Definition of Elements and atom
Origin of Universe
Theories of origin of Solar system and Earth
Chemical Composition of Planets
Chemical Composition of Earth
Chemical composition of Meteorites
Abundance of Elements
Information about these fluids is an invaluable aid in mineral exploration.
Conventional academic methods of analysing fluid inclusions are too slow and tedious to be of practical application in typical mineral exploration activities.
However, the academic data from numerous studies does show that CO2 is an exceptionally important indicator when exploring for most types of gold deposit.
Because the baro-acoustic decrepitation method is a rapid and reliable method to measure CO2 contents in fluids, it can be used to study a spatial array of data and it is an invaluable and practical exploration method.
Measurements of temperatures of fluid inclusions does not usually help in mineral exploration as hydrothermal minerals deposit over a wide temperature range and there is no specific temperature which is indicative of mineralisation. However, if temperatures are available on a large spatial array of samples, then temperature trends may be a useful exploration method to find the hottest part of the system, which is presumably the location of the best economic mineralisation. Baro-acoustic decrepitation is the most practical method to determine temperatures of the large numbers of samples required.
Salinities of fluid inclusions are of limited use in exploration and are difficult to measure. However, they can be used to recognise intrusion related hydrothermal systems.
This is my presentation on the tectonic control of sediments.
It includes the effects of tectonics either direct or indirect on sediments and sedimentation.
Sedimentation along various plate boundaries.
Few examples as evidence from Pakistan (the Siwalik Group) and Argentina (Fiambala Basin)
A presentation on Hydrothermal wall rock alteration with case studies on geophysical applications.
References : https://drive.google.com/drive/folders/16VSZMPMASMNVB47JdBUa_7udBk1qvK2U?usp=sharing
Boundary problems between :-
Precambrian/Cambrian
Permian/Triassic
Cretaceous/Tertiary
Neogene/Quaternary
Stratigraphic boundaries are determined by one or more of geological events such as volcanic activity, sedimentation, tectonism, paleo-environments & evolution of life.
Faunal records have played major role in determining the boundaries of the Phanerozoic units.
The other geological events are dated on the evidence of fossil records.
Information about these fluids is an invaluable aid in mineral exploration.
Conventional academic methods of analysing fluid inclusions are too slow and tedious to be of practical application in typical mineral exploration activities.
However, the academic data from numerous studies does show that CO2 is an exceptionally important indicator when exploring for most types of gold deposit.
Because the baro-acoustic decrepitation method is a rapid and reliable method to measure CO2 contents in fluids, it can be used to study a spatial array of data and it is an invaluable and practical exploration method.
Measurements of temperatures of fluid inclusions does not usually help in mineral exploration as hydrothermal minerals deposit over a wide temperature range and there is no specific temperature which is indicative of mineralisation. However, if temperatures are available on a large spatial array of samples, then temperature trends may be a useful exploration method to find the hottest part of the system, which is presumably the location of the best economic mineralisation. Baro-acoustic decrepitation is the most practical method to determine temperatures of the large numbers of samples required.
Salinities of fluid inclusions are of limited use in exploration and are difficult to measure. However, they can be used to recognise intrusion related hydrothermal systems.
This is my presentation on the tectonic control of sediments.
It includes the effects of tectonics either direct or indirect on sediments and sedimentation.
Sedimentation along various plate boundaries.
Few examples as evidence from Pakistan (the Siwalik Group) and Argentina (Fiambala Basin)
A presentation on Hydrothermal wall rock alteration with case studies on geophysical applications.
References : https://drive.google.com/drive/folders/16VSZMPMASMNVB47JdBUa_7udBk1qvK2U?usp=sharing
Boundary problems between :-
Precambrian/Cambrian
Permian/Triassic
Cretaceous/Tertiary
Neogene/Quaternary
Stratigraphic boundaries are determined by one or more of geological events such as volcanic activity, sedimentation, tectonism, paleo-environments & evolution of life.
Faunal records have played major role in determining the boundaries of the Phanerozoic units.
The other geological events are dated on the evidence of fossil records.
Theory of Planetary System Formation The mass of the presol.pdfadislifestyle
Theory of Planetary System Formation The mass of the pre-solar molecular cloud played the
largest role in terms of how the solar system formed. It might have begun with a 100 solar mass
cloud approximately 1 to 2 light years in diameter. It's possible that mutual gravitational attraction
between cloud particles was too weak to start the process. When gravity is too weak, the only
other force strong enough to bring a significant number of particles together is the electromagnetic
force. Barring that, perhaps a nearby shockwave from a supernova explosion caused the initial
motion of material: but once started, gravity took hold, causing the inevitable collapse. The
process it underwent followed a pattern that scientists believe is mirrored everywhere a star exists.
In this activity, you will put the solar system formation process parts in order from the beginning. 1.
Planetesimals accreted material until they became large enough to form planets. 2. Gravitational
potential energy of the collapsing gas cloud was converted into thermal energy. 3. Collapsing gas
cloud rotated faster as the collapse continued due to conservation of angular momentum. 4.
Planetesimals were massive enough to have a gravitational field sufficient to attract additional
nearby objects. 5. The random motions of material in the collapsing gas cloud were reduced to the
final motion of the material rotating in a disk. 6. The inner parts of the continuing, flattening cloud
free fell into the growing object at the center. 7. Continued motions brushed smaller particle grains
against larger grains. As this electrostatic "sticking" occurred, the particle grains became larger. 8.
Cloud of molecular gas started to collapse due to gravity or other astrophysical process. Use the
number of the process to order them from earliest to latest (left to right).Temperature and
Formation of Our Solar System Temperature was the key factor leading to the state distribution of
various objects made of different elements and compounds. The graph below shows the
temperature (expressed in kelvins) at different distances from the Sun (expressed in AU ) in the
solar system during the time when the planets were formed. To produce a linear plot, in the usual
sense, the vertical axis is inverted so that temperature goes from high to low starting near the Sun.
Use Figure 1 to fill in Table 1 with the formation temperatures for each planet, including the dwarf
planet, Ceres.Aktranomy 1511 Laboratory Manua! Bond albedo refers to the total radiation
reflected from an object compared to the total incident radiation from the Sun. The geometric
albedo refers to the amount of radiation equally reflected in all directions at all wavelengths off an
object. It is clear that a wide range of planetary formation temperatures existed in the early solar
system. The temperatures at which different compounds form or for which elements have physical
state changes will vary. Since the majority of material in the molecular cl.
The Rare Earth hypothesis argues that the emergence of complex life on Earth required an improbable combination of astrophysical and geophysical events and circumstances.
Presented by Dr. Dennis Wilson
In this presentation, I focused on the geomorphological aspect of earthquake which means tectonic plates. Additionally, we also included the origin of the Universe and tectonic plates. And also the Nepal and Taiwan earthquakes of 2015 was also described here in perspective with tectonic plates.
THE IMPORTANCE OF MARTIAN ATMOSPHERE SAMPLE RETURN.Sérgio Sacani
The return of a sample of near-surface atmosphere from Mars would facilitate answers to several first-order science questions surrounding the formation and evolution of the planet. One of the important aspects of terrestrial planet formation in general is the role that primary atmospheres played in influencing the chemistry and structure of the planets and their antecedents. Studies of the martian atmosphere can be used to investigate the role of a primary atmosphere in its history. Atmosphere samples would also inform our understanding of the near-surface chemistry of the planet, and ultimately the prospects for life. High-precision isotopic analyses of constituent gases are needed to address these questions, requiring that the analyses are made on returned samples rather than in situ.
Introduction:
RNA interference (RNAi) or Post-Transcriptional Gene Silencing (PTGS) is an important biological process for modulating eukaryotic gene expression.
It is highly conserved process of posttranscriptional gene silencing by which double stranded RNA (dsRNA) causes sequence-specific degradation of mRNA sequences.
dsRNA-induced gene silencing (RNAi) is reported in a wide range of eukaryotes ranging from worms, insects, mammals and plants.
This process mediates resistance to both endogenous parasitic and exogenous pathogenic nucleic acids, and regulates the expression of protein-coding genes.
What are small ncRNAs?
micro RNA (miRNA)
short interfering RNA (siRNA)
Properties of small non-coding RNA:
Involved in silencing mRNA transcripts.
Called “small” because they are usually only about 21-24 nucleotides long.
Synthesized by first cutting up longer precursor sequences (like the 61nt one that Lee discovered).
Silence an mRNA by base pairing with some sequence on the mRNA.
Discovery of siRNA?
The first small RNA:
In 1993 Rosalind Lee (Victor Ambros lab) was studying a non- coding gene in C. elegans, lin-4, that was involved in silencing of another gene, lin-14, at the appropriate time in the
development of the worm C. elegans.
Two small transcripts of lin-4 (22nt and 61nt) were found to be complementary to a sequence in the 3' UTR of lin-14.
Because lin-4 encoded no protein, she deduced that it must be these transcripts that are causing the silencing by RNA-RNA interactions.
Types of RNAi ( non coding RNA)
MiRNA
Length (23-25 nt)
Trans acting
Binds with target MRNA in mismatch
Translation inhibition
Si RNA
Length 21 nt.
Cis acting
Bind with target Mrna in perfect complementary sequence
Piwi-RNA
Length ; 25 to 36 nt.
Expressed in Germ Cells
Regulates trnasposomes activity
MECHANISM OF RNAI:
First the double-stranded RNA teams up with a protein complex named Dicer, which cuts the long RNA into short pieces.
Then another protein complex called RISC (RNA-induced silencing complex) discards one of the two RNA strands.
The RISC-docked, single-stranded RNA then pairs with the homologous mRNA and destroys it.
THE RISC COMPLEX:
RISC is large(>500kD) RNA multi- protein Binding complex which triggers MRNA degradation in response to MRNA
Unwinding of double stranded Si RNA by ATP independent Helicase
Active component of RISC is Ago proteins( ENDONUCLEASE) which cleave target MRNA.
DICER: endonuclease (RNase Family III)
Argonaute: Central Component of the RNA-Induced Silencing Complex (RISC)
One strand of the dsRNA produced by Dicer is retained in the RISC complex in association with Argonaute
ARGONAUTE PROTEIN :
1.PAZ(PIWI/Argonaute/ Zwille)- Recognition of target MRNA
2.PIWI (p-element induced wimpy Testis)- breaks Phosphodiester bond of mRNA.)RNAse H activity.
MiRNA:
The Double-stranded RNAs are naturally produced in eukaryotic cells during development, and they have a key role in regulating gene expression .
Multi-source connectivity as the driver of solar wind variability in the heli...Sérgio Sacani
The ambient solar wind that flls the heliosphere originates from multiple
sources in the solar corona and is highly structured. It is often described
as high-speed, relatively homogeneous, plasma streams from coronal
holes and slow-speed, highly variable, streams whose source regions are
under debate. A key goal of ESA/NASA’s Solar Orbiter mission is to identify
solar wind sources and understand what drives the complexity seen in the
heliosphere. By combining magnetic feld modelling and spectroscopic
techniques with high-resolution observations and measurements, we show
that the solar wind variability detected in situ by Solar Orbiter in March
2022 is driven by spatio-temporal changes in the magnetic connectivity to
multiple sources in the solar atmosphere. The magnetic feld footpoints
connected to the spacecraft moved from the boundaries of a coronal hole
to one active region (12961) and then across to another region (12957). This
is refected in the in situ measurements, which show the transition from fast
to highly Alfvénic then to slow solar wind that is disrupted by the arrival of
a coronal mass ejection. Our results describe solar wind variability at 0.5 au
but are applicable to near-Earth observatories.
Cancer cell metabolism: special Reference to Lactate PathwayAADYARAJPANDEY1
Normal Cell Metabolism:
Cellular respiration describes the series of steps that cells use to break down sugar and other chemicals to get the energy we need to function.
Energy is stored in the bonds of glucose and when glucose is broken down, much of that energy is released.
Cell utilize energy in the form of ATP.
The first step of respiration is called glycolysis. In a series of steps, glycolysis breaks glucose into two smaller molecules - a chemical called pyruvate. A small amount of ATP is formed during this process.
Most healthy cells continue the breakdown in a second process, called the Kreb's cycle. The Kreb's cycle allows cells to “burn” the pyruvates made in glycolysis to get more ATP.
The last step in the breakdown of glucose is called oxidative phosphorylation (Ox-Phos).
It takes place in specialized cell structures called mitochondria. This process produces a large amount of ATP. Importantly, cells need oxygen to complete oxidative phosphorylation.
If a cell completes only glycolysis, only 2 molecules of ATP are made per glucose. However, if the cell completes the entire respiration process (glycolysis - Kreb's - oxidative phosphorylation), about 36 molecules of ATP are created, giving it much more energy to use.
IN CANCER CELL:
Unlike healthy cells that "burn" the entire molecule of sugar to capture a large amount of energy as ATP, cancer cells are wasteful.
Cancer cells only partially break down sugar molecules. They overuse the first step of respiration, glycolysis. They frequently do not complete the second step, oxidative phosphorylation.
This results in only 2 molecules of ATP per each glucose molecule instead of the 36 or so ATPs healthy cells gain. As a result, cancer cells need to use a lot more sugar molecules to get enough energy to survive.
Unlike healthy cells that "burn" the entire molecule of sugar to capture a large amount of energy as ATP, cancer cells are wasteful.
Cancer cells only partially break down sugar molecules. They overuse the first step of respiration, glycolysis. They frequently do not complete the second step, oxidative phosphorylation.
This results in only 2 molecules of ATP per each glucose molecule instead of the 36 or so ATPs healthy cells gain. As a result, cancer cells need to use a lot more sugar molecules to get enough energy to survive.
introduction to WARBERG PHENOMENA:
WARBURG EFFECT Usually, cancer cells are highly glycolytic (glucose addiction) and take up more glucose than do normal cells from outside.
Otto Heinrich Warburg (; 8 October 1883 – 1 August 1970) In 1931 was awarded the Nobel Prize in Physiology for his "discovery of the nature and mode of action of the respiratory enzyme.
WARNBURG EFFECT : cancer cells under aerobic (well-oxygenated) conditions to metabolize glucose to lactate (aerobic glycolysis) is known as the Warburg effect. Warburg made the observation that tumor slices consume glucose and secrete lactate at a higher rate than normal tissues.
Richard's entangled aventures in wonderlandRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
Slide 1: Title Slide
Extrachromosomal Inheritance
Slide 2: Introduction to Extrachromosomal Inheritance
Definition: Extrachromosomal inheritance refers to the transmission of genetic material that is not found within the nucleus.
Key Components: Involves genes located in mitochondria, chloroplasts, and plasmids.
Slide 3: Mitochondrial Inheritance
Mitochondria: Organelles responsible for energy production.
Mitochondrial DNA (mtDNA): Circular DNA molecule found in mitochondria.
Inheritance Pattern: Maternally inherited, meaning it is passed from mothers to all their offspring.
Diseases: Examples include Leber’s hereditary optic neuropathy (LHON) and mitochondrial myopathy.
Slide 4: Chloroplast Inheritance
Chloroplasts: Organelles responsible for photosynthesis in plants.
Chloroplast DNA (cpDNA): Circular DNA molecule found in chloroplasts.
Inheritance Pattern: Often maternally inherited in most plants, but can vary in some species.
Examples: Variegation in plants, where leaf color patterns are determined by chloroplast DNA.
Slide 5: Plasmid Inheritance
Plasmids: Small, circular DNA molecules found in bacteria and some eukaryotes.
Features: Can carry antibiotic resistance genes and can be transferred between cells through processes like conjugation.
Significance: Important in biotechnology for gene cloning and genetic engineering.
Slide 6: Mechanisms of Extrachromosomal Inheritance
Non-Mendelian Patterns: Do not follow Mendel’s laws of inheritance.
Cytoplasmic Segregation: During cell division, organelles like mitochondria and chloroplasts are randomly distributed to daughter cells.
Heteroplasmy: Presence of more than one type of organellar genome within a cell, leading to variation in expression.
Slide 7: Examples of Extrachromosomal Inheritance
Four O’clock Plant (Mirabilis jalapa): Shows variegated leaves due to different cpDNA in leaf cells.
Petite Mutants in Yeast: Result from mutations in mitochondrial DNA affecting respiration.
Slide 8: Importance of Extrachromosomal Inheritance
Evolution: Provides insight into the evolution of eukaryotic cells.
Medicine: Understanding mitochondrial inheritance helps in diagnosing and treating mitochondrial diseases.
Agriculture: Chloroplast inheritance can be used in plant breeding and genetic modification.
Slide 9: Recent Research and Advances
Gene Editing: Techniques like CRISPR-Cas9 are being used to edit mitochondrial and chloroplast DNA.
Therapies: Development of mitochondrial replacement therapy (MRT) for preventing mitochondrial diseases.
Slide 10: Conclusion
Summary: Extrachromosomal inheritance involves the transmission of genetic material outside the nucleus and plays a crucial role in genetics, medicine, and biotechnology.
Future Directions: Continued research and technological advancements hold promise for new treatments and applications.
Slide 11: Questions and Discussion
Invite Audience: Open the floor for any questions or further discussion on the topic.
Comparative structure of adrenal gland in vertebrates
Origin and Abundance of elements in the Solar system and in the Earth and its Constituents
1. ORIGIN AND ABUNDANCE OF ELEMENTS
IN THE SOLAR SYSTEM AND IN THE
EARTH AND ITS CONSTITUENTS
Akshay D. Raut
M.Sc. Sem III
Department of Earth And
Environmental Science
2. ELEMENTS
Elements are the simplest pure substances
Made of only one kind of material, has
definite properties, and is the same all
throughout.
They cannot be broken down into simpler
substances without losing their identity.
3. ELEMENTS AND ATOMS
• The smallest particle of an element that
has the properties of that element is called
an atom.
• Atoms of same element are alike; atoms of
different elements are different.
4. ORIGIN OF UNIVERSE
BIG BANG THEORY
• A theory of Astronomy: the Universe originated 13.8
billions of years ago in an explosion from a Singularity.
• Singularity- A single point of nearly infinite energy
density- where all known space was compressed into an
infinitely small mass.
• In the first second after the universe began, the
surrounding temperature was about 5.5 billion Celsius,
according to NASA.
• After the Big Bang only the lightest elements were formed
– Hydrogen and Helium along with trace amount of
Lithium and Beryllium.
5. ORIGIN OF THE SOLAR SYSTEM AND THE EARTH
• The earliest accounts of how the sun, the Earth
and the rest of the solar system were formed are
to be found in early myths, legends and religious
texts. None of these can be considered a serious
scientific account.
• The earliest scientific attempts to explain the
origin of solar system invoked collision or
condensation from a gas cloud.
6. Continued….
Theories of Origin of Solar System -
Evolutionary Theories – Suggests that planets are formed
during the evolution of the Sun.
Ex. Nebular Hypothesis
Catastrophic Theories – Suggests that planets are formed
by some special accident or catastrophe, such as close
approach of two stars or collision of two stars.
Ex. Planetisimal Hypothesis, Gaseous Tidal Hypothesis.
9. ORIGIN OF ELEMENTS IN THE SOLAR SYSTEM
AND THE EARTH
• Equilibrium Theory - Frozen thermodynamic equilibrium
between atomic nuclei at some high temperature and
density.
• When the universe was first created, essentially all matter
was in the form of two elements- hydrogen and helium
with relative abundance ( by weight ) of 75% and 25%
respectively.
• Further expansion and cooling allowed the neutrons and
some of the protons to fuse to helium nuclei. During
condensation period to today – Hydrogen (73%), Helium
(25%) and other elements (2%).
10. Continued…..
Elemental matter started with hydrogen, which formed the
primitive matter from which stars were made.
• Hydrogen burning to produce helium.
• Two atoms of hydrogen are combined in a series of steps to
create helium-4.
These two reactions account for 85% of the Sun’s
energy. The remaining 15% comes from reactions that produce
the elements beryllium and lithium.
The energy from these nuclear reactions is emitted in
various forms of radiation. Energised particles such as
neutrinos and protons are released and it is then make up the
solar wind.
This energy streams warms the planet, drives weather
and provides energy for life on the Earth.
11. Dying Stars
When a star’s core run out of hydrogen, the star begins to
die out. The dying star expands into a red giant, and this now
begins to manufacture carbon atoms by fusing helium atoms.
Example of element making in helium burning reactions:
• 3 4He= 12C
• 12C+4He= 16O
• 16O+4He= 20Ne
• 20Ne+4He= 24Mg
12. Man-Made Elements
Only 90 of the 116 known elements occur naturally.
The remaining 26 found in the development of
nuclear power plants and machines known as
particle accelerators.
For Ex- By allowing fast neutrons to collide with the
common isotope of uranium known as U-238 in a
nuclear reactor, the new element plutonium was
made.
13. CHEMICAL COMPOSITION OF SOLAR
ATMOSPHERE
Element Name Abundance %
Hydrogen 73
Helium 25
Oxygen 0.80
Carbon 0.36
Iron 0.12
Other Elements 0.72
14. CHEMICAL COMPOSITION OF PLANETS
Mercury – No atmosphere and density similar to the Earth.
Composition of Mercury is probably high in iron.
Venus – Size and mass of Venus suggests its composition is
probably much like that of Earth. It has very dense
atmosphere, consisting entirely of CO2 and Nitrogen.
Mars - Clouds and dust storms have been observed on the
face of Mars. Polar frost caps form in winter and disappear
in summer. These caps appear to be formed thin layer of
H2O ice with some solid CO2. Much of surface of Mars has a
reddish or orange coloration, which may be due to iron
oxide coating. The size and mass indicate a bulk composition
similar to that of Earth. Oblateness of Mars and lack of
magnetic field suggests that it does not have fluid core.
15. Continued…..
Jupiter, Saturn, Uranus, Neptune –
Interior similar to that of Earth, but covered with great
thickness of ice and condensed gases and have atmosphere
containing hydrogen, helium, nitrogen, methane and
ammonia.
Ring of Saturn probably consist of ice particles.
The albedos and densities of some of the satellites of these
planets suggests that they consist largely of ice.
16. CHEMICAL COMPOSITION OF THE EARTH
Sl. No Elements By Weight (%)
1 Oxygen 46.60
2 Silicon 27.72
3 Aluminium 8.13
4 Iron 5.00
5 Calcium 3.63
6 Sodium 2.83
7 Potassium 2.59
8 Magnesium 2.09
9 Others 1.41
18. Comet
An object that moves around then sun, usually
at a great distance from it, that is seen on rare
occasions from the Earth as a bright line in the sky.
They are composed of rock, dust, water ice and
frozen gases such as co, co2, methane and ammonia
19. COMPOSITION OF METEORITES
• On the basis of composition, Meteorites can be classified
as follows
1. Siderites or Irons ( Average 98% metal)
2. Siderolites and Stony irons ( Average 50% metal
and 50% Silicates )
3. Aerolites or Stones
a)Chondrites
b) Achondrites
20. ABUNDANCE OF ELEMENTS
• The abundances show a rapid exponential decrease for
elements of lower atomic numbers ( to about atomic
number 40), followed by almost constant value for the
heavier value for the heavier elements.
• Elements of even atomic number are more abundant than
those of odd atomic numbers on either side.
• The relative abundances for elements of higher atomic
number than nickel vary less than those for elements of
lower atomic number.
• Only 10 elements – H, He, C, N, O, Ne, Mg, Si, and Fe, all
with atomic numbers than 27.
• There is pronounced abundance peak at atomic number
26 and smaller peaks at several other heavier atomic
numbers.