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Home > Microfacies, Diagenesis and Depositional Environments of Samana Suk Formation Middle Jurassic Carbonates Exposed in South East Hazara and Samana Range

Microfacies, Diagenesis and Depositional Environments of Samana Suk Formation Middle Jurassic Carbonates Exposed in South East Hazara and Samana Range

Thesis Info

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Author

Cheema, Amjed Hussain

Program

PhD

Institute

University of the Punjab

City

Lahore

Province

Punjab

Country

Pakistan

Thesis Completing Year

2010

Thesis Completion Status

Completed

Subject

Applied Sciences

Language

English

Link

http://prr.hec.gov.pk/jspui/handle/123456789/1265

Added

2021-02-17 19:49:13

Modified

2024-03-24 20:25:49

ARI ID

1676726642202

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This document presents the results of detailed work on the microfacies analysis, depositional environments and diagenetic history of the Middle Jurassic carbonates system, (The Samana Suk Formation) investigated in the three measured outcrop sections (total thickness 785m) in the Hazara and Kohat area. The three sections (Sanghar Gali, Bagh and Samana Range) lie along the northern rim of the Upper Indus Basin of Pakistan. Rocks exposed in the three above mentioned localities were investigated in the field for facies and sedimentary structures. 800 samples were collected and each sample was further investigated on polished slab, and 850 thin-sections were prepared for detailed petrographic analysis. All the data generated was interpreted for depositional environments and diagenetic imprints. This work is also supported by selected SEM photographs, forty two oxygen and carbon isotope analyses and fourteen trace element analyses. The data from the three studied sections is presented semi-quantitatively in Sedimentary Synthesis Logs and Diagenetic Feature Logs. The results are also supported by biostratigraphic analysis of selected shales and limestone samples. All the results of these studies were integrated to propose a likely depositional or sequence stratigraphic model of the Samana Suk Formation. Benthic foraminiferal data suggest that carbonate sedimentation started in Bajocian (Middle Jurassic) and might have continued until Callovian time. The data has also confirmed the Bathonian age from the middle part of the formation in the Samana Range Section. On the whole, the faunal/floral assemblage suggest sedimentation of the Samana Suk Formation occurred on the shallow to very shallow marine setting typical of gently dipping shelf/ramp., The assemblages suggest various episodes of sea level rise and fall. Thirty microfacies have been identified that were deposited in variety of environments. Generally the formation is dominated by oolitic grainstone, that have deposited in shallow marine subtidal to intertidal environments as an oolitic shoal complex on a gently inclined carbonate ramp/platform which might have attained slightly rimed shape in a later stage. Within the whole succession about 19, 20 and 31 shallowing upward cycles have been interpreted in the Sanghar Gali, Bagh and Samana Range Sections respectively. These cycles vary in numbers and thickness in the three studied sections and do not correlate individually across the study area. Such cycles normally start from mudstone (M2) and/or wackestone (W1 or W2) and terminate at oolitic grainstone while occasionally complete cycles go up to pelletal pack-grainstone (PG1) and/or unfossiliferous mudstone (M1), representing the tidal flat facies. These cycles are parasequences which started from subtidal environments and terminate in intertidal environments and rarely end in supratidal environment. Twenty six different diagenetic features have been identified in the Samana Suk Formation. Overall, diagenetic sequence ranges from marine phreatic to deep burial. However dominant influences of meteoric phreatic and mixed meteoric marine environments during shallow burial have also been observed. Dolomite, though minor component relative to limestone, is present in several forms in the Samana Suk Formation such as layers and thin beds, dolomitized burrows, grain selective and cement/matrix selective dolomite, molds and fracture filling dolomite, dolomite developed along sutured seams and stylolites, and pervasive dolomite. Dolomite in the Sanghar Gali and Bagh Sections is common, while in the Samana Range Section it is rare. Dolomitized burrows and pervasive dolomite in the upper 35m of the Bagh Section are volumetrically important. Dolomite layers, beds and pervasive dolomite were developed in meteoric marine mixing zone. Bio-pumping together with bacterial activities in the burrow network, related to the burrowing organisms, was probably responsible for the preferential dolomitization of burrow fillings. The grainstone horizons originally had good primary intergranular/ interparticle porosity, which was first reduced by early mechanical compaction and later on occluded during diagenesis by seven different types of calcite cements. Three phases of dissolution and four phases of fracturing have been identified which have generated secondary intergranular porosity (i. e., mouldic, vuggy and fracture) which has also been occluded. Two sets of fractures are filled with medium to coarse blocky calcite, 3rd set is filled with internal sediments whereas 4th set is filled with dolomite. The high resolution microfacies and cyclicity, biostratigraphic abundance data has been used to interpret the significant depositional surfaces such as flooding surfaces (transgressions) and sequence boundaries (regressions). Four flooding surfaces and four sequence boundaries have been interpreted which divides the whole Samana Suk Formation into four 3rd order sequences. These sequences have only highstand and transgressive system tracts. This interpretation is based on the most striking contrast in the microfacies. The proposed model shows proximal facies (mainly oolitic shoal and back shoal facies) towards the east-southeast while distal or open marine facies (mainly mudstone/marl) towards the west-northwest. This also implies that the lowstand system tract is probably preserved further west of the Samana Range section.
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مولانا سید مرتضیٰ حسن

مولانا سید مرتضیٰ حسن
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Optimizing Sensory Loads Using a Sensory Processing Skills Therapy among Autistic Spectrum Disorder

IntroductionSensory integration therapy can improve language skills, attention, and social interactions in children with ASD. However, it is also important to note that research in this field is ongoing, and more studies are needed to confirm the effectiveness of these therapies. The present study is aimed to identify the effects of occupational therapy-based sensory processing skill therapies in improving the autism severity and QoL among ASD children. MethodologyThe intervention was performed for 12 weeks, six sessions per week, each based on 60 minutes of duration. The treatment protocol comprised four sensory processing skills in which Each child was trained on every skill for 15 minutes, making a total of 60 minutes of duration for a single session. ResultsSignificant improvements in CARS, CGAS and PedsQL (p<0.001) were observed after 12-weeks of intervention. ConclusionSensory processing skills therapies are a practical treatment approach in optimizing sensory load among ASD children.   DOI: https: //doi. Org/10.59564/amrj/01.01/005

Production of Bacterial Pectinase Using Submerged Culture for Various Applications

Pectinases are pectin degrading enzymes and are naturally produced by plants, animals and microorganisms. Their major source of production at industrial scale is from microorganisms especially Bacillus sp, Aspergillus sp. and yeast sp. which are generally regarded as safe. Aspergillus sp. generally produce acidic pectinases which are used in the food and beverage industry for the extraction and clarification of fruit juices and maceration of vegetables for production of purees and pastes. Bacillus sp. are usually capable of producing alkaline pectinases which have diverse functions and are in use in many industrial processes, successfully substituting the use of harsh chemicals which not only causes the deterioration of product quality but also the deterioration of environment. Pectinases from Bacillus sp. are generally active at broad ranges of pH and temperature and due to this reason, they are multi-functional enzymes. Pectinases account for more than 10% of the industrial enzymes market and they constitute 25% of the global food enzymes market. The present study was concerned with the search for a novel bacterial isolate for the lab scale production of pectinase (Polygalacturonase). Keeping in view the increasing demand of pectinase, specially its need in Faisalabad, a textile city of Pakistan, isolation of new hyper producer bacterial strains locally is an easy and cheap way of getting the desirable products at low cost. Therefore, isolation of new strains for industrial enzyme production has been, and will be, a part of research. This method alone can also provide raw material for further research such as enzyme engineering or molecular directed evolution. Pectinase positive cultures were isolated using PSAM, the medium that is able to grow and differentiate pectin consuming bacteria from others. The pectinase producing bacteria form clear halos around their colonies while others do not form any clear zones. For the identification of hyper producer strains, colony PCR was done for 16S rRNA analysis. The reason to use the 16S rRNA gene for identification purposes is that there is a large database of DNA sequences available for the gene from the widest range of microbial species as compared with any other genetic target. The selected bacterial isolate NS1 (source of pectinase enzyme) was identified based on PCR amplification of 16S rRNA and for this purpose the amplified product was electrophoresed in agarose gel against a known species of Bacillus licheniformis. The 16S rRNA sequencing confirmed the Bacillus status of the strain NS1 and the nucleotide sequence BLAST results showed 98% similarity of strain NS1 having Accession No. KX765286 with few species of Bacillus licheniformis. The growth conditions of the newly isolated Bacillus licheniformis strain were investigated using submerged fermentation to understand the fermentation behaviour of the microorganism and the pattern of pectinase production by it. The growth of the organism and enzyme production by it was investigated using some local agrowastes such as wheat bran, gram bran, citrus peel, apple pomace, carrot pomace and peanut shells as carbon sources. Among these agrowastes citrus peel powder at 2.5% concentration proved as best substrate for pectinase production followed by wheat bran. Among various nitrogen sources investigated for their role in pectinase production, organic sources such as tryptone and yeast extract gave better results than inorganic nitrogen sources. Among inorganic sources Diammonium hydrogen phosphate gave more pectinase units than other inorganic nitrogen sources. Physical parameters like pH, temperature, inocula size and incubation period for high yield of pectinase in submerged fermentation were optimized by using Response Surface Methodology. Which is an efficient tool for increasing product yield many folds in short time due to limited number of experiments and lab work. In the present study, the yield of pectinase was increased 5.6 fold that optimization produced 219U/mL as compared to one variable at a time method which produced only 38.86U/mL. Several purification methods were evaluated to observe that which one is more advantageous and cost effective in the present study for pectinase purification. Three methods of protein purification (aqueous two phase purification system, macro-affinity ligand facilitated three phase partitioning and gel filtration chromatography) were used in the present study and macro-affinity ligand facilitated three phase partitioning were found to give high purification of pectinase with purification fold of 13.05. The pectinase from newly isolated Bacillus licheniformis showed some novelty in characteristics as compared to most of the pectinases produced by other species. Although its optimum activity was achieved at a temperature of 70ºC in glycine buffer pH 8 but it also showed considerable activity (26.75U/mL) even at 100ºC in phosphate buffer pH 7. Addition of 15mM CaCO3 to the enzyme assay mixture increased the pectinase activity by 3.1 fold and addition of chloroform to enzyme assay mixture increased the pectinase activity by 7.45 fold. Surfactants (CTAB, SDS and Triton X-100) increased the pectinase activity many fold as compared to control. Among various sugars investigated for their effect on pectinase activity, sorbitol was found as a stimulator of pectinase activity by increasing its activity by 1.8 fold while glucose, lactose and sucrose inhibited its activity. The pectinase produced in this study was investigated for applications such as oil extraction from sunflower seeds, apple juice extraction and clarification and starch extraction from potatoes. In all of the above applications, the locally produced pectinase enhanced the yield of apple juice, oil and starch several fold as compared to control without the application of pectinase enzymes. Apple juice yield was increased by 2.06 fold due to pectinase treatment while the juice clarification was increased by 1.62 fold. Pectinase application also increased the oil yield some 3.15 fold as compared to oil extraction by water without the addition of pectinase. Its effect on potato starch extraction was also appreciable and 3.95 fold increase in starch yield was observed due to pectinase treatment of potato slurry. All these investigations showed that the low cost pectinase produced by locally isolated microorganisms using low cost agrowastes as nutrient supplements are able to compete with costly commercial enzymes and can bring a revolution in product quality and yield if used by local industries.