Cambay Shale Formation Research Articles

Early Eocene biotic assemblage from the sedimentary deposits of the Tarkeshwar Lignite Mine, Gujarat and its palaeoenvironmental implications

The Palaeogene biota and the palaeoenvironmental history from the low latitudes are remarkably well–preserved in theopen–cast lignite deposits from Western India. Lignite sequences of the Cambay Shale Formation (Gujarat) have been a majorsource to understand the concept of early evolution of fossils including flora, arthropods, vertebrates fauna, and several aquaticforms during the Early Eocene. The study deals with an extensive record of amber inclusions and extracted pollen, vertebratefragments, dinoflagellate cysts and Carbon isotopes from the lignite and associated sediments from the Tarkeshwar Lignite Mineto add insights into the palaeoenvironment and depositional conditions of the Cambay Basin during the Early Eocene period. Thecurrent study demonstrates that throughout the late Palaeocene and early Eocene epoch, the palaeoenvironment changed fromlow land, marshy (lower portion), to shallow marine environment, presumably due to hyperthermal event PETM (middle part).Age diagnostic taxa, viz. Auxiodinium longispinosum, Apectodinium parvum and early wetzelielloid (Vallodinium? sp.) excursionprovide late Palaeocene–early Eocene period (~56–53 Ma) for the dinocyst interval in the middle part of the section. A pronouncednegative Carbon Isotope Excursion (CIE) in the middle part is correlated to the second Eocene Thermal maximum (53.7 Ma),which is a globally recorded hyperthermal event. During the ETM–2 warming, the rise in pCO2 caused warm, humid conditionsas well as a rise in sea level, which may have contributed to the establishment of constrained shallow marine environments in theexamined middle unit sedimentary succession. Floral (spore–pollens, leaf, wood, seed, fruits) and faunal assemblages (Crocodiles,fish remains, amber insects) revealed the prevalence of a dense tropical luxurious rain forest (floral and faunal) near shore duringthe ETM–2 in the Tarkeshwar Lignite Mines, Cambay Basin.

Organofacies and source evaluation of Cambay Shale Formation to assess unconventional hydrocarbon potential in Jambusar–Broach area, Cambay Basin, India

Organofacies and source evaluation of Cambay Shale Formation to assess unconventional hydrocarbon potential in Jambusar–Broach area, Cambay Basin, India

Authigenic Fe Mineralization in Shallow to Marginal Marine Environments: A Case Study from the Late Paleocene—Early Eocene Cambay Shale Formation

The late Paleocene–early Eocene warm greenhouse conditions, characterized by elevated pCO2 levels in the atmosphere and a dramatic increase in sea surface temperature, prompted abundant authigenic glauconite formation within the shallow marine sediments worldwide by lowering the net sedimentation rate, increasing organic productivity and expanding the oxygen minimum zones to shallow oceans. The early Eocene marginal marine Cambay Shale Formation experienced episodes of marine inundation represented by limestone–green shale alternations. The shales host abundant authigenic light-green, dark-green, and brown pellets. A detailed characterization of the pellets of the Valia and Vastan lignite mines, integrating the sedimentological, petrographical, mineralogical, and mineral geochemical data, suggests two distinct varieties of Fe–silicate formation, viz. glauconite and chamosite. While the glauconitic green pellets are ubiquitous to Valia and Vastan mines, brown chamosite pellets are confined within the basal part of the green shale facies alternating with fossiliferous limestone in the Vastan mine. The glauconites of the Valia mine manifest a ‘nascent’ to ‘slightly evolved’ maturation stage of glauconitization, whereas the glauconites of the Vastan mine represent the ‘evolved’ type. The limestone–green shale alternation in the Valia mine is overlain by a ~4 m-thick spherulitic mudstone facies comprising monomineralic sideritic spherulites, reflecting a pure FeCO3 composition. The glauconites in the Cambay Shale Formation transformed from kaolinite-rich clay pellets under dys-oxic depositional conditions. The increasing anoxicity within the microenvironment, possibly amplified by the rapid oxidation of continent-derived organic matter, facilitated chamosite formation instead of glauconite. The increased freshwater influx into the marginal marine depositional environment resulted in immature, K-poor glauconites of the Valia mine. The formation of siderite spherulites overlying the limestone–green shale alternation relates to the beginning of the regressive phase of sedimentation.

Petrographical-geochemical characteristics and floral-faunal compositions of the Valia lignite deposits from Cambay Basin (Gujarat), western India

Lignite-bearing sequence of the Valia mine, associated with the Cambay Shale Formation (early Eocene) in Cambay Basin of western Indian State Gujarat, has been studied. An integrated approach (including organic petrography, palynofacies, palynology, entomology, geochemistry) has been adopted to assess the origin and characters of lignite deposits and their potential for the hydrocarbon generation, besides to understand the evolution and interaction of different biotic (floral-faunal) groups of the geological time. The studied samples (lignites/shales) are characterized by the domination of huminite group (av. 67 vol.%)/phytoclasts (av. 58%) along with the abundance of short-chain n-alkanes (bacterial activity). The frequencies of detrohuminite sub-group, non-biostructured elements, macrophyte-derived amorphous organic matter (AOM, mainly), and high values of proxy aqueous are indicating the elevated bacterial degradation of the OM and/or also suggest the significant contribution of the herbaceous vegetation/aquatic macrophytes/algal input to the palaeo-peat. The relative abundance of hopanes and low values of the steroids/hopanoids ratios further indicate a high bacterial activity. On the other hand, the contents of telohuminite, liptinite group, and cuticle elements together with the high carbon preference index, low proxy wax, and terrigenous/aquatic ratios confirm both terrestrial and macrophyte contributions during the peat accumulation. Fascinatingly, we have found Dipterocarpus-derived amber (fossil resin) within the lignite seam (lower) with remarkably well-preserved arthropod inclusions consisting of arachnids and insects. Generally, insects have an association with flora and provide important ecosystem functions. In the studied amber samples, the insects to arachnids (spiders and pseudoscorpions) ratio is 3:1. Their quantitative analysis indicates the dominance of the Chironomidae (non-biting midges 32%) followed by Araneae, Myrmicinae, Cecidomyiidae, and Mycetophilidae. A rare entity such as pseudoscorpions has also been found during the investigation.The derived petrographic indices indicate that the peat-forming limno-telmatic vegetation was accumulated mainly in back-barrier settings with high groundwater (mesotrophic to rheotrophic) condition. The contents of pyrite (mainly framboidal) mineral and sulphur (0.69–2.24 wt.%) suggesting that peat had experienced the marine influx. Further, the high occurrence of funginite maceral (among inertinite group), and spores of family Microthyriaceae point towards a warm and moist condition. The plotting of palynofacies data on Tyson's APP diagram, and the values of pristane/phytane ratio suggest that the OM was primarily deposited in dysoxic to suboxic settings. The high incidence of family Chironomidae, non-biostructured and low cuticle contents indicate the proximal settings and a low energy environment like lake/pond or marshlands. However, the occurrence of granular-AOM along with high (relatively) opaque phytoclast contents in the upper part indicates that distal settings were formed at the termination of the OM accumulation. The total organic carbon (TOC) contents and hydrogen index values in the studied samples indicate a good to excellent source for the hydrocarbon generation. However, the low gross calorific value (av. 4467 cal/g), values of Tmax (mostly below 435 °C), and H/C and O/C atomic ratios showing that the samples are of immature (early diagenetic stage; huminite reflectance value: av. 0.28%) nature of the OM. Moreover, the different cross plots (hydrogen index (HI) vs. oxygen index (OI), S2vs. TOC, HI vs. Tmax) indicate that the Valia lignite-bearing succession contains admixed type-III/II kerogen, and can generate gaseous and some liquid hydrocarbons upon maturation or with additional heating.

Heterogeneity characterization from sequence stratigraphic analysis of Paleocene-Early Eocene Cambay Shale formation in Jambusar-Broach area, Cambay Basin, India

The heterogeneity of shale is significant for the evaluation and prediction of shale gas reservoir. In terms of core observations, electrolog data and correlations, the macroscopic and microscopic heterogeneity of Cambay Shale Formation, Cambay Basin, India is characterized and discussed at different scales. The formation is deposited through Paleocene to early Eocene due to marine transgression in the basin. Upper contact of the formation is represented by the Early/Middle Eocene hiatus or ‘Y’ marker, a 2nd order sequence boundary. The formation is subdivided as Older Cambay Shale (OCS) member and Younger Cambay Shale (YCS) member by Paleocene top or ‘Neck’ marker, a 1st order sequence boundary. Cambay Shale is the primary source rock of hydrocarbon in the basin and is considered to be homogenous. Log motif and core analysis suggest that the Cambay Shale is not homogeneous “shale”. Based on sequence stratigraphic analysis, a total of eleven lower order high frequency (3rd order) transgressive-regressive (T-R) sequences have been identified, seven within YCS member (Early Eocene, i.e. between ‘Y’ and ‘N’ Marker) and remaining four in OCS member (Paleocene, i.e. below ‘N’ Marker). These T-R sequences are thick in southern or central part of the basin while thinning towards the basin margin.The Cambay Shale Formation is divisible into three types of facies based on core studies. The top part of each T-R sequence is attributed with coarsening upward HST while the bottom part is fining upward TST, separated by marine flooding events. Quartz and carbonate mineral fractions are dominant in HST as compared to TST of each sequence. This approach of heterogeneity characterization from sequence stratigraphic analysis helps in identification of different sequences (T-R sequences) and provides clues in identifying broader distribution of brittle-ductile couplets within each T-R sequence in the heterogenous Cambay Shale Formation. This gives an impetus to identify suitable prospective locales to explore unconventional hydrocarbon potential in the study area.

Reaction kinetic, maturity, burial and thermal histories modelling of cambay shale source rocks, Cambay Basin, Western India

The Cambay Shale Formation (CSF), the known source rock for conventional oil and gas, now becomes a key target for shale oil/gas exploration in the Cambay Basin. In the present study, maturity, wellbore temperature and kerogen kinetics data from the several locations in the Cambay Basin have been integrated into PetroMod®, a basin and petroleum system modelling (BPSM) software, to generate maturity profile, burial and thermal history in the Cambay Basin. The Optkin program optimised kerogen kinetic results indicated that the activation energy for the type III kerogens, which are prominently available in the basin, varies widely (44–72 kcal/mol). A sample from Mehsana-Ahmedabad Block shows a narrow activation energy range (40–50 kcal/mol), a characteristics of type II kerogen and the maximum (91%) of the initial petroleum potential is contributed by a single activation energy (46 kcal/mol). BPSM models indicate that the major portion of the CSF in the north of the basin is mainly under early and main oil generation window, where shale oil prospect can be explored. Compared to the north part of the basin where late oil and wet gas generation windows enter into the Olpad Formation at ~2700 m and ~3100 m respectively, the source rocks, i.e. CSF at the centre of the Broach block in the South Cambay Basin indicate the presence of late oil and wet gas generation windows at ~3100 m and ~3900 m, respectively. The models generated in the study area suggest that the deeper section of the South Cambay Basin may have prospective for shale oil/gas.

“Out-of-India” dispersal for Adina (tribe Naucleeae; family Rubiaceae): evidence from the early Eocene fossil record from India

This study reports the oldest fossil record of the genus Adina, A. vastanenesis n. sp., from the early Eocene of Vastan lignite mine (Cambay Shale Formation), Surat district, Gujarat. This fossil wood is characterized by diffuse porous wood, predominantly solitary tylosed vessels, simple perforations, scanty paratracheal to diffuse to sometimes diffuse in aggregate axial parenchyma, predominantly uniseriate to occasionally biseriate rays, and non septate fibres with bordered pits and shows its best resemblance with the modern species, Adina multifolia Haviland, belonging to the tribe Naucleeae (subfamily Cinchonoideae) of the family Rubiaceae. The present discovery becomes the first fossil record of the wood of Adina, which provides an insight about the Gondwanan origin either for the genus Adina or the tribe Naucleeae and its further dispersal to Southeast Asia.

Mössbauer Spectroscopic Study of Samples from Cambay Shale Formation, Cambay Basin, in Context of Shale Gas or Shale Oil

Abstract In Cambay basin (India) a thick sedimentary sequence exits consisting of shales. This sequence is known as Cambay Shale Formation (both younger and older). In the present investigation 57Fe Mössbauer spectroscopy study was carried on samples of Cambay Shale Formation. These samples are collected from various depth interval from well UBER#2. Results thus obtained are also compared with the Mössbauer spectroscopic study already available on shale samples of (from Cambay Shale Formation) well K-263. It was found that samples from well UBER#2 show presence of iron mainly in clay forming minerals in Fe2+ state, but show no presence of pyrite or ferric sulphate minerals. In contrast sample studied from well K-263 show presence of iron mainly in pyrite and in ferric sulphate but iron clay minerals is absent in most of the samples. Implication of distribution of iron minerals in these wells is discussed in context of future shale oil and shale gas exploration from this basin.

Additional vertebral material of Thaumastophis (Serpentes: Caenophidia) from the early Eocene of India provides new insights on the early diversification of colubroidean snakes

The Ypresian Cambay Shale Formation at Vastan, Mangrol, and Tadkeshwar lignite mines in Gujarat, western India, has yielded a rich vertebrate fauna including madtsoiid, palaeophiid, booid, and colubroidean-like snakes. The latter are particularly abundant, but their systematic affinities are difficult to resolve. Here we describe new specimens of the colubroidean-like snake Thaumastophis missiaeni, including anterior, middle, and posterior trunk vertebrae, as well as caudal vertebrae. The combination of primitive and derived caenophidian and colubroidean vertebral characters confirms Thaumastophis as the earliest known stem-colubriform snake while Procerophis, from the same beds, is more derived and considered to represent a crown-Colubriformes. Additionally, Thaumastophis shares with Renenutet enmerwer from the late Eocene of Egypt a unique combination of vertebral characters that suggests an exchange with North Africa was possible along the southern margin of the Neotethys. We erect the new family Thaumastophiidae for Thaumastophis and Renenutet on the basis of their shared derived vertebral morphology.

Depositional environment and geomechanical properties of Cambay Shale: potential reservoir for shale oil and gas in India

This study aims to investigate mineralogy, depositional environment and rock mechanical properties of Cambay Shale Formation in Jambusar-Broach block of South Cambay Basin, India, by an integrated approach of combining wireline logs and laboratory studies. The study involves the analysis of spectral gamma ray (SGR) logs and laboratory studies of core samples using X-ray diffraction (XRD), thin-section analysis and scanning electron microscope-energy-dispersive X-ray spectroscopy (SEM-EDS). The results show that in the Cambay Shale, mineral components are dominated by clay minerals, quartz and siderite with minor amounts of feldspar, mica and pyrite. Both thorium (Th)–potassium (K) cross-plots derived from SGR logs and XRD analysis have revealed that kaolinite and chlorite are the dominant clay minerals. The dominant clay mineralogy and the analysis of thorium to uranium ratio plots indicate the deposition of the shale in marginal marine to marine environment. Pyrite framboid size distribution, used as a redox proxy, indicates deposition under anoxic conditions. The geomechanical property of Cambay Shale has been analysed based on the overall mineral composition of the core samples. Mineralogy-based brittleness index (BI) has been evaluated and found to vary between 0.21 and 0.66, suggesting low to moderately high brittleness. Kaolinite and chlorite, the dominant clay minerals, are the less swelling clays and exhibit a lower plasticity. It may be concluded that these factors might facilitate the intrinsic fracking properties of Cambay Shale.

A Morphometric Analysis of Early Eocene Euprimate Calcanei from Gujarat, India

Postcrania dating back to the early Eocene from the Cambay Shale Formation of Gujarat, India, provide a unique window for understanding early primate behavior. Previous metric analyses of postcrania assigned to Asiadapinae indicate that these primates were generalized arboreal quadrupeds. Examination of long bone cross‐sectional properties, however, complicates the initial behavioral interpretations because it shows that these fossils overlap with primates of differing locomotor behaviors. The purpose of this study is to re‐examine calcaneal morphology of the Indian material in order to refine the locomotor reconstructions of these fossils.Surface models of fossil calcanei (n=6) were generated from micro‐computed tomography scans while those (n=73) representing 23 extant primate species were downloaded from MorphoSource. A weighted spherical harmonics analysis was carried out on the total sample. This morphological analysis represents genus‐zero surfaces using a common set of spherical harmonic functions. The harmonic coefficients associated with each calcaneus serve as shape descriptors that can be summarized via principal components (PC) analysis. Bivariate plots and models representing plus and minus two standard deviations of each PC were created to visualize morphological differences.The first three PCs explain 52.4%, 9.7%, and 9.3% of the morphological variation in the sample respectively (71.4% combined). The first PC differentiates primates with elongated calcanei that are more likely to engage in vertical clinging and leaping, from more quadrupedal primates. The second PC distinguishes calcanei of slow climbers from primates that engage in other forms of locomotion (e.g., leaping and quadrupedalism). Extant primate morphology seems to follow a continuum in which relative anteroposterior calcaneal elongation negatively correlates with slow climber calcaneal morphology. As expected, the calcaneal morphology of Marcgodinotius indicus aligns with that of extant lemuriforms, and most closely resembles that of a generalized arboreal quadruped with some leaping ability. There are two fossils tentatively attributed to Asiadapis cambayensis included in the analysis. One groups with other generalized arboreal quadrupeds, while the other falls outside the range of calcaneal variation observed in extant primates. The outlier does not follow the general pattern of calcaneal morphology observed in extant primates; instead it is characterized by some aspects of slow climber morphology, but with a relative anteroposterior calcaneal elongation. These results may reflect the generalized morphology of this fossil, and consequently the behavior of this primitive euprimate.Support or Funding InformationSupported by NSF DGE‐1746891, National Geographic Society, Leakey Foundation

Minute and diverse in fossil sticky stuff: Tanytarsini (Diptera: Chironomidae) from early Eocene Indian Cambay amber

Abstract We here present a pioneering systematic review of fossil dipterans of the tribe Tanytarsini (family Chironomidae) discovered in Indian amber from Cambay. The specimens examined belong to five species: Gujaratomyia miripes,Stempellina stebneri sp. nov., Stempellinella pollex sp. nov., Tanytarsus forfex sp. nov. andTanytarsus ramus sp. nov., which are described. All species belong to the oldest known Tanytarsini and come from the Cambay shale formation in Tadkeshwar, dated to the early Eocene (~54 Mya). Displaying unusual characters/structures of diagnostic and phylogenetic importance, the specimens studied are discussed against the background of the evolution and systematics of the oldest fossil (Eocene) and extant representatives in the tribe. An updated checklist and key to the identification of genera and species of Tanytarsini from Eocene amber is also provided. The spectral characteristics and physical properties of Cambay amber are similar to those of glessite resins, which are discussed in detail in order to substantiate the identity of the amber and the origin of the inclusions studied.

Anatomy, Relationships, and Paleobiology of Cambaytherium (Mammalia, Perissodactylamorpha, Anthracobunia) from the lower Eocene of western India

ABSTRACT The anatomy of Cambaytherium, a primitive, perissodactyl-like mammal from the lower Eocene Cambay Shale Formation of Gujarat, India, is described in detail on the basis of more than 350 specimens that represent almost the entire dentition and the skeleton. Cambaytherium combines plesiomorphic traits typical of archaic ungulates such as phenacodontids with derived traits characteristic of early perissodactyls. Cambaytherium was a subcursorial animal better adapted for running than phenacodontids but less specialized than early perissodactyls. The cheek teeth are bunodont with large upper molar conules, not lophodont as in early perissodactyls; like perissodactyls, however, the lower molars have twinned metaconids and m3 has an extended hypoconulid lobe. A steep wear gradient with heavy wear in the middle of the tooth row suggests an abrasive herbivorous diet. Three species of Cambaytherium are recognized: C. thewissi (∼23 kg), C. gracilis (∼10 kg), and C. marinus (∼99 kg). Body masses were estimated from tooth size and long bone dimensions. Biostratigraphic and isotopic evidence indicates an age of ca. 54.5 Ma for the Cambay Shale vertebrate fauna, the oldest Cenozoic continental vertebrate assemblage from India, near or prior to the initial collision with Asia. Cambaytheriidae (also including Nakusia and Perissobune) and Anthracobunidae are sister taxa, constituting the clade Anthracobunia, which is sister to Perissodactyla. We unite them in a new higher taxon, Perissodactylamorpha. The antiquity and occurrence of Cambaytherium—the most primitive known perissodactylamorph—in India near or before its collision with Asia suggest that Perissodactyla evolved during the Paleocene on the Indian Plate or in peripheral areas of southern or southwestern Asia.

An enigmatic new ungulate‐like mammal from the early Eocene of India

AbstractWe report a new genus and species of herbivorous mammal, Pahelia mysteriosa, from the early Eocene Cambay Shale Formation, Tadkeshwar Lignite Mine, Gujarat, India. The new taxon, approximately the size of a small phenacodontid (e.g. Ectocion parvus), is represented by three mandibular fragments, the most complete of which documents nearly the entire symphysis and mandibular body plus P3–M3. Pahelia has incipiently selenolophodont molars with strong exodaenodonty, absent paraconids, weak but distinct entolophids, and prominent ectostylids. Molar size increases distally, but M3 does not develop a prominent third lobe. Premolars are simple, with prominent protoconids and short talonids but little development of other trigonid cusps. The mandibular symphysis is strongly fused, and there is an enlarged alveolus for an anterior tooth. The combination of features present in the new taxon does not closely match that of any known mammal, but there are some similarities to a diversity of ungulates from Africa, Asia, Europe and North America. Preserved morphology is insufficient to assess the affinities of the new taxon with confidence, but a link to Quettacyonidae, also endemic to the Indian subcontinent, is morphologically and biogeographically plausible. If this scenario is correct, it suggests that P. mysteriosa could be a part of the endemic mammalian fauna of India prior to its initial faunal contact with Asia.

New fossils from Tadkeshwar Mine (Gujarat, India) increase primate diversity from the early Eocene Cambay Shale

Several new fossil specimens from the Cambay Shale Formation at Tadkeshwar Lignite Mine in Gujarat document the presence of two previously unknown early Eocene primate species from India. A new species of Asiadapis is named based on a jaw fragment preserving premolars similar in morphology to those of A. cambayensis but substantially larger. Also described is an exceptionally preserved edentulous dentary (designated cf. Asiadapis, unnamed sp. nov.) that is slightly larger and much more robust than previously known Cambay Shale primates. Its anatomy most closely resembles that of Eocene adapoids, and the dental formula is the same as in A. cambayensis. A femur and calcaneus are tentatively allocated to the same taxon. Although the dentition is unknown, exquisite preservation of the dentary of cf. Asiadapis sp. nov. enables an assessment of masticatory musculature, function, and gape adaptations, as well as comparison with an equally well-preserved dentary of the asiadapid Marcgodinotius indicus, also from Tadkeshwar. The new M. indicus specimen shows significant gape adaptations but was probably capable of only weak bite force, whereas cf. Asiadapis sp. nov. probably used relatively smaller gapes but could generate relatively greater bite forces.

A gymnodont fish jaw with remarkable molariform teeth from the early Eocene of Gujarat, India (Teleostei, Tetraodontiformes)

ABSTRACTThe lower jaw of a gymnodont fish collected from the lower Eocene Cambay Shale Formation in Gujarat Province, western India, has fused dentaries without a beak and a remarkable series of teeth that are unique among all known fossil and living Tetraodontiformes. The teeth are molariform, with raised spokes radiating inward from the emarginated peripheral edge of the crown. Tooth development is intraosseous, with new teeth developing in spongy bone before they erupt and attach to the dentary by pedicels. Although many of the 110 tooth loci in the fossil have lost their teeth, in life the teeth would have grown to fit tightly together to form a broad and continuous crushing surface. The estimated age of the Cambay Shale vertebrate fauna is ca. 54.5 Ma, making the jaw the second oldest confirmed gymnodont fossil. Preliminary comparisons with extant taxa of gymnodonts with fused dentaries (e.g., Diodon, Chilomycterus, and Mola) show detailed similarities in jaw structure, but further study of the dentition is needed to better understand the evolutionary position of the new fossil. We describe the new gymnodont as †Avitoplectus molaris, gen. et sp. nov., in †Avitoplectidae, fam. nov., and place the family as incertae sedis within Gymnodontes.http://zoobank.org/urn:lsid:zoobank.org:pub:46BF7C65-2241-4B89-B088-6DC6721CD2FDCitation for this article: Bemis, K. E., J. C. Tyler, W. E. Bemis, K. Kumar, R. S. Rana, and T. Smith. 2017. A gymnodont fish jaw with remarkable molariform teeth from the early Eocene of Gujarat, India (Teleostei, Tetraodontiformes). Journal of Vertebrate Paleontology. DOI: 10.1080/02724634.2017.1369422.

First mammal of Gondwanan lineage in the early Eocene of India

Based on well-preserved lower dentition, a new adapisoriculid from the Cambay Shale Formation (basal Eocene, ∼54.5Ma) in the open cast lignite mine of Vastan, Gujarat State, western India, is described. Indolestes kalamensis gen. et sp. nov adds significantly to the diversity of basal eutherians from Vastan as it represents a family hitherto not known from the Eocene of the Indian Subcontinent. Phylogenetic analysis suggests that Indolestes is derived relative to Deccanolestes and Afrodon, but primitive relative to the European adapisoriculids Bustylus and Adapisoriculus. The new data from the early Eocene provide evidence for continued survival of a Gondwanan mammal lineage following the Deccan volcanic activity (Cretaceous–Paleogene transition) in the Indian Subcontinent.

Brittleness modeling of Cambay shale formation for shale gas exploration: a study from Ankleshwar area, Cambay Basin, India

Unconventional gas shales are described as organic-rich, fine-grained reservoirs and are typically dominated by clays. The shale gas reservoirs have received great attention in the past decade, because of their large reserves as well as recent technical advances in developing these resources. Accordingly, there are increasing demands to understand the petrophysical and mechanical properties of these gas shale rocks. The mineral composition and the presence of organic matter can influence not only the distribution of pores and fluid saturation, but also the effectiveness of stimulation. The geomechanical study of a shale gas reservoir is useful in identifying the intervals which can be fractured effectively. The estimation of geomechanical properties from well logs and their calibration with laboratory-derived properties on cores has been attempted in the present paper for Cambay shale of Cambay Basin, India, which is very much prospective for shale gas exploration. Powder X-ray diffraction (XRD) analysis was carried out on drill cutting samples in the study area, and it was seen that the major mineralogy is quartz, kaolinite, pyrite, calcite and mixed clays. Petrographic observation and Fourier transform infrared spectroscopy (FTIR) results also conform to the same minerals which are identified from XRD. Geomechanical properties (Young’s modulus, Poisson’s ratio, brittleness) of Cambay shale derived from sonic logs and density logs and are validated with the available predicted brittleness index (BI) from mineralogy through petrographic observation, XRD and FTIR interpretation results. Modeling using petrel software with log data and P-impedance was carried out and a relation between log results and P-impedance volume was established. The study concluded that (BI) varies from 0.44 (less brittle) to 0.75 (highly brittle) using both mineralogy and sonic logs. This study successfully identified the areas of high BI in the study area which can be an input for effective stimulation for shale gas exploration and exploitation.

New euprimate postcrania from the early Eocene of Gujarat, India, and the strepsirrhine–haplorhine divergence

The oldest primates of modern aspect (euprimates) appear abruptly on the Holarctic continents during a brief episode of global warming known as the Paleocene-Eocene Thermal Maximum, at the beginning of the Eocene (∼56 Ma). When they first appear in the fossil record, they are already divided into two distinct clades, Adapoidea (basal members of Strepsirrhini, which includes extant lemurs, lorises, and bushbabies) and Omomyidae (basal Haplorhini, which comprises living tarsiers, monkeys, and apes). Both groups have recently been discovered in the early Eocene Cambay Shale Formation of Vastan lignite mine, Gujarat, India, where they are known mainly from teeth and jaws. The Vastan fossils are dated at ∼54.5 Myr based on associated dinoflagellates and isotope stratigraphy. Here, we describe new, exquisitely preserved limb bones of these Indian primates that reveal more primitive postcranial characteristics than have been previously documented for either clade, and differences between them are so minor that in many cases we cannot be certain to which group they belong. Nevertheless, the small distinctions observed in some elements foreshadow postcranial traits that distinguish the groups by the middle Eocene, suggesting that the Vastan primates—though slightly younger than the oldest known euprimates—may represent the most primitive known remnants of the divergence between the two great primate clades.

New early Eocene vertebrate assemblage from western India reveals a mixed fauna of European and Gondwana affinities

The Ypresian Cambay Shale Formation at Vastan and Mangrol lignite mines in Gujarat, western India, has yielded a rich vertebrate fauna with numerous taxa of European affinities. Here we report a new, approximately contemporary vertebrate assemblage from two fossiliferous layers in the nearby mine of Tadkeshwar. These layers have yielded a similar mammal fauna with the co-occurrence of the perissodactyl-like cambaytheriid Cambaytherium thewissi, the adapoid primates Marcgodinotius indicus and cf. Asiadapis cambayensis, and the hyaenodontid Indohyaenodon raoi. The presence of these species in both Vastan and Tadkeshwar mines and at different levels suggests that the deposits between the two major lignite seams represent a single land mammal age. Apart from the aforementioned species there is a new, smaller species of Cambaytherium, and a new genus and species of esthonychid tillodont. This fauna also contains the first large early Eocene vertebrates from India, including an unidentified Coryphodon-like pantodont, a dyrosaurid crocodyliform and a new giant madtsoiid snake. Among the Tadkeshwar vertebrates several taxa are of Gondwana affinities, such as Pelomedusoides turtles, dyrosaurids, and large madtsoiids, attesting that the early Eocene was a crucial period in India during which Laurasian taxa of European affinities co-existed with relict taxa from Gondwana before the India-Asia collision. Our results suggest that terrestrial faunas could have dispersed to or from Europe during episodes of contact between the Indian subcontinent and different island blocks along the northern margin of the Neotethys, such as the Kohistan–Ladakh island-arc system. Gondwana taxa might represent remnants of ghost lineages shared with Madagascar, which reached the Indian subcontinent during the late Cretaceous; alternatively they might have come from North Africa and passed along the southern margin of the Neotethys to reach the Indian subcontinent. These dispersals would have been possible as a result of favourable paleogeographic conditions such as the particular Neotethys conformation during the beginning of the early Eocene.