[1]
|
S. Xiao and M. Laflamme, “On the Eve of Animal Radiation: Phylogeny, Ecology and Evolution of the Ediacaran Biota,” Trends in Ecology and Evolution, Vol. 24, No. 1, 2008, pp. 31-40. doi:10.1016/j.tree.2008.07.015
|
[2]
|
T. P. Crimes and D. Mcllroy, “A Biota of Ediacaran Aspect from Lower Cambrian Strata on the Digermul Peninsula, Arctic Norway,” Geological Magazine, Vol. 136, No. 6, 1999, pp. 633-642.
doi:10.1017/S0016756899003179
|
[3]
|
R. K. Bambach, A. H. Knoll and J. J. Sepkoski, “Anatomical and Ecological Constraints on Phanerozoic Animal Diversity in Marine Realm,” Proceedings of the National Academy of Sciences, Vol. 99, No.10, 2007, pp. 6854-6859. doi:10.1073/pnas.092150999
|
[4]
|
B. A. MacGabhann, “Discoidal Fossils of the Ediacaran biota: A Review of Current Understanding,” Geological Society of London: Special Publication, Vol. 286, No. 1, 2007, pp.297-313. doi:10.1144/SP286.21
|
[5]
|
H. S. Pareek, “Quaternary Geology and Mineral Resources of Northwestern Rajasthan,” Memoir of Geological Survey of India, Vol. 115, 1984, pp. 1-95.
|
[6]
|
S. S. Rathore, T. R. Venkatesan and R. K. Srivastava, “Rb/Sr Isotope Dating of Neoproterozoic (Malani Group) Magmatism from Southwest Rajasthan, India: Evidence of Younger Pan-African Thermal Event by 40Ar-39Ar Studies”, Gondwana Research, Vol. 2, No. 2, 1999, pp. 271-181. doi:10.1016/S1342-937X(05)70151-9
|
[7]
|
A. Mazumdar and H. Staruss, “Sulfur and Strontium Isotopic Compositions of Carbonate and Evaporate Rocks from the Late Neoproterozoic—Early Cambrian Bilara Group (Nagaur-Ganganagar Basin, India): Constraints on Intrabasinal Correlation and Global Sulfur Cycle,” Precambrian Research, Vol. 149, No. 3-4, 2006, pp. 217-230.
doi:10.1016/j.precamres.2006.06.008
|
[8]
|
M. K. Pandit, A. N. Sial, S. S. Jamrani and V. P. Ferreira, “Carbon Isotope Profile across the Bilara Group Rocks of Trans Aravalli Marwar Supergroup in Western Rajasthan, India: Implications for Neproterozoic-Cambrian Transition,” Gondwana Research, Vol. 4, No. 3, 2001, pp. 387394. doi:10.1016/S1342-937X(05)70338-5
|
[9]
|
P. Srivastava, “Treptichnus pedum: An Ichnofossil Representing Ediacaran-Cambrian Boundary in the Nagaur Group, the Marwar Supergroup, Rajasthan, India,” Proceedings Indian National Science Academy, Vol. 78, No. 2, 2012, pp. 161-169..
|
[10]
|
B. Prasad, R. Asher and B. Bargohai, “Late Neoproterozoic (Ediacaran)—Early Palaeozoic (Cambrian) Acritarchs from the Marwar Supergroup, Bikaner-Nagaur Basin, Rajasthan,” Geological Society of India, Vol. 75, No. 2, 2010, pp. 415-431.
|
[11]
|
S. Kumar and S. K. Pandey, “Note on the Occurrence of Arumberia banksi and Associated Fossils from the Jodhpur Sandstone, Marwar Supergroup, Western Rajasthan,” Journal Palaeontological Society of India, Vol. 54, No. 2, 2009, pp. 171-178.
|
[12]
|
P. Srivastava, “Problematic Worms and Priapulid—Like Fossils from the Nagaur Group, the Marwar Supergroup, India,” Ichnos, Vol. 19, No. 3, 2012, pp. 156-164.
doi:10.1080/10420940.2012.702606
|
[13]
|
D. S. Chauhan, B. Ram and N. Ram, “Jodhpur Sandstone: A Gift of Ancient Beaches to Western Rajasthan,” Journal Geological Society of India, Vol. 64, 2004, pp. 265276.
|
[14]
|
S. Sarkar, P. K. Bose, P. Samanta, P. Sengupta and P. Eriksson, “Microbial Mat Mediated Structures in the Ediacaran Sonia Sandstone, Rajasthan, India and Their Implications for Proterozoic Sedimentation,” Precambrian Research, Vol. 162, No. 1-2, 2008, pp. 248-263.
doi:10.1016/j.precamres.2007.07.019
|
[15]
|
S. Kumar, P. K. Misra and S. K. Pandey, “Ediacaran Megaplant Fossils with Vaucherian Affinity from the Jodhpur Sandstone, Marwar Supergroup, Western Rajasthan,” Current Science, Vol. 97, No. 5, 2009, pp. 701705.
|
[16]
|
K. S. Raghav, C. De and R. L. Jain, “The First Record of Vendian Medusoids and Trace Fossil Bearing Algal Mat Ground from the Basal Part of the Marwar Supergroup of Rajasthan, India,” Indian Minerals, Vol. 59, No. 1-2, 2005, pp. 2330.
|
[17]
|
D. Mcllroy, T. P. Crimes and C. J. Pauley, “Fossils and Matgrounds from the Neoproterozoic Longmyndian Supergroup, Shropshire, UK,” Geological. Magazine, Vol. 142, No. 4, 2005, pp. 441-455.
doi:10.1017/S0016756805000555
|
[18]
|
M. L. Droser and J. G. Gehling, “Synchronous Aggregate Growth in an Abundant New Ediacaran Tubular Organism,” Science, Vol. 319, No. 5870, 2008, pp. 1660-1662.
doi:10.1126/science.1152595
|
[19]
|
N. J. Butter?eld, “Probable Proterozoic Fungi,” Palaeobiology, Vol. 31, No. 1, 2005, pp. 165-182.
doi:10.1666/0094-8373(2005)031<0165:PPF>2.0.CO;2
|
[20]
|
B. R. Vashishtha, “Botany for Degree Students. Part-1,” Algae, S. Chand and Company Limited, 1977, p. 545.
|
[21]
|
M. A. Fedonkin, “Nonskeletal Fauna of the Podolian Pridnyestrovya,” In: V. A. Velikanov, E. A. Aseeva and M. A. Fedonkin, Eds., Vend Ukrainy, Nauk Dumka, Kiev, 1983, pp.128-139.
|
[22]
|
G. M. Narbonne and J. D. Aitken, “Ediacaran Fossils from the Sekwi Brook Area, Mackenzie Mountains, Northwestern Canada,” Journal of Palaeontology, Vol. 33, No. 4, 1990, pp. 945-980.
|
[23]
|
B. S. Sokolov, “Organic World of the Earth on Its Way to the Phanerozoic Differentiation,” Vestrik Akademii, Nauk SSSR, Vol. 1, 1976, pp. 126-143.
|
[24]
|
J. B. Caron and A. Jackson, “Palaeoecology of the Greater Phyllopod Bed Community, Burgess Shale,” Palaeogeography, Palaeoclimatology and Palaeoecology, Vol. 258, No. 3, 2008, pp. 222-256.
doi:10.1016/j.palaeo.2007.05.023
|
[25]
|
G. M. Narbonne, “The Ediacara Biota: Neoproterozoic Origin of Animals and Their Ecosystems,” Annual Review of Earth and Planetary Science, Vol. 33, No. 1, 2005, pp. 421-442.
doi:10.1146/annurev.earth.33.092203.122519
|
[26]
|
N. C. Hughes, “Morphological Plasticity and Genetic Flexibility in a Cambrian Trilobite,” Geology, Vol. 19, No. 9, 1991, pp. 913-916.
doi:10.1130/0091-7613(1991)019<0913:MPAGFI>2.3.CO;2
|
[27]
|
S. Kumar and S. K. Pandey, “Trace Fossils from the Nagaur Sandstone, Marwar Supergroup, Dulmera Area, Bikaner District, Rajasthan, Indian,” Journal of Asian Earth Science, Vol. 38, No. 3-4, 2010, pp. 77-85.
|