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Illustrating the

Natural

World


1

Overview

Behavior among two or more organisms within

the same species, and encompasses any behavior in

which one member affects the other. Social behavior

can be seen as similar to an exchange of goods, with

the expectation that when you give, you will receive

the same. This behavior can be affected by both the

qualities of the individual and the environmental

(situational) factors. Therefore, social behavior arises

as a result of an interaction between the organism

and its environment.

A major aspect of social behavior is communication,

which is the basis for survival and reproduction.

Behavior can arise by those consciously behaving

(where there is an awareness and intent), or by pure

impulse. These factors that determine behavior can

work in different situations and moments, and can

even oppose one another. There are distinctions

between different types of social behavior, such as

mundane versus defensive social behavior. Mundane

social behavior is a result of interactions in day-to-day

life, and are behaviors learned as one is exposed

to those different situations. On the other hand,

defensive behavior arises out of impulse, when one is

faced with conflicting desires.

Development

The development of behavior is deeply tied with

the biological and cognitive changes one is experiencing

at any given time. Culture (parents and individuals

that influence socialization in children) play a large

role in the development of a child's social behavior, as

the parents or caregivers are typically those who

decide the settings and situations that the child is

exposed to. Emotions also play a large role in the

development of social behavior, as they are intertwined

with the way an individual behaves. Through social

interactions, emotion is understood through various

verbal and nonverbal displays, and thus plays a large

role in communication. The individual characteristics

of the child (their temperament) is important to

understanding how the individual learns social

behaviors and cues given to them, and this learnability

is not consistent across all children.

Organism

Social

Behavior

Overview

In biology, an organism (from Greek: ὀργανισμός,

organismos) is any individual entity that embodies the

properties of life. An organism may be defined as an

assembly of molecules functioning as a more or less

stable whole that exhibits the properties of life. Dictionary

definitions can be broad, using phrases such as

"any living structure, such as a plant, animal, fungus

or bacterium, capable of growth and reproduction.”

An organism may be either a prokaryote or a

eukaryote. Prokaryotes are represented by two

separate domains - bacteria and archaea. Eukaryotic

organisms are characterized by the presence of a

membrane-bound cell nucleus and contain additional

membrane-bound compartments called organelles.

Fungi, animals and plants are examples of kingdoms

of organisms within the eukaryotes. Estimates on the

number of Earth's current species range from two

million to one trillion, of which over 1.7 million

have been documented. More than 99% of all species,

amounting to over five billion species, that ever lived

are estimated to be extinct.

Structure

All organisms consist of structural units called

cells; some contain a single cell (unicellular) and

others contain many units (multicellular). Multicellular

organisms are able to specialize cells to perform specific

functions. A group of such cells is a tissue, and in

animals these occur as four basic types, namely epithelium,

nervous tissue, muscle tissue, and connective tissue.

Several types of tissue work together in the form of

an organ to produce a particular function. This pattern

continues to a higher level with several organs functioning

as an organ system such as the reproductive

system, and digestive system. Many multicellular

organisms consist of several organ systems, which

coordinate to allow for life.

2



Sandstone

Overview

Opal is a hydrated amorphous form of silica

(SiO2·nH2O); its water content may range from three

to 21% by weight, but is usually between six and

10%. Because of its amorphous character, it is classed

as a mineraloid, unlike crystalline forms of silica, which

are classed as minerals. It is deposited at a relatively

low temperature and may occur in the fissures of

almost any kind of rock, being most commonly

found with limonite, sandstone, rhyolite, marl, and

basalt. There are two broad classes of opal: precious

and common. Precious opal displays play-of-color,

common opal does not.

The internal structure of precious opal causes it to

diffract light, resulting in play-of-color. Depending

on the conditions in which it formed, opal may be

transparent, translucent, or opaque and the background

color may be white, black, or nearly any color

of the visual spectrum. Black opal is considered to

be the rarest, whereas white, gray, and green are the

most common.

4

Types

Precious opal shows a variable interplay of internal

colors, and though it is a mineraloid, it has an internal

structure. At microscopic scales, precious opal is

composed of silica spheres some 150 to 300 nm in

diameter in a hexagonal or cubic close-packed lattice.

Visible light cannot pass through large thicknesses of

the opal. This is the basis of the optical band gap in a

photonic crystal. For gemstone use, most opal is cut

and polished to form a cabochon. "Solid" opal refers

to polished stones consisting wholly of precious opal.

Opals too thin to produce a "solid" may be combined

with other materials to form attractive gems.

Common opal include the milk opal, milky bluish

to greenish (which can sometimes be of gemstone

quality); resin opal, which is honey-yellow with a

resinous luster; wood opal, which is caused by the

replacement of the organic material in wood with opal.

Other types are menilite, which is brown or grey;

hyalite, a colorless glass-clear opal sometimes called

Muller's glass; geyserite, also called siliceous sinter,

deposited around hot springs or geysers. Common

opal often displays a hazy-milky-turbid sheen from

within the stone.

Overview

Sandstone is a clastic sedimentary rock composed

mainly of sand-sized (0.0625 to two mm) silicate grains.

Sandstones make up about 20 to 25 percent of all

sedimentary rocks. Most sandstone is composed of

quartz or feldspar because they are the most resistant

minerals to weathering processes at the Earth's surface.

Like uncemented sand, sandstone may be any color

due to impurities within the minerals, but the most

common colors are tan, brown, yellow, red, grey,

pink, white, and black.

Sandstones are clastic in origin. The silicate sand

grains from which they form are the product of

physical and chemical weathering of bedrock.

As sediments continue to accumulate in the

depositional environment, older sand is buried by

younger sediments, and it undergoes diagenesis.

This mostly consists of compaction and lithification

of the sand. Early stages of diagenesis, take place at

shallow depths. The red hematite that gives red bed

sandstones their color is likely formed during this

process. Compaction takes place as the sand comes

under increasing pressure from overlying sediments.

Points of contact between grains are under the greatest

strain, and the strained mineral is more soluble than

the rest of the grain. As a result, the contact points

are dissolved away, allowing the grains to come into

closer contact.

Uses

Sandstone has been used since prehistoric times

for construction, decorative art works and housewares,

and continues to be used. It has been widely

employed around the world in constructing temples,

homes, and other buildings. Although its resistance

to weathering varies, sandstone is easy to work. That

makes it a common building and paving material,

including in asphalt concrete. However, some types

that have been used in the past, such as the Collyhurst

sandstone used in North West England, have had

poor long-term weather resistance, necessitating

repair and replacement in older buildings. Because

of the hardness of individual grains, uniformity of

grain size and friability of their structure, some types

of sandstone are excellent materials from which to

make grindstones, for sharpening blades and other

implements. Non-friable sandstone can be used

to make grindstones for grinding grain. A type of

pure quartz sandstone, orthoquartzite, with more

of 90–95 percent of quartz, has been proposed for

nomination to the Global Heritage Stone Resource.

In some regions of Argentina, the orthoquartzitestoned

facade is one of the main features of the

Mar del Plata style bungalows.

3

Opal



5

Overview

Maratus is a spider genus of the family Salticidae

(jumping spiders). These spiders are commonly

referred to as peacock spiders due to the males’

colorful and usually iridescent patterns on the upper

surface of the abdomen often enhanced with lateral

flaps or bristles, which they display during courtship.

Females lack these bright colors, being cryptic in

appearance. In at least one species, Maratus vespertilio,

the expansion of the flaps also occurs during ritualised

contests between males. The male display and courtship

dance are complex, involving visual and vibratory signals.

Maratus species are small spiders, with a total body

length mostly around 4-5 mm (0.2 in), sometimes

smaller, with a high degree of sexual dimorphism.

Not all species have colors that appear bright to human

vision; Maratus vespertilio is relatively cryptically

colored, with most iridescence on the lateral flaps.

The abdominal display is used in courtship and, in at

least one species, also in aggressive interactions with

rival males.

Taxonomy

The genus Maratus was first described by

Ferdinand Karsch in 1878. Karsch was a curator at

the Museum für Naturkunde, Berlin, and named

spiders and other animals from preserved specimens

collected by others. He described the species Maratus

amabilis, the type of his new genus, on the basis

of a single male specimen, whose origin was only

recorded as "Australia". All species of Maratus are

found in Australia, with the exception of Maratus

furvus from China. M. furvus was first described in

1992 in the genus Lycidas, becoming part of Maratus

when Lycidas was synonymized in 2012. His short

description mentioned the abdomen being flattened

and quadrangular in shape, but otherwise did not refer

to the characteristic abdominal "flaps.” One molecular

phylogenetic study, by Junxia Zhang in 2012, concluded

that the seven Australian genera Hypoblemum,

Jotus, Lycidas, Maileus, Maratus, Saitis and Prostheclina

were so closely related that they could all be accommodated

in Saitis but this suggestion has not been

carried through to any taxonomic publication.

Crypsis

Peacock Spider

Overview

In ecology, crypsis is the ability of an animal to

avoid observation or detection by other animals.

It may be a predation strategy or an antipredator

adaptation. Methods include camouflage, nocturnality,

subterranean lifestyle and mimicry. Crypsis can

involve visual, olfactory (with pheromones), or

auditory concealment. When it is visual, the term

cryptic coloration, effectively a synonym for animal

camouflage, is sometimes used, but many different

methods of camouflage are employed by animals.

There is a strong evolutionary pressure for animals to

blend into their environment or conceal their shape,

for prey animals to avoid predators and for predators

to be able to avoid detection by prey. Cryptic animals

include the tawny frogmouth (feather patterning

resembles bark), the tuatara (hides in burrows all day;

nocturnal), some jellyfish (transparent), the leafy sea

dragon, and the flounder (covers itself in sediment).

Methods

This first method is visually, Many animals have

evolved so that they visually resemble their surroundings

by using any of the many methods of natural

camouflage that may match the color and texture of

the surroundings and/or break up the visual outline

of the animal itself. Such animals may resemble rocks,

sand, twigs, leaves, and even bird droppings. Other

methods including transparency and silvering are

widely used by marine animals. Next is olfactory.

Some animals, in both terrestrial and aquatic environments,

appear to camouflage their odor, which might

otherwise attract predators. Numerous arthropods,

both insects and spiders, mimic ants, whether to

avoid predation, to hunt ants, or to trick the ants

into feeding them. Lastly is auditory crypsis, some

insects were originally theorized to defend themselves

against predation by echolocating bats, both by

passively absorbing sound with soft, fur-like body

coverings and by actively creating sounds to mimic

echoes from other locations or objects.

6



8

Overview

Paleontology is the scientific study of life that existed

prior to, and sometimes including, the start of the

Holocene Epoch (roughly 11,700 years before

present). It includes the study of fossils to classify

organisms and study interactions with each other

and their environments. Paleontological observations

have been documented as far back as the 5th century

BCE. It lies on the border between biology and geology,

but differs from archaeology in that it excludes the

study of anatomically modern humans. It now uses

techniques drawn from a wide range of sciences,

including biochemistry, mathematics, and engineering.

Body fossils and trace fossils are the principal types

of evidence about ancient life, and geochemical

evidence has helped to decipher the evolution of life

before there were organisms large enough to leave

body fossils.

Subdivisions

As knowledge has increased, paleontology has

developed specialised subdivisions. Vertebrate

paleontology concentrates on fossils from the

earliest fish to the immediate ancestors of modern

mammals. Invertebrate paleontology deals with

fossils such as molluscs, arthropods, annelid worms

and echinoderms. Paleobotany studies fossil plants,

algae, and fungi. Palynology, the study of pollen and

spores produced by land plants and protists, straddles

paleontology and botany, as it deals with both living

and fossil organisms. Micropaleontology deals with

microscopic fossil organisms of all kinds. Paleoecology

examines the interactions between different ancient

organisms, such as their food chains, and the two-way

interactions with their environments.

Tuatara

Overview

Tuatara are reptiles endemic to New Zealand.

Although resembling most lizards, they are part of

a distinct lineage, the order Rhynchocephalia. The

single species of tuatara is the sole surviving member

of its order, hich originated in the Triassic period

around 250 million years ago and which flourished

during the Mesozoic era. Tuatara are greenish brown

and grey, and measure up to 80 cm (31 in) from

head to tail-tip and weigh up to 1.3 kg (2.9 lb) with

a spiny crest along the back, especially pronounced

in males. They have two rows of teeth in the upper

jaw overlapping one row on the lower jaw, which is

unique among living species. They are also unusual

in having a pronounced photoreceptive eye, the

third eye, which is thought to be involved in setting

circadian and seasonal cycles.

Taxonomy

Tuatara, along with other now-extinct members

of the order Sphenodontia, belong to the superorder

Lepidosauria, the only surviving taxon within

Lepidosauromorpha. Squamates and tuatara both

show caudal autotomy (loss of the tail-tip when

threatened), and have transverse cloacal slits. The

origin of the tuatara probably lies close to the split

between the Lepidosauromorpha and the Archosauromorpha.

Though tuatara resemble lizards, the

similarity is superficial, because the family has several

characteristics unique among reptiles. The typical

lizard shape is very common for the early amniotes;

the oldest known fossil of a reptile, the Hylonomus,

resembles a modern lizard. While there is currently

considered to be only one living species of tuatara,

two species were previously identified: Sphenodon

punctatus and the much rarer Sphenodon guntheri.

Paleontology

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9

Overview

Botany is the science of plant life and a branch of

biology. The term "botany" comes from the Ancient

Greek word βοτάνη (botanē) meaning "pasture,"

"grass," or "fodder.” Traditionally, botany has also

included the study of fungi and algae by mycologists

and phycologists respectively. Today, botanists study

approximately 410,000 species of land plants. Botany

originated in prehistory as herbalism with the efforts

of early humans to identify - and later cultivate - edible,

medicinal and poisonous plants, making it one of

the oldest branches of science. In the 19th and 20th

centuries, new techniques were developed for the

study of plants, including methods of optical microscopy

and live cell imaging, electron microscopy, etc.

Modern botany is a broad, multidisciplinary

subject with inputs from most other areas of

science and technology.

Importance

The study of plants is vital because they underpin

almost all animal life on Earth by generating a large

proportion of the oxygen and food that provide

humans and other organisms with aerobic respiration

with the chemical energy they need to exist. Plants

are crucial to the future of human society as they

provide food, oxygen, medicine, and products for

people, as well as creating and preserving soil. Botanists

examine both the internal functions and processes

within plant organelles, cells, tissues, whole plants,

plant populations and plant communities. Virtually

all staple foods come either directly from primary

production by plants, or indirectly from animals that

eat them.Plants and other photosynthetic organisms

are at the base of most food chains because they use

the energy from the sun and nutrients from the soil

and atmosphere, converting them into a form that

can be used by animals. Botanists study how plants

produce food and how to increase yields.

Caffeine

Botany

Overview

Caffeine is a central nervous system (CNS) stimulant

of the methylxanthine class. It is the world's most widely

consumed psychoactive drug. Unlike many other

psychoactive substances, it is legal and unregulated

in nearly all parts of the world. There are several

known mechanisms of action to explain the effects

of caffeine. The most prominent is that it reversibly

blocks the action of adenosine on its receptors and

consequently prevents the onset of drowsiness induced

by adenosine. Caffeine also stimulates certain portions

of the autonomic nervous system. Caffeine is found

in the seeds, nuts, or leaves of a number of plants

native to Africa, East Asia and South America, and

helps to protect them against predator insects and to

prevent germination of nearby seeds. The most

well-known source of caffeine is the coffee bean.

People may drink beverages containing caffeine to

relieve or prevent drowsiness and to improve

cognitive performance.

Natural Occurance

Around thirty plant species are known to contain

caffeine. Common sources are the “beans” (seeds) of

the two cultivated coffee plants, Coffea arabica and

Coffea canephora. Along with the cocoa plant,

Theobroma cacao; the leaves of the tea plant; and

kola nuts. Caffeine in plants acts as a natural pesticide:

it can paralyze and kill predator insects feeding on

the plant. High caffeine levels are found in coffee

seedlings when they are developing foliage and lack

mechanical protection. Caffeine is stored in tea leaves

in two places. Firstly, in the cell vacuoles where it is

complexed with polyphenols. This caffeine probably

is released into the mouths of insects, to discourage

herbivory. Secondly, around the vascular bundles,

where it probably inhibits pathogenic fungi from

entering and colonizing the vascular bundles. Caffeine

in nectar may improve the reproductive success of

the pollen producing plants by enhancing the reward

memory of pollinators such as honey bees.

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Yaupon Holly

Overview

Ilex vomitoria, commonly known as yaupon or

yaupon holly, is a species of holly that is native to

southeastern North America. The word yaupon

was derived from the Catawban yąpą, from yą- tree

and pą leaf. The plant was traditionally used by

Native Americans to make an infusion containing

caffeine. It is among a very few plants endemic to

North America that produce caffeine. The plant is

also widely used for landscaping in its native range.

Yaupon holly is an evergreen shrub or small tree

reaching 5–9 m tall, with smooth, light gray bark and

slender, hairy shoots. The leaf arrangement is alternate,

with leaves ovate to elliptical and a rounded apex with

crenate or coarsely serrated margin that’s glossy dark

green above, slightly paler below. The flowers are

5–5.5 mm diameter, with a white four-lobed corolla.

The fruit is a small round, shiny, and red drupe.

Uses

Native Americans brewed the leaves and stems to

brew a tisane, commonly thought to be called asi or

black drink for male-only purification and unity rituals.

The ceremony included vomiting, and Europeans

deduced that yaupon caused it. Native Americans

may have also used the infusion as a laxative. Ilex

vomitoria is also a common landscape plant in the

Southeastern United States. The most common

cultivars are slow-growing shrubs popular for their

dense, evergreen foliage and their adaptability to

pruning into hedges of various shapes.

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