1. The document defines soil inhabitants as organisms that live in soil for part or all of their life. It discusses the different types of living organisms found in soil, including archaea, bacteria, fungi, protists, and various fauna ranging from micro to macro in size.
2. Soil organisms play an important role in maintaining soil fertility, structure, and nutrient cycling. They break down organic matter, release nutrients, and convert them to forms usable by plants.
3. The document discusses the different size groups of soil organisms from micro to mega, providing examples such as protists, microfauna including protozoa and nematodes, mesofauna including mites and springtails, macrofauna
The document provides information about soil biology and biodiversity. It discusses the different types of organisms that inhabit soil, grouped into microbiota, mesofauna, and macrofauna based on their size. Microbiota includes microorganisms and microfauna less than 200 亮m in size that decompose organic matter. Mesofauna ranges from 200 亮m to 10 mm and includes microarthropods. Macrofauna are visible to the naked eye, such as earthworms, ants, and termites. These different soil organisms perform important functions like nutrient cycling, decomposition, and regulating soil structure. Certain macroinvertebrates like termites, ants, and earthworms are considered ecological engineers as they modify
Soils give a mechanical support to plants from which they extract nutrients. soil provides shelters for many animal types, from invertebrates such as worms and insects up to mammals like rabbits, moles, foxes and badgers. It also provides habitats colonised by a staggering variety of microorganisms. This module is about the microbial life in soils.
Soil microbiology- Microbes Associated with SoilSruthyPB3
油
This document summarizes the key points from a university lecture on soil microorganisms. It discusses the types and abundance of microorganisms found in soil, including bacteria, fungi, and protozoa. It explains the important roles microorganisms play in decomposing organic matter, cycling nutrients, enhancing soil structure, and maintaining soil quality. The document also covers how environmental factors like pH, phosphorus, and soil texture can influence microbial communities. In summary, soil microorganisms drive many critical ecosystem functions through their roles in decomposition and nutrient cycling.
Agricultural Microbiology: Role of microbes in soil fertilitySarthakMoharana
油
Description on different microbes which plays role in maintaining soil fertility.
Fertile soils teem with microorganisms, which directly contribute to the biological fertility of that soil.
Biological fertility is under-studied and our scientific knowledge of it is incomplete.
In addition to fertility, soil microorganisms also play essential roles in the nutrient cycles that are fundamentally important to life on the planet.
In the past, agricultural practices have failed to promote healthy populations of microorganisms, limiting production yields and threatening sustainability.
Scientific research is exploring new and exciting possibilities for the restoration and promotion of healthy microbial populations in the soil.
Soil is essential for the maintenance of biodiversity above and below ground. The wealth of biodiversity below ground is vast and unappreciated: millions of microorganisms live and reproduce in a few grams of topsoil, an ecosystem essential for life on earth
From:油Australian Soils and Landscape, An Illustrated Compendium
Soil microorganisms play a vital role in soil fertility and the nutrient cycles that support life. There are diverse types of microbes in soil including bacteria, fungi, actinomycetes, algae, protozoa, viruses, and nematodes. Each group serves important functions like decomposing organic matter, mineralizing nutrients, and supporting plant growth. A healthy population of soil microbes is essential for agricultural production and sustainability, but past practices have sometimes failed to promote microbial health. More research seeks to restore and promote soil microbes through improved agricultural methods.
Roots of plants and their decay contribute organic matter to soil which provides nutrients for microorganisms and plants. Bacteria, fungi, actinomycetes, and algae are important microflora in soil. Bacteria are the most abundant and come in various shapes. Fungi form networks and reproduce sexually and asexually. Actinomycetes are filamentous bacteria that degrade resistant organic compounds. Algae include single-celled and multicellular forms found in water and soil and are important for photosynthesis.
The document discusses microbial ecology and the composition of soil as an environment for microorganisms. It notes that soil is a complex ecosystem containing a vast array of microbes, plants, and animals. The lithosphere is composed of weathered rock, humus, and nutrients. The rhizosphere around plant roots contains associated bacteria, fungi, and protozoa. Microbes play important roles in soil, including nutrient provision, decomposition, nitrogen fixation, and preventing pathogens. Bacteria, actinomycetes, and fungi are the dominant microbial groups in soil and influence processes like nutrient cycling and plant growth.
This document describes the diversity of organisms found in soil and their roles in the ecosystem. It shows that bacteria are the most abundant, numbering in the tens of billions per gram of soil. Larger organisms like earthworms, beetles and spiders become fewer in number as size increases. All organisms contribute to nutrient cycling through decomposition of organic matter and predation on one another. The document explores key organisms like fungi, protozoa, nematodes, and mites under a microscope to show their forms and functions in soil.
The document provides information about the fundamentals of soil science. It discusses 5 units that cover topics like soil formation, physical properties, water and air movement in soil, reaction and pH, colloids, organic matter, soil organisms, and pollution. Unit 5 discusses how soil organisms can have both beneficial and harmful effects, and how pollution affects soil through pesticides and other contaminants. Prevention of pollution includes reducing deforestation and proper waste management.
B.sc. agri sem ii agricultural microbiology unit 2 soil microorganismsRai University
油
The document discusses the various microorganisms found in soil, including bacteria, actinomycetes, fungi, algae, protozoa, and higher animal forms. It describes the different groups of bacteria and microorganisms, their roles in soil processes like decomposition and nutrient cycling, and how they vary depending on environmental conditions. Methods for enumerating and classifying soil microorganisms are also summarized.
This document discusses the microbial flora of soil. It defines soil microflora as microorganisms that contribute to the biological properties of soil, including bacteria, fungi, algae, and protozoa. The five major groups interact and form a soil food web, with bacteria and fungi serving important roles in decomposition. Physical and chemical factors like pH and nutrients influence the growth and activity of soil microflora. The microflora are then classified and examples are given of bacteria, fungi, algae, protozoa, and their functions in the soil ecosystem.
The document provides an overview of microbial ecology in soil. It discusses soil as an environment for microorganisms and describes the typical soil habitat. It explains that soils can be divided into mineral and organic types and notes the key components of vegetated soils. The document also examines soil organic matter and the roles of microorganisms like bacteria, fungi, algae, protozoa, and others in soils. It discusses various microbe-plant interactions such as those in the rhizosphere, phyllosphere, and mycorrhizal associations.
Soil Biota and Organic Residue Decomposition MethodsSOUVIKGANGULY11
油
The document discusses soil components and soil organisms. It defines soil as a mixture of minerals, organic matter, gases, liquids, and organisms. The basic soil components are minerals, organic matter, water and air. Organic matter contains humus, roots, and organisms. Soil biota includes a wide variety of organisms that spend time in the soil profile or at the soil interface and contribute to nutrient cycling. These organisms include bacteria, fungi, algae, protozoa, nematodes, earthworms, insects and other invertebrates. When organic residues are added to soils, they are decomposed by the soil biota through a series of biological and chemical processes.
The document summarizes the abiotic and biotic components of ecosystems. Abiotic components include non-living factors like temperature, light intensity, and soil composition. Biotic components are the living plants and animals that interact with each other and their environment. These interactions include producer-consumer relationships in food chains and webs, as well as symbiotic relationships like mutualism, commensalism, parasitism, and saprophytism. Succession over time transforms environments like mangrove swamps as pioneer species establish and later species move in.
Soil biology is the study of microorganisms that live in soil, including their interactions with the environment and each other. There are many important groups of soil organisms including bacteria, fungi, protozoa, nematodes, micro- and mesofauna, and macrofauna like earthworms. Soil organisms carry out essential functions such as decomposition, nutrient cycling, and improving soil structure.
Earthworms
Earthworms are the intestine of the earth said Aristotle they decompose organic matter like plants leaving decaying fruits and soil also. The soil fertility increases with an increase in the nutrients, proper aeration, and water-holding capacity, along with these factors microbial activities also have a huge impact on the soil.
Soil is made up of particles of rocks, dead plants, and organisms and contains water and air. It supports plant growth by holding plants upright, providing nutrients, and allowing for water infiltration. Soil is teeming with life, including bacteria, fungi, protozoa, nematodes, arthropods, and earthworms. These organisms help decompose dead organic matter, recycle nutrients, improve soil structure, and support ecosystems both above and below ground.
The document discusses microbiology in terrestrial environments. It begins by defining terrestrial as living on land, and environment as surroundings. It then discusses the various types of terrestrial habitats like deserts and forests. [END SUMMARY]
This document discusses biodiversity and its importance. It defines biodiversity as the variety of life on Earth, including genetic, species, and ecosystem diversity. It notes that biodiversity forms the basis of the planet's productivity and natural systems, but that human activities over the last 50 years have resulted in substantial and largely irreversible loss of biodiversity. The five main causes of biodiversity loss are identified as habitat change, climate change, invasive species, overexploitation, and pollution.
Terrestrial ecosystems are ecosystems that exist on land, as opposed to aquatic ecosystems. They can vary greatly in size and include ecosystems like forests, grasslands, deserts, and tundra. Terrestrial ecosystems are characterized by greater temperature fluctuations, higher light availability, and more readily available gases than aquatic ecosystems. They contain a variety of plant life like flowering plants, conifers, and mosses, as well as many animal species including insects, birds, and mammals. Abiotic factors like temperature, sunlight, water, and wind all influence the living and non-living components of terrestrial ecosystems.
This document discusses the drilosphere, which is the zone of soil influenced by earthworm activity and casts. It describes the components of the drilosphere, including the earthworm gut microbiome and secretions, casts, middens, and burrows. These structures and secretions influence soil organic matter dynamics, microbial communities, aggregation, porosity, and plant growth. The drilosphere interacts closely with other spheres like the rhizosphere to regulate key soil functions over various spatial and temporal scales. Soil organic matter pools are also impacted, with earthworms and microbes influencing active and protected carbon.
Lichens , types of lichens based on growth and habitat, importance of lichens, fungal habits and colonization strategies, Air borne fungi and micotoxins.
The document provides information about the fundamentals of soil science. It discusses 5 units that cover topics like soil formation, physical properties, water and air movement in soil, reaction and pH, colloids, organic matter, soil organisms, and pollution. Unit 5 discusses how soil organisms can have both beneficial and harmful effects, and how pollution affects soil through pesticides and other contaminants. Prevention of pollution includes reducing deforestation and proper waste management.
B.sc. agri sem ii agricultural microbiology unit 2 soil microorganismsRai University
油
The document discusses the various microorganisms found in soil, including bacteria, actinomycetes, fungi, algae, protozoa, and higher animal forms. It describes the different groups of bacteria and microorganisms, their roles in soil processes like decomposition and nutrient cycling, and how they vary depending on environmental conditions. Methods for enumerating and classifying soil microorganisms are also summarized.
This document discusses the microbial flora of soil. It defines soil microflora as microorganisms that contribute to the biological properties of soil, including bacteria, fungi, algae, and protozoa. The five major groups interact and form a soil food web, with bacteria and fungi serving important roles in decomposition. Physical and chemical factors like pH and nutrients influence the growth and activity of soil microflora. The microflora are then classified and examples are given of bacteria, fungi, algae, protozoa, and their functions in the soil ecosystem.
The document provides an overview of microbial ecology in soil. It discusses soil as an environment for microorganisms and describes the typical soil habitat. It explains that soils can be divided into mineral and organic types and notes the key components of vegetated soils. The document also examines soil organic matter and the roles of microorganisms like bacteria, fungi, algae, protozoa, and others in soils. It discusses various microbe-plant interactions such as those in the rhizosphere, phyllosphere, and mycorrhizal associations.
Soil Biota and Organic Residue Decomposition MethodsSOUVIKGANGULY11
油
The document discusses soil components and soil organisms. It defines soil as a mixture of minerals, organic matter, gases, liquids, and organisms. The basic soil components are minerals, organic matter, water and air. Organic matter contains humus, roots, and organisms. Soil biota includes a wide variety of organisms that spend time in the soil profile or at the soil interface and contribute to nutrient cycling. These organisms include bacteria, fungi, algae, protozoa, nematodes, earthworms, insects and other invertebrates. When organic residues are added to soils, they are decomposed by the soil biota through a series of biological and chemical processes.
The document summarizes the abiotic and biotic components of ecosystems. Abiotic components include non-living factors like temperature, light intensity, and soil composition. Biotic components are the living plants and animals that interact with each other and their environment. These interactions include producer-consumer relationships in food chains and webs, as well as symbiotic relationships like mutualism, commensalism, parasitism, and saprophytism. Succession over time transforms environments like mangrove swamps as pioneer species establish and later species move in.
Soil biology is the study of microorganisms that live in soil, including their interactions with the environment and each other. There are many important groups of soil organisms including bacteria, fungi, protozoa, nematodes, micro- and mesofauna, and macrofauna like earthworms. Soil organisms carry out essential functions such as decomposition, nutrient cycling, and improving soil structure.
Earthworms
Earthworms are the intestine of the earth said Aristotle they decompose organic matter like plants leaving decaying fruits and soil also. The soil fertility increases with an increase in the nutrients, proper aeration, and water-holding capacity, along with these factors microbial activities also have a huge impact on the soil.
Soil is made up of particles of rocks, dead plants, and organisms and contains water and air. It supports plant growth by holding plants upright, providing nutrients, and allowing for water infiltration. Soil is teeming with life, including bacteria, fungi, protozoa, nematodes, arthropods, and earthworms. These organisms help decompose dead organic matter, recycle nutrients, improve soil structure, and support ecosystems both above and below ground.
The document discusses microbiology in terrestrial environments. It begins by defining terrestrial as living on land, and environment as surroundings. It then discusses the various types of terrestrial habitats like deserts and forests. [END SUMMARY]
This document discusses biodiversity and its importance. It defines biodiversity as the variety of life on Earth, including genetic, species, and ecosystem diversity. It notes that biodiversity forms the basis of the planet's productivity and natural systems, but that human activities over the last 50 years have resulted in substantial and largely irreversible loss of biodiversity. The five main causes of biodiversity loss are identified as habitat change, climate change, invasive species, overexploitation, and pollution.
Terrestrial ecosystems are ecosystems that exist on land, as opposed to aquatic ecosystems. They can vary greatly in size and include ecosystems like forests, grasslands, deserts, and tundra. Terrestrial ecosystems are characterized by greater temperature fluctuations, higher light availability, and more readily available gases than aquatic ecosystems. They contain a variety of plant life like flowering plants, conifers, and mosses, as well as many animal species including insects, birds, and mammals. Abiotic factors like temperature, sunlight, water, and wind all influence the living and non-living components of terrestrial ecosystems.
This document discusses the drilosphere, which is the zone of soil influenced by earthworm activity and casts. It describes the components of the drilosphere, including the earthworm gut microbiome and secretions, casts, middens, and burrows. These structures and secretions influence soil organic matter dynamics, microbial communities, aggregation, porosity, and plant growth. The drilosphere interacts closely with other spheres like the rhizosphere to regulate key soil functions over various spatial and temporal scales. Soil organic matter pools are also impacted, with earthworms and microbes influencing active and protected carbon.
Lichens , types of lichens based on growth and habitat, importance of lichens, fungal habits and colonization strategies, Air borne fungi and micotoxins.
Neutralization Reaction by Sarah Ashfaq 51 5.pptxSarah Ashfaq 51
油
Neutralization reaction A neutralization reaction is when an acid and a base react to form water and a salt and involves the combination of H+ ions and OH- ions to generate water. The neutralization of a strong acid and strong base has a pH equal to 7.
This document defines and describes different types of plant stems. It begins by introducing stems and their main functions of supporting leaves, flowers, and fruits and transporting water and nutrients. It then defines stems and lists their main characteristics. The bulk of the document categorizes 13 main types of stems, including herbaceous, woody, fistular, solid, jointed, cylindrical, angular, flattened, glaucous, glabrous, succulent, spiny, and prickly stems. Each type is defined and examples are provided. The document concludes that stems are the important structural axes of plants that support growth and transport water.
Virus transmission and dissemination in plants Sarah Ashfaq 51.pdfSarah Ashfaq 51
油
This document discusses various methods of virus transmission and dissemination in plants. It outlines 10 main methods of transmission: 1) seed transmission, 2) vegetative propagation, 3) mechanical transmission through sap, 4) soil transmission, 5) insect transmission, 6) transmission by fungi, 7) transmission by soil-inhabiting nematodes, 8) mite transmission, 9) pollen transmission, and 10) transmission by dodder. It provides examples for each method and discusses how viruses are transmitted and spread to uninfected plants.
This document provides information about the apple scab disease caused by the fungus Venturia inaequalis. It discusses the systematic position of the fungus, the symptoms of the disease including lesions on leaves and fruit, and the reproduction process involving both sexual reproduction through ascospores and asexual reproduction through conidia. The lifecycle of the fungus and disease management approaches are also summarized. Apple scab is an economically important disease that can significantly reduce apple yields. Proper fungicide application and use of resistant apple varieties are recommended for effective disease control.
Introduction to plant Systematics by sarah Ashfaq.pptxSarah Ashfaq 51
油
This document provides an introduction to plant systematics. It discusses how early botanists like Theophrastus and Pliny helped establish the field by classifying plant species. It also mentions how Charles Darwin influenced the field with his theory of evolution in Origin of Species. The document defines key terms like plant systematics, taxonomy, and plant taxonomy. It discusses how plants are classified based on characteristics like reproductive structures. It also covers identification of plants using features of leaves, flowers, fruits, and stems. The document mentions the International Code of Botanical Nomenclature which established the binomial naming system for formally naming plant species.
VERTEBRATES.pptx by Sarah Ashfaq botanist and mycologistSarah Ashfaq 51
油
Vertebrates originated during the Cambrian explosion around 518 million years ago and are defined as animals that have a vertebral column or backbone. There are five main groups of vertebrates: fish, amphibians, reptiles, birds, and mammals. Fish are cold-blooded and live exclusively in water, while amphibians undergo metamorphosis and spend part of their life in water and part on land, and the other groups are warm-blooded and breathe air.
ASCOMYCOTA SLIDE.pptx fungi university of the punjabSarah Ashfaq 51
油
The document summarizes key characteristics of Ascomycota fungi. It describes:
1) General characteristics including that they sexually produce spores called ascospores contained within an ascus sac.
2) Their diverse fruiting bodies including cleistothecia, perithecia, apothecia, gymnothecia, and pseudothecia.
3) Their asexual spores including arthroconidia, microconidia, proconidia, blastic conidia, and thallic conidia. Examples of each type are provided.
This document discusses smog, including its sources, types, effects, and measures to address it. Smog forms from the combination of smoke and fog from natural and human-caused sources like vehicle emissions and industrial pollution. It exists in two main types - Los Angeles photochemical smog formed by chemical reactions involving sunlight, and London reducing smog containing high sulfur dioxide. Smog harms human health, plants, and the environment through respiratory and cardiovascular impacts, reduced visibility, and acid rain. Addressing smog requires reducing emissions and taking precautions during smog episodes. Pakistan faces severe smog problems, with plans to install anti-smog technology in Lahore and other cities in 2023.
1. Antioxidant enzymes play an important role in stabilizing or deactivating free radicals before they can damage cellular components. They work by reducing the energy of free radicals or donating electrons to make them stable.
2. Some key antioxidant enzymes in plants include superoxide dismutase, catalase, ascorbate peroxidase, monodehydroascorbate reductase, dehydroascorbate reductase, and glutathione peroxidase. Glutathione reductase also helps maintain glutathione levels.
3. Antioxidant enzymes use different mechanisms to neutralize reactive oxygen species like hydrogen peroxide and superoxide, which are natural byproducts of cellular processes but can become harmful if
How to create security group category in Odoo 17Celine George
油
This slide will represent the creation of security group category in odoo 17. Security groups are essential for managing user access and permissions across different modules. Creating a security group category helps to organize related user groups and streamline permission settings within a specific module or functionality.
Unit 1 Computer Hardware for Educational Computing.pptxRomaSmart1
油
Computers have revolutionized various sectors, including education, by enhancing learning experiences and making information more accessible. This presentation, "Computer Hardware for Educational Computing," introduces the fundamental aspects of computers, including their definition, characteristics, classification, and significance in the educational domain. Understanding these concepts helps educators and students leverage technology for more effective learning.
How to Configure Proforma Invoice in Odoo 18 SalesCeline George
油
In this slide, well discuss on how to configure proforma invoice in Odoo 18 Sales module. A proforma invoice is a preliminary invoice that serves as a commercial document issued by a seller to a buyer.
Blind spots in AI and Formulation Science, IFPAC 2025.pdfAjaz Hussain
油
The intersection of AI and pharmaceutical formulation science highlights significant blind spotssystemic gaps in pharmaceutical development, regulatory oversight, quality assurance, and the ethical use of AIthat could jeopardize patient safety and undermine public trust. To move forward effectively, we must address these normalized blind spots, which may arise from outdated assumptions, errors, gaps in previous knowledge, and biases in language or regulatory inertia. This is essential to ensure that AI and formulation science are developed as tools for patient-centered and ethical healthcare.
How to Configure Deliver Content by Email in Odoo 18 SalesCeline George
油
In this slide, well discuss on how to configure proforma invoice in Odoo 18 Sales module. A proforma invoice is a preliminary invoice that serves as a commercial document issued by a seller to a buyer.
Effective Product Variant Management in Odoo 18Celine George
油
In this slide well discuss on the effective product variant management in Odoo 18. Odoo concentrates on managing product variations and offers a distinct area for doing so. Product variants provide unique characteristics like size and color to single products, which can be managed at the product template level for all attributes and variants or at the variant level for individual variants.
Hannah Borhan and Pietro Gagliardi OECD present 'From classroom to community ...EduSkills OECD
油
Hannah Borhan, Research Assistant, OECD Education and Skills Directorate and Pietro Gagliardi, Policy Analyst, OECD Public Governance Directorate present at the OECD webinar 'From classroom to community engagement: Promoting active citizenship among young people" on 25 February 2025. You can find the recording of the webinar on the website https://oecdedutoday.com/webinars/
2. DEFINITION
An organism inhibiting the soil during part or all of its life
is called as living inhabitants of soil.
Inhabitants : It means A person or animal that lives in a place.
3. LIVING ORGANISMS:
Living organisms present in soil include archaea , bacteria,
Actinomycetes, fungi, protozoa and a wide variety of larger
Soil fauna including springtails mites ,nematodes, earthworm,
ants and insects that spend all or part of their life underground
even larger organisms such as burrowing rodents.
4. IMPORTANCE OF SOIL ORGANISMS
Soil organisms, which range in size from microscopic cells that
digest decaying organic material to small mammals that live
primarily on other soil organisms, play an important role in
maintaining fertility, structure, drainage, and aeration of soil. They
also break down plant and animal tissues, releasing stored
nutrients and converting them into forms usable by plants. Some
soil organisms are pests. Among the soil organisms that are pests of
crops are nematodes, slugs and snails, beetles larvae, fly larvae,
caterpillars, and root aphids. Some soil organisms cause rots, some
release substances that inhibits plant growth, and others are hosts
for organisms that cause animal diseases.
5. DIVERSITY OF SOIL ORGANISMS
one square meter of rich soil can have as many as 1,000,000,000
organisms.
6. ARBITRARY GROUPS
Soil organisms are commonly divided into five arbitrary groups
according to size.
Protists Microfauna Mesofauna
Macrofauna Megafauna
7. Protists:
A protist is any eukaryotic organism that is not an animal, plant, or
fungus. While it is likely that protists share a common ancestor, the
exclusion of other eukaryotes means that protists do not form a
natural group, or clade.
EXAMPLES : Bacteria, actinomycetes and algae.
8. KINGDOM PROTISTA:
Protists include:
(1) protozoa, the animal-like protists,
(2) algae, the plant-like protists, and
(3) slime molds and water molds,
the fungus-like protists.
embibe.com
9. MICROFAUNA:
Microfauna, which are less than 100 microns in length and
generally feed upon other microorganisms. The microfauna include
single-celled protozoans, some smaller flatworms, nematodes,
rotifers, and tardigrades (eight-legged invertebrates).
11. MESOFAUNA:
The mesofauna are somewhat larger , including creatures that feed
on microorganisms, decaying matter, and living plants. The category
includes nematodes, mites, springtails (wingless insects so called for
the springing organ which enables them to leap), the insect like
proturans, which feed on fungi.
SIZE:
Soil mesofauna are invertebrates between 0.1mm and 2mm in size,
which live in the soil or in a leaf litter layer on the soil surface.
13. MACROFAUNA:
DEFINITION:
Soil Macrofauna, earthworms, termites, ants and some insect larvae,
can make the pore spaces and hence can change the soil porosity,
one aspect of soil morphology.
SIZE:
Some are centimeter or more long but smaller than an
earthworm.
15. MEGAFAUNA OF SOIL:
Megafauna are large animals that roamed the Earth during the
Pleistocene Epoch, 1.6 million - 10,000 years ago. ... In North
American, Megafauna included Giant Ground Sloths and Sabre-
toothed Tigers, and African Megafauna included elephants, giraffes,
rhinoceroses and hippopotamuses.
16. SOIL AND ITS INHABITANTS BY THE
NUMBERS:
1.Microfungi 2.Earthworms 3.Nematodes 4.Bacteria 5.Archaea
These plants like
cells related to
mushrooms can fill
between one-tenth
and three-tenth of
area around plant
roots.
Each has more than
7000 species of
these crawlers.
Around 100 to 500
squiggly earthworms
can live beneath 0.8
square meter.
These unsegmented
worms are around a
millimeter long.
Around 10 million
nematodes can live
beneath 0.8 square
meter of soil.
A teaspoon of
healthy soil can
contain between 100
million and 1 billion
of these microbes.
Up to one in every
10 microbes in most
soils may belong to
this family of
organisms.
17. AFFECT OF SOIL ORGANISM IN SOIL
Soil organisms fulfill key processes in the soil, such
as decomposition and nutrient mineralization. Many
microorganisms engage in mutualistic interactions with plant hosts,
aiding in the uptake of nutrients and water (e.g., arbuscular
mycorrhizal fungi, AMF), in exchange for photosynthates or other
plant metabolites.
19. ROLE OF MICROORGANISMS IN THE
SOIL AND CROP PRODUCTION:
Microorganisms in the topsoil are important, improving soil
productivity, cycling of nutrient compounds in the biosphere, and
sources of manufacturing products such as growth hormones,
enzymes, antibiotics, vitamins, etc.
20. EXTREMELY DIVERSE
Differences in morphological
traits between nine species of
soil invertebrates belonging to
three groups: earthworms,
ground beetles, and
springtails (Drawing
credits: www.lesbullesdemo.fr
).
21. BODY SIZE:
An important structural difference between earthworms, springtails,
and ground beetles, and between species within these groups, is
their body size. Size is an example of a morphological trait. The
smallest earthworm measures several cm long, while the largest,
found in tropical forests, can be 2 m long. In Europe, ground
beetles measure between 2 mm and 8 cm from the top of the head
to the last segment of the abdomen. Springtails are much smaller,
with an average body size of only 2 mm, but their size varies
depending on where they live. Some springtail species living in
dead leaves are bigger than other species that live deeper in the
soil.
22. MOVEMENT:
To find a habitat with enough food, other organisms with which to
reproduce, and a low number of predators, soil organisms have
developed numerous techniques for moving, both at the surface and
within the soil. Earthworms do not have legs, but some species have
strong muscles and small hairs that they use to burrow between soil
particles. With their six legs, ground beetles can run on the soil surface to
catch their prey. Many species of ground beetles have wings, allowing
them to rapidly escape from a predator or other disturbance, or to move
to a place where they can find more prey or mates. Springtails also move
on their six legs, but thanks to a special appendage that acts like a
spring, some springtails can jump several centimeters into the air to
escape predators.
23. SOIL ORGANISMS IN
ACTION:
Figure - Soil organisms in action.
(1) Earthworm living and feeding on dead
leaves. (2) Earthworm reaching the soil
surface through its large, deep burrow. (3)
Earthworms living in the soil and digging
many burrows. (4) Different springtail
species transforming dead leaves into
fecal pellets. (5) Springtail escaping from a
predator by jumping with its spring-like
appendage. (6) Ground beetle feeding on
a snail. (7) Ground beetle ready to fly
(Drawing credits: www.lesbullesdemo.fr).
24. COLOR:
Soil organisms can be colorful. Some earthworms that live in the few first
centimeters of soil, in the dead leaves, or in compost or manure are reddish-
brown, which enables them to camouflage from their predators against orange-
brown dead leaves, but which also protects them from UV light
Part of the suns rays that are invisible to the naked eye and can cause sunburn
Other earthworms live deeper in the soil and often have pale colors, such as pale
pink, gray, or green. In the dark soil, pigmentation is not necessary because UV
light does not penetrate. Still other earthworms live mostly in the soil, but they put
their heads out of the soil to feed on dead leaves; consequently, only their heads
are pigmented. Springtails show almost the same color patterns as earthworms:
pigmented species live on top of the soil and unpigmented ones live within the soil
. Finally, ground beetles can have many wonderful color patterns. The vivid colors
might discourage their bird predators or might help them to camouflage in their
environments.
25. Conclusion:
Soil organisms are incredibly diverse in shape and behavior. Soil
ecologists explore the wonderful world of the soil and have the chance to
discover new species and new traits. By looking at the characteristics of
the species they find, soil scientists can better understand the interactions
between organisms and ecosystems. Taken together, the numerous roles
played by the wide variety of soil organisms are complementary and
fundamental to maintaining healthy soils. It is thus very important for us to
maintain and conserve soil biodiversity, which is facing the increasing
impacts of human activities, such as intensive agriculture and climate
change. Raising public awareness of the importance of soil organisms
and improving our knowledge of soil biodiversity will be key to decreasing
our impacts on the amazing ecosystems under our feet.
26. .
Bottinelli, N., Hedde , M., Jouquet, P., and Capowiez, Y. 2020. An explicit definition of earthworm
ecological categoriesMarcel Bouch辿s triangle revisited. Geoderma 372:114361. doi:
10.1016/j.geoderma.2020.114361
Potapov, A. A., Semenina, E. E., Korotkevich, A. Yu., Kuznetsova, N. A., and Tiunov, A. V. 2016.
Connecting taxonomy and ecology: trophic niches of collembolans as related to taxonomic identity and
life forms. Soil Biol. Biochem. 101:2031. doi: 10.1016/j.soilbio.2016.07.002
Pey, B., Nahmani, J., Auclerc, A., Capowiez, Y., Cluzeau, D., Cortet, J., et al. 2014. Current use of and
future needs for soil invertebrate functional traits in community ecology. Basic Appl. Ecol. 15:194206.
doi: 10.1016/j.baae.2014.03.007
[ Capowiez, Y., Bottinelli, N., Sammartino, S., Michel, E., and Jouquet, P. 2015. Morphological and
functional characterisation of the burrow systems of six earthworm species (Lumbricidae). Biol. Fertil.
Soils 51:86977. doi: 10.1007/s00374-015-1036-x
REFERENCES: