Environmental science Module 1 Topic. This PPT is not a work of mine and was provided by our college professor during our graduation, so I am not sure about the original author. The credit goes to the Original author.
Environmental science Module 1 Topic. This PPT is not a work of mine and was provided by our college professor during our graduation, so I am not sure about the original author. The credit goes to the Original author.
The nitrogen cycle is the biogeochemical cycle by which nitrogen is converted into various chemical forms as it circulates among the atmosphere and terrestrial and marine ecosystems. The conversion of nitrogen can be carried out through both biological and physical processes. Important processes in the nitrogen cycle include fixation, ammonification, nitrification, and denitrification. The majority of Earth's atmosphere (78%) is nitrogen, making it the largest pool of nitrogen. However, atmospheric nitrogen has limited availability for biological use, leading to a scarcity of usable nitrogen in many types of ecosystems. The nitrogen cycle is of particular interest to ecologists because nitrogen availability can affect the rate of key ecosystem processes, including primary production and decomposition. Human activities such as fossil fuel combustion, use of artificial nitrogen fertilizers, and release of nitrogen in wastewater have dramatically altered the global nitrogen cycle.
Carbon cycle ppt
definition of Carbon cycle ppt
types of Carbon cycle ppt
discovery of Carbon cycle ppt
importance of Carbon cycle ppt
steps of Carbon cycle ppt
carbon cycle in water
harmful effect of Carbon cycle ppt
Introduction,Definition, Cycling elements, Types of biogeochemical cycle- Gaseous cycle and sedimentary cycle Nitrogen cycle, steps of Nitrogen cycle- Nitrogen fixation, Nitrification, Assimilation Ammonification, and Denitrification and ecological function of nitrogen, use of nitrogen cycle phosphorus cycle, steps of phosphorus cycle, biological functions of phosphorus cycle and other functions of phosphorus and conclusion
The nitrogen cycle is the biogeochemical cycle by which nitrogen is converted into various chemical forms as it circulates among the atmosphere and terrestrial and marine ecosystems. The conversion of nitrogen can be carried out through both biological and physical processes. Important processes in the nitrogen cycle include fixation, ammonification, nitrification, and denitrification. The majority of Earth's atmosphere (78%) is nitrogen, making it the largest pool of nitrogen. However, atmospheric nitrogen has limited availability for biological use, leading to a scarcity of usable nitrogen in many types of ecosystems. The nitrogen cycle is of particular interest to ecologists because nitrogen availability can affect the rate of key ecosystem processes, including primary production and decomposition. Human activities such as fossil fuel combustion, use of artificial nitrogen fertilizers, and release of nitrogen in wastewater have dramatically altered the global nitrogen cycle.
Carbon cycle ppt
definition of Carbon cycle ppt
types of Carbon cycle ppt
discovery of Carbon cycle ppt
importance of Carbon cycle ppt
steps of Carbon cycle ppt
carbon cycle in water
harmful effect of Carbon cycle ppt
Introduction,Definition, Cycling elements, Types of biogeochemical cycle- Gaseous cycle and sedimentary cycle Nitrogen cycle, steps of Nitrogen cycle- Nitrogen fixation, Nitrification, Assimilation Ammonification, and Denitrification and ecological function of nitrogen, use of nitrogen cycle phosphorus cycle, steps of phosphorus cycle, biological functions of phosphorus cycle and other functions of phosphorus and conclusion
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 .
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.
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.
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.
The increased availability of biomedical data, particularly in the public domain, offers the opportunity to better understand human health and to develop effective therapeutics for a wide range of unmet medical needs. However, data scientists remain stymied by the fact that data remain hard to find and to productively reuse because data and their metadata i) are wholly inaccessible, ii) are in non-standard or incompatible representations, iii) do not conform to community standards, and iv) have unclear or highly restricted terms and conditions that preclude legitimate reuse. These limitations require a rethink on data can be made machine and AI-ready - the key motivation behind the FAIR Guiding Principles. Concurrently, while recent efforts have explored the use of deep learning to fuse disparate data into predictive models for a wide range of biomedical applications, these models often fail even when the correct answer is already known, and fail to explain individual predictions in terms that data scientists can appreciate. These limitations suggest that new methods to produce practical artificial intelligence are still needed.
In this talk, I will discuss our work in (1) building an integrative knowledge infrastructure to prepare FAIR and "AI-ready" data and services along with (2) neurosymbolic AI methods to improve the quality of predictions and to generate plausible explanations. Attention is given to standards, platforms, and methods to wrangle knowledge into simple, but effective semantic and latent representations, and to make these available into standards-compliant and discoverable interfaces that can be used in model building, validation, and explanation. Our work, and those of others in the field, creates a baseline for building trustworthy and easy to deploy AI models in biomedicine.
Bio
Dr. Michel Dumontier is the Distinguished Professor of Data Science at Maastricht University, founder and executive director of the Institute of Data Science, and co-founder of the FAIR (Findable, Accessible, Interoperable and Reusable) data principles. His research explores socio-technological approaches for responsible discovery science, which includes collaborative multi-modal knowledge graphs, privacy-preserving distributed data mining, and AI methods for drug discovery and personalized medicine. His work is supported through the Dutch National Research Agenda, the Netherlands Organisation for Scientific Research, Horizon Europe, the European Open Science Cloud, the US National Institutes of Health, and a Marie-Curie Innovative Training Network. He is the editor-in-chief for the journal Data Science and is internationally recognized for his contributions in bioinformatics, biomedical informatics, and semantic technologies including ontologies and linked data.
2. The term biogeochemical tells us that Biological, Geological &
Chemical factors are involved.
In earth science, a biogeochemical cycle is a pathway by which a
chemical substances moves through both Biotic(Biosphere) &
Abiotic(Lithosphere, Atmosphere & Hydrosphere) compartments of earth.
A cycle is a series of change which comes back to the starting point &
which can be repeated.
INTRODUCTION
3. – “ More or less circular pathways, through which the
chemical elements, including all the essential elements of
the protoplasm, circulate in the biosphere from environment
to organisms and back to the environment, are known as the
Biogeochemical cycle”.
Biogeochemical cycles always involve Hot equilibrium states:
A balance in the cycling of the elements between
compartments.
As biogeochemical cycles describe the movements of
substances on the entire globe, the study of these is inherently
multidisciplinary.
DEFINATION
4. Macronutrients: required in relatively large
amounts
“Big six": Carbon , Hydrogen , Oxygen , Nitrogen,
Phosphorous.
other Macronutrients:
Sulfur, Potassium , Calcium , Iron , Magnesium
Micronutrients: required in very small amounts,
(but still necessary)
Boron
Copper
Molybdenum
CYCLING ELEMENTS
5. TYPE OF BIOGEOCHEMICAL CYCLE
Biogeochemical cycles can be
classed as;
GASEOUS CYCLE – The term
gaseous cycle refers to the
transformation of gases
between various biogeochemical
reservoirs; Hydrosphere,
Atmosphere & Biosphere
Important gaseous cycles are;
a) NITROGEN CYCLE
b) OXYGEN CYCLE
c) CARBON CYCLE
d) WATER CYCLE
6. Sedimentary cycles include the
leaching of minerals & salt’s from
the earth’s crust, which the settle as
sediment or rock before the cycle
repeats. Sedimentary cycle includes;
a) PHOSPHORUS CYCLE
b) SULFUR CYCLE
c) IRON CYCLE
d) CALCIUM CYCLE
Sedimentary cycles vary from one
elements to another, but each cycle
consist fundamentally of a solution
phase & a sediment phase.
SEDIMENTARY CYCLE
LITHOSPHERE
7. The majority of earth’s atmosphere is Nitrogen(78%).
However, Atmospheric N2 has limited availability for
biological use, and this form is relatively nonreactive and
unusable by plants.
Nitrogen availability can affect the rate of key ecosystem
processes including primary production and decomposition
The Nitrogen(N2) cycle is the process by which N2 is
converted between its various chemical forms.
This transformation can be carried out through both
biological & physical processes.
NITROGEN CYCLE
8.
9. The nitrogen cycle processes
The processes involved in a complete nitrogen
cycle are:
Nitrogen fixation:
Atmospheric nitrogen is converted into the
usable form by lightning strikes or symbiotic
bacteria which are known as Diazotrophs. These
bacteria consist of a nitrogenase enzyme which
has the capability to combine gaseous nitrogen
with hydrogen to form ammonia.
10.
11. Ammonification
When plants or animal die organic nitrogen is
again released back into the soil. Bacteria or fungi
present in the soil convert them back into
ammonium. This process is also called as
mineralization.
Assimilation
Primary producers take in this gas from the soil
with the help of their roots in the form of amino
acids, nitrite ions, nitrate ions or ammonium ions.
This way it enters the food cycle when the
consumers eat the plants.
13. In this process, the ammonia is converted into
nitrate by the presence of bacteria in the soil.
Ammonia is oxidized to form nitrites by bacteria
such as Nitrosomonas species.
Nitrates are converted into nitrates by Nitrobacter.
This conversion is very important as ammonia gas
is toxic for plants.
Nitrification
14. Denitrification
In order to complete the nitrogen cycle, the nitrites
are reduced back to inert nitrogen gas in this process.
This is done by bacterial species such as Clostridium
and Pseudomonas in the absence of oxygen.
To learn more about the nitrogen cycle, visit BYJU’S.
15. The phosphorus cycle is the slowest Biogeochemical cycle
that describes the movements of phosphorus(P) through
the Lithosphere, Hydrosphere & Biosphere.
Unlike many other biogeochemical cycles, the atmosphere
does not play a significant role in the movements of
phosphorus.
It is an essential nutrient for plants and animals.
It is a part of DNA-molecules and RNA-molecules,
molecules that store energy (ATP and ADP)
It is also a building block of certain parts of the human
and animal body, such as the bones and teeth.
Phosphorus Cycle
16.
17. Ecological Function
Phosphorus is an essential nutrient for
plants and animals.
Limiting nutrient for aquatic
organisms.
Forms parts of important lifesustaining
molecules that are very common in the
biosphere.
18. Biological Function
The primary biological importance of
phosphates is as a component of nucleotides,
which serve as energy storage within cells
(ATP) or when linked together, form the
nucleic acids DNA and RNA..
19. Ecology and Environment – P. D. SHARMA
Biogeochemical cycle – Wikipedia, the free
encyclopedia.
REFERENCE