Great events which moulded life jurassic period

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Age of Gymnosperms & Dinosaurs full of activities of a variety of species and many transitional forms as the process of evolution of mammals and birds was gaining momentum

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Great Events Which Moulded Life 50
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Great events which moulded life jurassic period

More from SantoshBhatnagar1

EXO ELECTROGENIC SPECIES ARE FOUND IN MANY GENERA OF EUKARYOTIC AS WELL AS PROKARYOTIC ORGANISMS ;BUT BACTERIA ,PARTICULARLY CYANOBACTERIA AND PHOTOSYNTHETIC EUKAROTES LIKE ALGAE AREIN THE FOREFRONT - BOTH MICRO AMD MACRO ALGAE ARE BEING UTILISED WITH OR WITHOUT BACTERIA IN MFCs FOR TREARING POLLUTED WATER AND SIMULTANEOUS PRODUCTION OF ELECTRICITY -THE ADVANTAGE WITH ALGAE IS THEY SUCK IN CO2 AND GIVE OUT O2 AND ARE THUS BETTER FOR ENVIRONMENT NITZCHIA IS A LARGE GENUS OF DIATOMS WHICH INCLUDES BOTH FRESH WATER AND MARINE SPECIES -MANY TOXIC ALSO;BUT THEY ALSO SERVES AS GOOD BIOSENSORS MAINLY DUE TO THEIR BIOLUMINESCENT POROUS SILICON FRISTULE DIATOMS LIKE NITZSCIA ARE ALSO PREFERRED DUE TO THEIR OIL PRODUCTION AND OTHER USES OF THEIR FRISTULE

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EXOELECTROGENS ARE ORGANISMS WHICH CAN RECEIVE ELECTRONS FROM DONARS AND CAN EXPORT ELECTRONS OUTSIDE THE CELL OR CELLS THE ELECTRONS PRODUCED DURING PHOTOSYNTHESIS OR RESPIRATION AVAILABLE TO THEM CAN BE PASSED ON TO ELCTRON ACCEPTORS VIA ELECTRODES AND DURING THE PROCESS ELECTRICITY GETS GENERATED IN THE CIRCUIT . THE CHALLENGE IS TO EXTRACT ELECTRONS AND USE THEM FOR POWER GENERATION AS WELL AS SIMULTANEOUSLY CLEAN POLLUTED WATER AND PRODUCE HYDROGEN ETC AND OTHER BY PRODUCTS .

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EXOELECTROGENS -CYANOBACTERIA.docx

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SHEWANELLA - VERSATILE EXOELECTROGENIC FACULTATIVE ANAEROBE CAPABLE OF GENERATING ELECTRICITY BY REDUCING MANY METALS WHILE RESPIRING AND TRANSFERING ELECTRONS EXTRACELLULARLY HENCE THEIR BIOFILMS AREUSED IN MFCs,MECs. ;KNOWN FOR THRIVING ON A VARIETY OF SUBSTRATES AND REDUCING MANY NOBLE METALS LIKE GOLD SILVER PLATINUM ETC ; ALSO CAPABLE OF PRODUCING HYDROGEN AND H2S; ALSO FAMOUS FOR BIOSYNTHESIS OF NANOPARICLES ;PRAISED FOR EFFICIENCY OF ITS NANOWIRES AND BIOFILMS ; CAN GENERATE ELECTRICITY FROM WASTE ALSO;HENCE SELECTED FOR DEEPSPACE RESEARCH -COULD SOLVE ASTRAUNOTS URINE DISPOSAL PROBLEM AS IT CAN MAKE IT REUSABLE WHILE PROVIDING POWER TO SATELLITE;IT IS ALSO INFAMOUS FOR SPOILING FOOD-FISH MEAT ETC AND CAUSING DISEASES IN HUMANS .

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GEOBACTER IS ONE OF THE MOST FAMOUS EXOELECTROGENIC BACTERIA WHICH WAS THE FIRST BACTERIUM DISCOVERED WITH CAPABLITY OF OXIDISING ORGANIC COMPONDS AND METALS( INCLUDING RADIOACTIVE METALS AND PETROLEUM COMPOUNDS )INTO CO2 USING IRONOXIDE ETC AS ELECTRON ACCEPTOR AND PRODUCING ELECTRIC CURRENT. ITHAS BEEN USED IN VARY MANY EXPERIMENTS TO TEST THE WONDERFUL QUALITIES, ABILITIES AND CAPABILITIES OF VERSATILE EXOELECTROGENS AND THEIR USE FOR BIOREMEDIATION AND BIOFUEL PRODUCTION., THEY ARE ALSO CAPABLE OF RESPIRING ON GRAPHITE ELECTRODES

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EXOELECTROGENS ARE VERSATILE HEROES CAPABLE OF SIMULTANEOUSLY DELIVERING MULTIPLE BENEFITS TO US INVARIOUS FIELDS RANGING FROM BIOREMEDIATION TO ENERGY,ENVIRONMENT, SENSORS, CLEAN BIO FUELS DESALINATION,Etc AND ARE POISED TO SOLVE OUR WASTE DISPOSAL PROBLEM EVEN IN SPACE. ONE FEALS LIKE SALUTING THEM FOR THEIR MULTIPLE TALENTS. THEY INCLUDE MAINLY BACTERIA BUT ALSO MICRO ALGAE, FUNGI,AND EVEN SOME ANGIOSPERMS .

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VIRUSES ARE NOT CONSIDERED LIVING BEINGS BUT EVEN IF THEY WERE THEY WOULD NOT FIT IN ANY KINGDOM ;THEY ARE ACTUALLY ENEMIES OF ALL KINGDOMS OF LIVING BEINGS; HENCE I WAS INITIALLY RELUCTENT TO INCLUDE THEM IN ABOOK ABOUT LIVING BEINGS BUT THEN I THOUGHT WITHOUT THEM THE STORY OF LIVING BEINGS IS NOT COMPLETE ;FURTHER THEY ARE NOT TREATED AS LIVING BY OUR DEFINITION OF LIFE AND LIVING BEINGS OTHERWISE THEY HAVE MANY CHARCTERISTICS OF BEINGS AND ARE WORTHY OF DUE CONSIDERATION AND FIT INTO OUR DEFINITION OF CHAMPIONS AMONGST VIRUSES PITHO VIRUSESARE LARGEST AND MOST ANCIENT AND WITH MANY INTERESTING FEATURES .

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YEAST IS ONE OF THE SMALLEST FUNGI KNOWN ;BUT IT IS UNLIKE TYPICAL FUNGI .ITS MAIN FEATURE IS ITS UNICELLULAR CHARACTER AND ITS ABILITY TO CAUSE FERMENTATION BY ANAEROBIC RESPIRATION ;AND THEREFORE ITS USE IN BEER &BREAD MAKING ; ITS USE FOR GENERATING ELECTRICITY IS ALSO EMERGING AS ANOTHER USEFUL FEATURE .FOR SCIENTISTS IT IS A MODEL ORGANISM FOR SCIENTIFIC RESEARCH TO LEARN ABOUT INTRA CCELLULAR PROCESSES OF EUKARYOTES AND GENETICS

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CHAMPIONS ARE THOSE WHICH EXCEL IN SOME FIELD AND OUTBIDDING NEAREST RIVALS SHOWING THEY ARE THE BEST AND REACH THE TOP ;EXCELLENCE IS NOT THE PRESERVE OF THE TALLEST BIGGEST LARGESTOR HIGHEST -IT CAN BE EXHIBITED EVEN THE SMALLEST SHORTEST OR LIGHTEST;HERE INTERESTING EXAMPLES HAVE BEEN GIVEN FROM ALL TYPES DESCRIBING THEIR SPECIAL FEATURES AND CONSIDERING THEM CHAMPIONS ON THE BASIS OF SCIENTIFICALLY ESTABLISHED FACTS

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Context. WASP-76 b has been a recurrent subject of study since the detection of a signature in high-resolution transit spectroscopy data indicating an asymmetry between the two limbs of the planet. The existence of this asymmetric signature has been confirmed by multiple studies, but its physical origin is still under debate. In addition, it contrasts with the absence of asymmetry reported in the infrared (IR) phase curve. Aims. We provide a more comprehensive dataset of WASP-76 b with the goal of drawing a complete view of the physical processes at work in this atmosphere. In particular, we attempt to reconcile visible high-resolution transit spectroscopy data and IR broadband phase curves. Methods. We gathered 3 phase curves, 20 occultations, and 6 transits for WASP-76 b in the visible with the CHEOPS space telescope. We also report the analysis of three unpublished sectors observed by the TESS space telescope (also in the visible), which represents 34 phase curves. Results. WASP-76 b displays an occultation of 260±11 and 152±10 ppm in TESS and CHEOPS bandpasses respectively. Depending on the composition assumed for the atmosphere and the data reduction used for the IR data, we derived geometric albedo estimates that range from 0.05 ± 0.023 to 0.146 ± 0.013 and from <0.13 to 0.189 ± 0.017 in the CHEOPS and TESS bandpasses, respectively. As expected from the IR phase curves, a low-order model of the phase curves does not yield any detectable asymmetry in the visible either. However, an empirical model allowing for sharper phase curve variations offers a hint of a flux excess before the occultation, with an amplitude of ∼40 ppm, an orbital offset of ∼−30◦ , and a width of ∼20◦ . We also constrained the orbital eccentricity of WASP-76 b to a value lower than 0.0067, with a 99.7% confidence level. This result contradicts earlier proposed scenarios aimed at explaining the asymmetry observed in high-resolution transit spectroscopy. Conclusions. In light of these findings, we hypothesise that WASP-76 b could have night-side clouds that extend predominantly towards its eastern limb. At this limb, the clouds would be associated with spherical droplets or spherically shaped aerosols of an unknown species, which would be responsible for a glory effect in the visible phase curves.

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www.seribangash.com The Mariana Trench is one of the most remarkable geological features on Earth. Here are some details about it: Location: The Mariana Trench is located in the western Pacific Ocean, east of the Mariana Islands. It stretches for about 2,550 kilometers (1,580 miles) and is known as the deepest part of the world's oceans. Depth: The trench reaches incredible depths, with its deepest point known as the Challenger Deep, which plunges down to approximately 10,984 meters (36,037 feet) below sea level. To put this into perspective, if Mount Everest, the tallest mountain on Earth, were placed at the bottom of the Challenger Deep, its peak would still be over 2 kilometers (1.25 miles) underwater. Formation: The Mariana Trench was formed by the subduction of the Pacific Plate beneath the Mariana Plate. This process creates a deep trench as the heavier Pacific Plate is forced beneath the lighter Mariana Plate. Geological Features: The trench is characterized by steep, V-shaped valleys, and its walls are composed of highly compressed sedimentary rock. At the bottom of the trench, there are also large amounts of marine sediment. Pressure: The pressure at the bottom of the Mariana Trench is immense, reaching over 1,000 times the pressure at the surface. This extreme pressure creates a challenging environment for exploration and makes it difficult for organisms to survive. Exploration: Despite its extreme conditions, the Mariana Trench has been the subject of numerous scientific expeditions and explorations. One of the most famous explorations was the dive to the Challenger Deep by Swiss scientist Jacques Piccard and U.S. Navy Lieutenant Don Walsh in 1960. More recently, in 2012, filmmaker James Cameron made a solo dive to the bottom of the Challenger Deep in the Deepsea Challenger submersible. Biological Discoveries: Despite the harsh conditions, the Mariana Trench is home to a surprising variety of life forms, including unique species of deep-sea fish, crustaceans, and microbial life. Some organisms have adapted to survive in the extreme pressure and darkness of the trench. Environmental Importance: Studying the Mariana Trench provides valuable insights into the geology, biology, and oceanography of the deep sea. It also helps scientists better understand the processes that shape the Earth's crust and the distribution of life in the oceans. Conservation: Due to its remote location and extreme depths, the Mariana Trench has remained relatively untouched by human activity. However, there is growing concern about the potential impacts of deep-sea mining and pollution on this fragile ecosystem, highlighting the need for conservation efforts to protect this unique environment. https://seribangash.com/barber-shop-business-complete-guide-for-beginners/ https://seribangash.com/legend-virat-kohli-in-cricket-history/

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Theoretical predictions and observational data indicate a class of sub-Neptune exoplanets may have water-rich interiors covered by hydrogen-dominated atmospheres. Provided suitable climate conditions, such planets could host surface liquid oceans. Motivated by recent JWST observations of K2-18 b, we self-consistently model the photochemistry and potential detectability of biogenic sulfur gases in the atmospheres of temperate sub-Neptune waterworlds for the first time. On Earth today, organic sulfur compounds produced by marine biota are rapidly destroyed by photochemical processes before they can accumulate to significant levels. Domagal-Goldman et al. suggest that detectable biogenic sulfur signatures could emerge in Archean-like atmospheres with higher biological production or low UV flux. In this study, we explore biogenic sulfur across a wide range of biological fluxes and stellar UV environments. Critically, the main photochemical sinks are absent on the nightside of tidally locked planets. To address this, we further perform experiments with a 3D general circulation model and a 2D photochemical model (VULCAN 2D) to simulate the global distribution of biogenic gases to investigate their terminator concentrations as seen via transmission spectroscopy. Our models indicate that biogenic sulfur gases can rise to potentially detectable levels on hydrogen-rich water worlds, but only for enhanced global biosulfur flux (20 times modern Earth’s flux). We find that it is challenging to identify DMS at 3.4 μm where it strongly overlaps with CH4, whereas it is more plausible to detect DMS and companion byproducts, ethylene (C2H4) and ethane (C2H6), in the mid-infrared between 9 and 13 μm. Unified Astronomy Thesaurus concepts: Exoplanet atmospheres (487); Exoplanet

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