. The sequence is oldest at the seaward end of the Nielsen basin, and youngest near the fault-bounded landward end. It is interpreted as reflecting pre-break-up deposition on a passive, rifted continental margin. The age of the assemblages has been established by comparison with the zonal scheme developed in the Perth Basin of Western Australia. Similarity of the Antarctic palynofloras with those known from basins on the east coast of India confirms continental reconstructions that show this part of East Antarctica to have been contiguous with eastern India prior to break-up. The non-marine character of the palynomorphs suggests that marine conditions in this region of the Antarctic margin did not develop until at least late Early Cretaceous time.


2018 ◽  
Vol 2 (2) ◽  
pp. 305-322 ◽  
Author(s):  
Priyanjali Gogikar ◽  
Bhishma Tyagi ◽  
Rashmi Rekha Padhan ◽  
M. Mahaling

1984 ◽  
Vol 75 ◽  
pp. 743-759 ◽  
Author(s):  
Kerry T. Nock

ABSTRACTA mission to rendezvous with the rings of Saturn is studied with regard to science rationale and instrumentation and engineering feasibility and design. Future detailedin situexploration of the rings of Saturn will require spacecraft systems with enormous propulsive capability. NASA is currently studying the critical technologies for just such a system, called Nuclear Electric Propulsion (NEP). Electric propulsion is the only technology which can effectively provide the required total impulse for this demanding mission. Furthermore, the power source must be nuclear because the solar energy reaching Saturn is only 1% of that at the Earth. An important aspect of this mission is the ability of the low thrust propulsion system to continuously boost the spacecraft above the ring plane as it spirals in toward Saturn, thus enabling scientific measurements of ring particles from only a few kilometers.


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