Brachiopods are marine invertebrates with hard shells known as valves. They are divided into two classes - Articulata and Inarticulata. Articulata have valves that are hinged and can open, while Inarticulata valves are cemented together and cannot open. Brachiopods live with their lophophore protruding between the valves to filter feed on plankton. Their shells have distinct features like teeth and sockets that interlock the valves together. Brachiopods were most common in the Paleozoic era and remain important index fossils for determining paleoenvironments.
MORPHOLOGY AND SIGNIFICANCE OF CONODONT (group-D).pptxKuki Boruah
Conodonts are marine organism ranging from Cambrian to Triassic periods, having a long wormlike body, numerous small teeth and a pair of eyes.
It is now believed as the earliest vertebrate and now it is an extinct group of organism.
First identified by the LATVIAN embryologist and palaeontologist Christian Pander in 1856.
Conodonts are most frequently occuring fossil in marine Sedimentary Rocks.
Size of Conodonts commonly in between 200 microns and 5 millimetres.
The preserved color varying from translucent and colorless through light brown to black.
Brief description on Phylum Brachiopods with general terms used for Paleontology.
Structure paleoecology, geography, morphology.
And also easily understandable as since it discuss only specific terms only.
Graptolites is an important index fossil for Paleozoic rocks and common throughout the world. As in Pakistan the sequences from the Ordovician to carboniferous age missing but these strata are exist in Noshehra and Chitral, so thats why its more valuable as regional fossil of sub-continent.
MORPHOLOGY AND SIGNIFICANCE OF CONODONT (group-D).pptxKuki Boruah
Conodonts are marine organism ranging from Cambrian to Triassic periods, having a long wormlike body, numerous small teeth and a pair of eyes.
It is now believed as the earliest vertebrate and now it is an extinct group of organism.
First identified by the LATVIAN embryologist and palaeontologist Christian Pander in 1856.
Conodonts are most frequently occuring fossil in marine Sedimentary Rocks.
Size of Conodonts commonly in between 200 microns and 5 millimetres.
The preserved color varying from translucent and colorless through light brown to black.
Brief description on Phylum Brachiopods with general terms used for Paleontology.
Structure paleoecology, geography, morphology.
And also easily understandable as since it discuss only specific terms only.
Graptolites is an important index fossil for Paleozoic rocks and common throughout the world. As in Pakistan the sequences from the Ordovician to carboniferous age missing but these strata are exist in Noshehra and Chitral, so thats why its more valuable as regional fossil of sub-continent.
Trilobites are extinct group in fossil record TimeMarkers
Biozone markers
Paleoclimatic indicators Stratigraphic boundarymarkers Significance in Phylogenic studies
Good time markers in Cambrian-Permianas
Index fossils
Short lived but long and significant markers in Stratigraphic studies.
Ichnology,classification & significance of trace fossilUjjavalPatel16
Ichnology,classification& significance of trace fossil
Most trace fossils are largely facies dependant.
No secondary displacement or transport.
Trace fossils are common in rocks that otherwise are unfossiliferous. (siliciclastics, shorelines)
Non-preservation of the causative organism.
Multiple architects may produce a single structure.
The same individual can produce different structures corresponding to different behavior.
The same individual may produce different structures corresponding with identical behavior but in different substrates.
Identical structures may be produced by the activity of systematically different organisms where behavior is similar.
Abundance - one animal, especially if mobile, can make many traces during its lifetime, whereas it may or may not have its body preserved in the fossil record.
Trilobites are extinct group in fossil record TimeMarkers
Biozone markers
Paleoclimatic indicators Stratigraphic boundarymarkers Significance in Phylogenic studies
Good time markers in Cambrian-Permianas
Index fossils
Short lived but long and significant markers in Stratigraphic studies.
Ichnology,classification & significance of trace fossilUjjavalPatel16
Ichnology,classification& significance of trace fossil
Most trace fossils are largely facies dependant.
No secondary displacement or transport.
Trace fossils are common in rocks that otherwise are unfossiliferous. (siliciclastics, shorelines)
Non-preservation of the causative organism.
Multiple architects may produce a single structure.
The same individual can produce different structures corresponding to different behavior.
The same individual may produce different structures corresponding with identical behavior but in different substrates.
Identical structures may be produced by the activity of systematically different organisms where behavior is similar.
Abundance - one animal, especially if mobile, can make many traces during its lifetime, whereas it may or may not have its body preserved in the fossil record.
Corals are marine invertebrates in class Anthozoa of phylum Cnidaria typically living in compact colonies of many identical individual "polyps".
Corals are gastrovascular marine organisms. Each one of these animals is known as a coral
"polyp". Coral Polyps are tiny, primitive marine organisms.
A single polyp has a tube-shaped body with a mouth which is surrounded by tentacles.
The polyp of hard corals produces a stony skeleton of calcium carbonate which form the base. Often the skeleton forms a cup-like structure in which the polyp lives. Coral polyps in colonies make up the cora reefs.
The analysis of all of the significant processes that formed a basin and deformed its sedimentary fill from basin-scale processes (e.g., plate tectonics)
to centimeter-scale processes (e.g., fracturing)
Seismic waves are the waves of energy caused by the sudden breaking of rock within the earth or an explosion.
Response of material to the arrival of energy fronts released by rupture.
Energy that travels through the earth and is recorded on seismographs.
A fossil is the preserved remains of a once-living organism.
Fossils give clues about organisms that lived long ago. They help to show that evolution has occurred.
They also provide evidence about how Earth’s surface has changed over time.
Fossils help scientists understand what past environments may have been like.
A fossil is an impression, cast,
original material or track of any animal or plant that is preserved in rock after the original organic material is transformed or removed.
Second-largest phylum in number of species- over 100,000 described.
Ecologically widespread- marine, freshwater, terrestrial (gastropods very successful on land)
Variety of body plans (therefore, many classes within the phylum)
Variety in body size- from ~1 mm to ~18 m (60 feet). 80% are under 5 cm, but many are large and therefore significant as food for man.
A synthetic gemstone is identical to a natural gemstone in almost every way.This includes the same basic crystal structure, refractive index, specific gravity, chemical composition, colors, and other characteristics. Since the same gemological tests are used for stone identification on both natural and synthetic gems, it is sometimes even possible for a gemologist to be puzzled as to whether or not a stone is natural or synthetic. When this occurs, the best course of action is to send the stone to an accredited gem laboratory, like the Gemological Institute of America. They can positively determin ewhether a stone is synthetic or naturally occuring. Only minor internal characteristics allow separation of a synthetic gemstone from a natural gemston
This presentation explores a brief idea about the structural and functional attributes of nucleotides, the structure and function of genetic materials along with the impact of UV rays and pH upon them.
Richard's aventures in two entangled wonderlandsRichard 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.
Seminar of U.V. Spectroscopy by SAMIR PANDASAMIR PANDA
Spectroscopy is a branch of science dealing the study of interaction of electromagnetic radiation with matter.
Ultraviolet-visible spectroscopy refers to absorption spectroscopy or reflect spectroscopy in the UV-VIS spectral region.
Ultraviolet-visible spectroscopy is an analytical method that can measure the amount of light received by the analyte.
(May 29th, 2024) Advancements in Intravital Microscopy- Insights for Preclini...Scintica Instrumentation
Intravital microscopy (IVM) is a powerful tool utilized to study cellular behavior over time and space in vivo. Much of our understanding of cell biology has been accomplished using various in vitro and ex vivo methods; however, these studies do not necessarily reflect the natural dynamics of biological processes. Unlike traditional cell culture or fixed tissue imaging, IVM allows for the ultra-fast high-resolution imaging of cellular processes over time and space and were studied in its natural environment. Real-time visualization of biological processes in the context of an intact organism helps maintain physiological relevance and provide insights into the progression of disease, response to treatments or developmental processes.
In this webinar we give an overview of advanced applications of the IVM system in preclinical research. IVIM technology is a provider of all-in-one intravital microscopy systems and solutions optimized for in vivo imaging of live animal models at sub-micron resolution. The system’s unique features and user-friendly software enables researchers to probe fast dynamic biological processes such as immune cell tracking, cell-cell interaction as well as vascularization and tumor metastasis with exceptional detail. This webinar will also give an overview of IVM being utilized in drug development, offering a view into the intricate interaction between drugs/nanoparticles and tissues in vivo and allows for the evaluation of therapeutic intervention in a variety of tissues and organs. This interdisciplinary collaboration continues to drive the advancements of novel therapeutic strategies.
Nutraceutical market, scope and growth: Herbal drug technologyLokesh Patil
As consumer awareness of health and wellness rises, the nutraceutical market—which includes goods like functional meals, drinks, and dietary supplements that provide health advantages beyond basic nutrition—is growing significantly. As healthcare expenses rise, the population ages, and people want natural and preventative health solutions more and more, this industry is increasing quickly. Further driving market expansion are product formulation innovations and the use of cutting-edge technology for customized nutrition. With its worldwide reach, the nutraceutical industry is expected to keep growing and provide significant chances for research and investment in a number of categories, including vitamins, minerals, probiotics, and herbal supplements.
What is greenhouse gasses and how many gasses are there to affect the Earth.moosaasad1975
What are greenhouse gasses how they affect the earth and its environment what is the future of the environment and earth how the weather and the climate effects.
Deep Behavioral Phenotyping in Systems Neuroscience for Functional Atlasing a...Ana Luísa Pinho
Functional Magnetic Resonance Imaging (fMRI) provides means to characterize brain activations in response to behavior. However, cognitive neuroscience has been limited to group-level effects referring to the performance of specific tasks. To obtain the functional profile of elementary cognitive mechanisms, the combination of brain responses to many tasks is required. Yet, to date, both structural atlases and parcellation-based activations do not fully account for cognitive function and still present several limitations. Further, they do not adapt overall to individual characteristics. In this talk, I will give an account of deep-behavioral phenotyping strategies, namely data-driven methods in large task-fMRI datasets, to optimize functional brain-data collection and improve inference of effects-of-interest related to mental processes. Key to this approach is the employment of fast multi-functional paradigms rich on features that can be well parametrized and, consequently, facilitate the creation of psycho-physiological constructs to be modelled with imaging data. Particular emphasis will be given to music stimuli when studying high-order cognitive mechanisms, due to their ecological nature and quality to enable complex behavior compounded by discrete entities. I will also discuss how deep-behavioral phenotyping and individualized models applied to neuroimaging data can better account for the subject-specific organization of domain-general cognitive systems in the human brain. Finally, the accumulation of functional brain signatures brings the possibility to clarify relationships among tasks and create a univocal link between brain systems and mental functions through: (1) the development of ontologies proposing an organization of cognitive processes; and (2) brain-network taxonomies describing functional specialization. To this end, tools to improve commensurability in cognitive science are necessary, such as public repositories, ontology-based platforms and automated meta-analysis tools. I will thus discuss some brain-atlasing resources currently under development, and their applicability in cognitive as well as clinical neuroscience.
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 .
2. Copy diagram on pageCopy diagram on page
125 a) and b) Black125 a) and b) Black to show to show
a typical articulate a typical articulate
brachiopod.brachiopod.
They have 2 They have 2 VALVESVALVES
(shells) that totally enclose (shells) that totally enclose
the soft parts.the soft parts.
The average size is 20 - 70 The average size is 20 - 70
mm but can range up to 370 mm but can range up to 370
mm.mm.
The valves can open and are The valves can open and are
hinged at one end; muscles hinged at one end; muscles
open and close the shell.open and close the shell.
3. Morphology 2Morphology 2
They usually allow water into They usually allow water into
the shell, as they are filter the shell, as they are filter
feeders extracting food from feeders extracting food from
seawater.seawater.
The two valves are different The two valves are different
in size (as opposed to in size (as opposed to
bivalves).bivalves).
However; they do show a However; they do show a
line of lateral symmetryline of lateral symmetry
along the middle of the along the middle of the
animalanimal. . Highlight this onHighlight this on
your diagramyour diagram..
4. Morphology 3:Morphology 3:Naming of the valvesNaming of the valves
The smaller valve is the The smaller valve is the
BRACHIALBRACHIAL valve (upper in valve (upper in
life position).life position).
The larger valve is the The larger valve is the
PEDICLEPEDICLE valve (lower in life valve (lower in life
position).position).
The animal secretes the The animal secretes the
valves as it grows, the valves as it grows, the
original small shell is called original small shell is called
thethe UMBOUMBO and the shell and the shell
grows outwards from either grows outwards from either
side of this point. side of this point. Make sureMake sure
that you can see the umbothat you can see the umbo
on a hand specimen.on a hand specimen.
5. Morphology 4:Morphology 4:
Often the pedicle valve has aOften the pedicle valve has a
small circular openingsmall circular opening
((FORAMENFORAMEN) at the end) at the end
through which a type of footthrough which a type of foot
extends called theextends called the
PEDICLEPEDICLE.. Make sure thatMake sure that
you can see the foramen inyou can see the foramen in
a hand specimen.a hand specimen.
The pedicle allows theThe pedicle allows the
brachiopod to attach itself tobrachiopod to attach itself to
the sea floor.the sea floor.
Inside the shell the body fillsInside the shell the body fills
much of the body cavity.much of the body cavity.
6. Morphology 5:Morphology 5:
Some shells like rhynchonellidsSome shells like rhynchonellids
have ahave a wrinkly COMMISUREwrinkly COMMISURE
withwith FOLDSFOLDS (one on either(one on either
side of the sulcus)side of the sulcus) and aand a
SULCUS (in the middle)SULCUS (in the middle)..
Draw a rhynchonellid showingDraw a rhynchonellid showing
the fold and sulcus and thethe fold and sulcus and the
inhalentinhalent andand exhalentexhalent currents.currents.
Folds have inhalent and sulcusFolds have inhalent and sulcus
has the exhalent.has the exhalent.
The currents are thereforeThe currents are therefore
separated.separated.
The crenulated commissureThe crenulated commissure
also provides a greater surfacealso provides a greater surface
area.area.
7. The inside of the shell is theThe inside of the shell is the
MANTLE CAVITYMANTLE CAVITY and is mainlyand is mainly
thethe LOPHOPHORE, whichLOPHOPHORE, which is ais a
food gathering and water-food gathering and water-
filtering device.filtering device.
Draw diagram (d) fromDraw diagram (d) from
page 125 Black.page 125 Black.
The important muscles are:The important muscles are:
At the posterior end is theAt the posterior end is the
pedicle “foot” type ofpedicle “foot” type of
ligament/muscle which whenligament/muscle which when
extended could usually reachextended could usually reach
outside of the shell.outside of the shell.
The main muscles were theThe main muscles were the
ADDUCTOR and DIDUCTORADDUCTOR and DIDUCTOR
muscles, which were used tomuscles, which were used to
close the shell.close the shell.
8. Internal morphology 2:Internal morphology 2:
Draw diagrams from pageDraw diagrams from page
125 Black:125 Black:
c)c) for muscle position.for muscle position.
e) and f)e) and f) showing internal viewsshowing internal views
of shells with muscle scars.of shells with muscle scars.
Both sets of muscles wereBoth sets of muscles were
attached to the shell andattached to the shell and
although not preserved in thealthough not preserved in the
fossils there are scars left fromfossils there are scars left from
where the muscles werewhere the muscles were
attached to the shell.attached to the shell.
TheThe CARDINAL PROCESSCARDINAL PROCESS andand
HINGEHINGE acts as a fulcrum onacts as a fulcrum on
which the muscles can pull.which the muscles can pull.
The diductor muscles contractThe diductor muscles contract
and pull down the cardinaland pull down the cardinal
process and open the shell.process and open the shell.
9. Internal Morphology 3:Internal Morphology 3:
As the diductor musclesAs the diductor muscles
relax the adductor musclesrelax the adductor muscles
contract and close the shell.contract and close the shell.
Role of theRole of the lophophorelophophore is tois to
act as a feeding device,act as a feeding device,
which collects suspendedwhich collects suspended
particles.particles.
Some brachiopods likeSome brachiopods like
spiriferids have a spiralspiriferids have a spiral
calcite support called acalcite support called a
lophophore support orlophophore support or
spiralia.spiralia.
Draw diagram d on pageDraw diagram d on page
137.137.
10. Internal morphology 4:Internal morphology 4:
On the diagram you can seeOn the diagram you can see
that the brachiopod hasthat the brachiopod has
TEETHTEETH (pedicle valve) and(pedicle valve) and
SOCKETSSOCKETS (brachial valve).(brachial valve).
What do you think the role ofWhat do you think the role of
these are?these are?
11. Articulate Brachiopod Orders:Articulate Brachiopod Orders:
There are 7 orders.There are 7 orders.
(including Productids).(including Productids).
For each draw a simpleFor each draw a simple
diagram.diagram.
Make a note of the typeMake a note of the type
of hinge line:of hinge line:
Long orLong or
ShortShort
12. They tended to live inThey tended to live in
shallow marine conditionsshallow marine conditions
(up to 500 m but may go(up to 500 m but may go
down to 6, 000m).down to 6, 000m).
Modern forms live in cool -Modern forms live in cool -
temperate waters around thetemperate waters around the
Pacific (Japan, S. Australia,Pacific (Japan, S. Australia,
New Zealand, N. AtlanticNew Zealand, N. Atlantic
and W. Scotland).and W. Scotland).
As there are modern dayAs there are modern day
equivalents we know theirequivalents we know their
environments and so theyenvironments and so they
are good palaeoenvironmentare good palaeoenvironment
indicators (indicators (index fossilsindex fossils).).
13. Index fossils etc.Index fossils etc.
Define an index fossil:Define an index fossil:
A fossil that is restricted to aA fossil that is restricted to a
particularparticular
palaeoenvironment.palaeoenvironment.
Corals mare perhaps theCorals mare perhaps the
best index fossils.best index fossils.
The most commonThe most common
question regardingquestion regarding
Brachiopods is how to tellBrachiopods is how to tell
the difference betweenthe difference between
them and Bivalves.them and Bivalves.
We will cover this next whenWe will cover this next when
we look at Bivalves.we look at Bivalves.
14. Brachiopods are a long-livedBrachiopods are a long-lived
Phylum ranging from thePhylum ranging from the
Cambrian to Present.Cambrian to Present.
They were very common inThey were very common in
the Palaeozoic and slightlythe Palaeozoic and slightly
less so in the Mesozoic butless so in the Mesozoic but
still remain important.still remain important.
In the Present not manyIn the Present not many
forms are left withforms are left with
approximately 70 Genera.approximately 70 Genera.
Over 2500 fossil Genera areOver 2500 fossil Genera are
known.known.
The largest were found inThe largest were found in
the Cambrian (370 mm).the Cambrian (370 mm).