Mesozoic era climate conditions. Jurassic period Mesozoic era

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general information

The Mesozoic era lasted approximately 160 million years.

years. It is usually divided into three periods: Triassic, Jurassic and Cretaceous; The first two periods were much shorter than the third, which lasted 71 million.

Biologically, the Mesozoic was a time of transition from old, primitive to new, progressive forms. Neither four-rayed corals (rugosas), nor trilobites, nor graptolites crossed the invisible border that lay between the Paleozoic and Mesozoic.

The Mesozoic world was much more diverse than the Paleozoic; the fauna and flora appeared in it in a significantly updated composition.

2. Triassic period

Periodization: from 248 to 213 million years ago.

The Triassic period in the history of the Earth marked the beginning Mesozoic era, or the era of "middle life". Before him, all the continents were merged into a single giant supercontinent, Panagea. With the onset of the Triassic, Pangea again began to split into Gondwana and Laurasia, and the Atlantic Ocean began to form.

Sea levels around the world were very low. The climate, almost everywhere warm, gradually became drier, and vast deserts formed in inland areas. Shallow seas and lakes evaporated intensely, causing the water in them to become very salty.

Animal world.

Dinosaurs and other reptiles became the dominant group of land animals. The first frogs appeared, and a little later land and sea turtles and crocodiles. The first mammals also appeared, and the diversity of mollusks increased.

New species of corals, shrimp and lobsters formed. By the end of the period, almost all ammonites became extinct. Marine reptiles, such as ichthyosaurs, established themselves in the oceans, and pterosaurs began to explore air environment.

The largest aromorphoses: the appearance of a four-chambered heart, complete separation of arterial and venous blood, warm-bloodedness, mammary glands.

Vegetable world.

Below was a carpet of club mosses and horsetails, as well as palm-shaped bennettites.

Fauna and flora in the Mesozoic. Development of life in the Triassic, Jurassic and Cretaceous periods

Jurassic period

Periodization: from 213 to 144 million years ago.

By the beginning of the Jurassic period, the giant supercontinent Pangea was in the process of active disintegration. There was still a single vast continent south of the equator, which was again called Gondwana. Subsequently, it also split into parts that formed today's Australia, India, Africa and South America.

The sea flooded a significant part of the land. Intensive mountain building took place. At the beginning of the period, the climate was warm and dry everywhere, then it became more humid.

Land animals northern hemisphere could no longer move freely from one continent to another, but they still spread unhindered throughout the southern supercontinent.

Animal world.

The number and diversity of sea turtles and crocodiles increased, and new species of plesiosaurs and ichthyosaurs appeared.

The land was dominated by insects, the predecessors of modern flies, wasps, earwigs, ants and bees. The first bird, Archeopteryx, also appeared. Dinosaurs reigned supreme, evolving into many forms: from giant sauropods to smaller, fleet-footed predators

Vegetable world.

The climate became more humid, and all the land was overgrown with abundant vegetation. The predecessors of today's cypresses, pines and mammoth trees appeared in the forests.

The largest aromorphoses have not been identified.

Cretaceous period

Mesozoic biological Triassic Jurassic

Periodization: from 144 to 65 million years ago.

During Cretaceous period The “great split” of continents continued on our planet. The huge land masses that formed Laurasia and Gondwana gradually fell apart. South America and Africa moved away from each other, and the Atlantic Ocean became wider and wider. Africa, India and Australia also began to diverge different sides, and giant islands eventually formed south of the equator.

Most of the territory of modern Europe was then under water.

The sea flooded vast areas of land.

The remains of hard-covered planktonic organisms formed huge layers of chalk sediments on the ocean floor. At first the climate was warm and humid, but then it became noticeably colder.

Animal world.

The number of belemnites in the seas has increased.

The oceans were dominated by giant sea turtles and predatory marine reptiles. Snakes appeared on land, in addition, new varieties of dinosaurs appeared, as well as insects such as moths and butterflies. At the end of the period, another mass extinction led to the disappearance of ammonites, ichthyosaurs and many other groups of marine animals, and on land all dinosaurs and pterosaurs became extinct.

The largest aromorphosis is the appearance of the uterus and intrauterine development of the fetus.

Vegetable world.

The first flowering plants appeared, establishing close “cooperation” with insects that carried their pollen.

They began to quickly spread throughout the land.

The largest aromorphosis is the formation of a flower and fruit.

5. Results of the Mesozoic era

The Mesozoic era is the era of middle life. It is named so because the flora and fauna of this era are transitional between Paleozoic and Cenozoic. During the Mesozoic era, the modern outlines of continents and oceans, modern marine fauna and flora gradually formed.

The Andes and Cordillera, the mountain ranges of China and East Asia, were formed. The depressions of the Atlantic and Indian oceans were formed. The formation of the Pacific Ocean depressions began. Serious aromorphoses also occurred in the plant and animal worlds. Gymnosperms become the predominant division of plants, and in the animal world the appearance of a four-chambered heart and the formation of the uterus are of equal importance.

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Mesozoic era

The beginning of the Mesozoic era as a transitional period in development earth's crust and life.

Significant restructuring of the structural plan of the Earth. Triassic, Jurassic and Cretaceous periods of the Mesozoic era, their description and characteristics (climate, animal and plant worlds).

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Cretaceous period

Geological structure of the planet during the Cretaceous period. Tectonic changes during the Mesozoic stage of development.

Reasons for the extinction of dinosaurs. The Cretaceous period is the last period of the Mesozoic era. Characteristics of vegetation and animals, their aromorphoses.

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Silurian period of the Paleozoic era

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Mesozoic era

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Mesozoic era

The Mesozoic era (252-66 million years ago) is the second era of the fourth eon - Phanerozoic. Its duration is 186 million years. The main features of the Mesozoic: the modern outlines of continents and oceans, modern marine fauna and flora are gradually formed. The Andes and Cordillera, the mountain ranges of China and East Asia, were formed. The depressions of the Atlantic and Indian oceans were formed. The formation of the Pacific Ocean depressions began.

Periods of the Mesozoic era

Triassic period, Triassic, - the first period of the Mesozoic era, lasts 51 million years.

This is the time of formation of the Atlantic Ocean. The single continent of Pangea again begins to break into two parts - Gondwana and Laurasia. Inland continental reservoirs are beginning to actively dry up. The depressions left from them are gradually filled with rock deposits.

New mountain heights and volcanoes are appearing and exhibiting increased activity. A huge part of the land is still occupied by desert zones with weather conditions unsuitable for the life of most species of living beings. The salt level in water bodies is rising. During this time period, representatives of birds, mammals and dinosaurs appear on the planet. Read in detail - Triassic period.

Jurassic period (Jura)- the most famous period of the Mesozoic era.

It received its name due to the sedimentary deposits of that time found in the Jura (mountain ranges of Europe). The average period of the Mesozoic era lasts about 56 million years. The formation of modern continents begins - Africa, America, Antarctica, Australia. But they are not yet located in the order to which we are accustomed.

Deep bays and small seas appear, separating the continents. Active formation of mountain ranges continues. The Arctic Sea floods the north of Laurasia. As a result, the climate is moistened, and vegetation forms in place of deserts.

Cretaceous period (Cretaceous)- the final period of the Mesozoic era, occupies a time period of 79 million years. Appear angiosperms. As a result of this, the evolution of fauna representatives begins. The movement of continents continues - Africa, America, India and Australia are moving away from each other. The continents of Laurasia and Gondwana begin to break up into continental blocks. Huge islands are forming in the south of the planet.

The Atlantic Ocean is expanding. The Cretaceous period is the time when flora and fauna flourished on land. Due to the evolution of the plant world, fewer minerals enter the seas and oceans. The amount of algae and bacteria in water bodies decreases. Read in detail - Cretaceous period

Climate of the Mesozoic era

At the very beginning, the climate of the Mesozoic era was the same throughout the entire planet. The air temperature at the equator and poles remained at the same level.

At the end of the first period of the Mesozoic era, drought reigned on Earth for most of the year, which was briefly replaced by rainy seasons. But, despite the dry conditions, the climate became significantly colder than it was during the Paleozoic period.

Some species of reptiles have completely adapted to cold weather. From these species of animals mammals and birds would later develop.

During the Cretaceous period it becomes even colder. All continents have their own climate. Tree-like plants appear, which lose their foliage during the cold season. Snow begins to fall at the North Pole.

Plants of the Mesozoic era

At the beginning of the Mesozoic, the continents were dominated by lycophytes, various ferns, the ancestors of modern palms, conifers and ginkgo trees.

In the seas and oceans, the dominance belonged to algae that formed reefs.

The increased humidity of the climate of the Jurassic period led to the rapid formation of plant matter on the planet. The forests consisted of ferns, conifers and cycads. Thujas and araucarias grew near the ponds. In the middle of the Mesozoic era, two vegetation belts formed:

1. Northern, which was dominated by herbaceous ferns and gingkovic trees;
2. Southern.

   Tree ferns and cycads reigned here.

In the modern world, ferns, cycads (palm trees reaching 18 meters in size) and cordaites of that time can be found in tropical and subtropical forests.

Horsetails, mosses, cypresses and spruce trees had practically no differences from those that are common in our time.

The Cretaceous period is characterized by the appearance of plants with flowers. In this regard, butterflies and bees appeared among insects, thanks to which flowering plants were able to quickly spread throughout the planet.

Also at this time, ginkgo trees with leaves that fall off during the cold season begin to grow. Coniferous forests of this time period are very similar to modern ones.

These include yews, firs and cypresses.

The development of higher gymnosperms lasts throughout the Mesozoic era. These representatives of the earth's flora got their name due to the fact that their seeds did not have an outer protective shell. Most widespread received cycads and bennettites.

In appearance, cicadas resemble tree ferns or cycads. They have straight stems and massive leaves that look like feathers. Bennettites are trees or shrubs. They are similar in appearance to cicadas, but their seeds are covered with a shell. This brings the plants closer to angiosperms.

Angiosperms appeared in the Cretaceous period. From this moment a new stage in the development of plant life begins. Angiosperms (flowering plants) are at the top rung of the evolutionary ladder.

They have special reproductive organs - stamens and pistil, which are located in the flower cup. Their seeds, unlike gymnosperms, are hidden by a dense protective shell. These plants of the Mesozoic era quickly adapt to any climatic conditions and actively develop. Behind short term Angiosperms began to dominate the entire Earth. Their various types and forms have reached modern world– eucalyptus, magnolia, quince, oleander, walnut trees, oak, birch, willow and beech trees.

Of the gymnosperms of the Mesozoic era, we are now familiar only with coniferous species - fir, pine, sequoia and some others. The evolution of plant life of that period significantly outstripped the development of representatives of the animal world.

Animals of the Mesozoic era

Animals actively evolved during the Triassic period of the Mesozoic era.

A huge variety of more developed creatures formed, which gradually replaced the ancient species.

One of these types of reptiles was the animal-like pelycosaurs - sailing lizards.

On their backs there was a huge sail, like a fan. They were replaced by therapsids, which were divided into 2 groups - predators and herbivores.

Their legs were powerful and their tails were short. Therapsids were much superior to pelycosaurs in speed and endurance, but this did not save their species from extinction at the end of the Mesozoic era.

The evolutionary group of lizards from which mammals would later evolve are the cynodonts (dog teeth). These animals got their name due to their powerful jaw bones and sharp teeth, with which they could easily chew raw meat.

Their bodies were covered with thick hair. The females laid eggs, but the newborn cubs fed on their mother's milk.

At the beginning of the Mesozoic era, a new species of lizards emerged - archosaurs (ruling reptiles).

They are the ancestors of all dinosaurs, pterosaurs, plesiosaurs, ichthyosaurs, placodonts and crocodylomorphs. Archosaurs, adapted to the climatic conditions on the coast, became predatory thecodonts.

They hunted on land near bodies of water. Most thecodonts walked on four legs. But there were also individuals that ran on their hind legs. In this way, these animals developed incredible speed. After some time, thecodonts evolved into dinosaurs.

By the end of the Triassic period, two species of reptiles predominated. Some are the ancestors of the crocodiles of our time.

Others turned into dinosaurs.

Dinosaurs have a body structure that is not similar to other lizards. Their paws are located under the body.

This feature allowed dinosaurs to move quickly. Their skin is covered with waterproof scales. Lizards move on 2 or 4 legs, depending on the species. The first representatives were fast coelophysis, powerful herrerasaurs and huge plateosaurs.

Besides dinosaurs, archosaurs gave rise to another species of reptile that was different from the rest.

These are pterosaurs - the first lizards that can fly. They lived near bodies of water and ate various insects for food.

Animal world depths of the sea The Mesozoic era is also characterized by a variety of species - ammonites, bivalves, families of sharks, bony and ray-finned fish. The most prominent predators were the underwater lizards that appeared not so long ago. Dolphin-like ichthyosaurs had high speed.

One of the giant representatives of ichthyosaurs is Shonisaurus. Its length reached 23 meters, and its weight did not exceed 40 tons.

Lizard-like nothosaurs had sharp fangs.

Placadonts, similar to modern newts, searched for mollusk shells on the seabed, which they bit with their teeth. Tanystrophei lived on land. Long (2-3 times the body size), slender necks allowed them to catch fish while standing on the shore.

Another group of sea lizards of the Triassic period are plesiosaurs. At the beginning of the era, plesiosaurs reached a size of only 2 meters, and by the middle of the Mesozoic they evolved into giants.

The Jurassic period is the time of the development of dinosaurs.

The evolution of plant life gave impetus to the emergence different types herbivorous dinosaurs. And this, in turn, led to an increase in the number of predatory individuals. Some dinosaur species were the size of cats, while others were as large as giant whales. The most giant individuals are diplodocus and brachiosaurs, reaching a length of 30 meters.

Their weight was about 50 tons.

Archeopteryx is the first creature standing on the border between lizards and birds. Archeopteryxes were not yet able to fly long distances. The beak was replaced by jaws with sharp teeth. The wings ended in fingers. Archeopteryx was the size of modern crows.

They lived mainly in forests and ate insects and various seeds.

In the middle of the Mesozoic era, pterosaurs were divided into 2 groups - pterodactyls and rhamphorhynchus.

Pterodactyls lacked a tail and feathers. But there were large wings and a narrow skull with few teeth. These creatures lived in flocks on the coast. During the day they obtained food for themselves, and at night they hid in the trees. Pterodactyls ate fish, shellfish and insects. This group of pterosaurs had to jump from high places to take to the skies. Rhamphorhynchus also lived on the coast. They ate fish and insects. They had long tails with a blade at the end, narrow wings and a massive skull with teeth of different sizes, which were convenient for catching slippery fish.

The most dangerous predator the depths of the sea was Liopleurodon, weighing 25 tons.

Huge coral reefs were formed, in which ammonites, belemnites, sponges and sea mats settled. Representatives of the shark family and bony fishes are developing. New species of plesiosaurs and ichthyosaurs, sea turtles and crocodiles appeared. Saltwater crocodiles developed flippers instead of legs. This feature allowed them to increase speed in the aquatic environment.

During the Cretaceous period of the Mesozoic era, bees and butterflies appeared. Insects carried pollen, and flowers gave them food.

Thus began a long-term collaboration between insects and plants.

The most famous dinosaurs of the time were the predatory tyrannosaurs and tarbosaurs, the herbivorous bipedal iguanodons, the four-legged rhinoceros-like Triceratops, and the small armored ankylosaurs.

Most mammals of that period belong to the subclass Allotheria.

These are small animals, similar to mice, weighing no more than 0.5 kg. The only exceptional species is the repenomama. They grew up to 1 meter and weighed 14 kg. At the end of the Mesozoic era, the evolution of mammals occurs - the ancestors of modern animals separate from allotheria. They are divided into 3 species - oviparous, marsupial and placental. It is they who replace the dinosaurs at the beginning of the next era. Rodents and primates emerged from the placental species of mammals. Purgatorius became the first primates.

From marsupial species modern opossums evolved, and egg-laying ones gave rise to platypuses.

The airspace is dominated by early pterodactyls and new species of flying reptiles - Orcheopteryx and Quetzatcoatli. These were the most gigantic flying creatures in the entire history of the development of our planet.

Together with representatives of pterosaurs, birds dominate the air. During the Cretaceous period, many ancestors of modern birds appeared - ducks, geese, loons. The length of the birds was 4-150 cm, weight - from 20 grams. up to several kilograms.

The seas were dominated by huge predators reaching 20 meters in length - ichthyosaurs, plesiosaurs and mososaurs. Plesiosaurs had very long neck and a small head.

Their large size did not allow them to develop high speed. The animals ate fish and shellfish. Mososaurs replaced saltwater crocodiles. These are giant predatory lizards with an aggressive character.

At the end of the Mesozoic era, snakes and lizards appeared, the species of which have reached the modern world unchanged. The turtles of this time period were also no different from those we see now.

Their weight reached 2 tons, length - from 20 cm to 4 meters.

By the end of the Cretaceous period, most reptiles began to die out en masse.

Minerals of the Mesozoic era

A large number of natural resource deposits are associated with the Mesozoic era.

These are sulfur, phosphorites, polymetals, construction and combustible materials, oil and natural gas.

In Asia, due to active volcanic processes, the Pacific belt was formed, which gave the world large deposits of gold, lead, zinc, tin, arsenic and other types of rare metals. In terms of coal reserves, the Mesozoic era is significantly inferior to the Paleozoic era, but even during this period several large deposits of brown and hard coal were formed - the Kansky basin, Bureinsky, Lensky.

Mesozoic oil and gas fields are located in the Urals, Siberia, Yakutia, and the Sahara.

Phosphorite deposits have been found in the Volga region and Moscow region.

To the table: Phanerozoic eon

01 of 04. Periods of the Mesozoic era

The Paleozoic era, like all major eras on a geological time scale, ended with a mass extinction. The Permian mass extinction is considered the largest loss of species in Earth's history. Almost 96% of all living species were wiped out due to the large number of volcanic eruptions that led to massive and relatively rapid climate change during the Mesozoic era.

The Mesozoic Era is often called the "Age of the Dinosaurs" because it is the time period in which dinosaurs evolved and eventually went extinct.

The Mesozoic era is divided into three periods: Triassic, Jurassic and Cretaceous.

02 of 04. Triassic period (251 million years ago - 200 million years ago)

Fossil of Pseudopalatus from the Triassic period.

National Park Service

The beginning of the Triassic period was quite sparse in terms of life forms on Earth. Because there were so few species left after the Permian mass extinction, it took a very long time for recolonization and increased biodiversity. The Earth's topography also changed during this time period. At the beginning of the Mesozoic era, all continents were connected into one large continent. This supercontinent was named Pangea.

During the Triassic period, continents began to separate due to plate tectonics and continental drift.

As animals began to emerge from the oceans again and colonize nearly empty land, they also learned to dig burrows to protect themselves from the changes. environment. For the first time in history, amphibians such as frogs appeared, followed by reptiles such as turtles, crocodiles, and eventually dinosaurs.

By the end of the Triassic period, birds also appeared, splitting off from the dinosaur branch of the phylogenetic tree.

Plants were also few in number. In the Triassic period they began to flourish again.

Development of life in the Mesozoic era

Most land plants at that time were conifers or ferns. By the end of the Triassic period, some of the ferns had developed seeds for reproduction. Unfortunately, another mass extinction brought an end to the Triassic period. This time, about 65% of the species on Earth did not survive.

03 of 04. Jurassic period (200 million years ago - 145 million years ago)

Plesiosaur from the Jurassic period.

Tim Evanson

After the Triassic mass extinction, life and species diversified to fill niches that were left open. Pangea broke into two large parts - Laurasia was a land mass in the north, and Gondwana was in the south. Between these two new continents was the Tethys Sea. Diverse climates on each continent allowed many new species to emerge for the first time, including lizards and small mammals. However, dinosaurs and flying reptiles continued to dominate the earth and skies.

There were a lot of fish in the oceans.

Plants bloomed on earth for the first time. There were numerous extensive pastures for herbivores, which also provided food for predators. The Jurassic period was like a Renaissance era for life on Earth.

04 of 04. Cretaceous period (145 million years ago - 65 million years ago)

Fossil Pachycephalosaurus from the Cretaceous period.

Tim Evanson

The Cretaceous period is the last period of the Mesozoic era. Favorable conditions for life on Earth continued from the Jurassic period to the early Cretaceous period. Laurasia and Gondwana began to expand even further, eventually forming the seven continents we see today. As landmass expanded, Earth's climate became warm and humid. These were very favorable conditions for plant life to flourish. Flowering plants began to proliferate and dominate the land.

As plant life was abundant, the population of herbivores also increased, which in turn led to an increase in the number and size of predators. Mammals also began to split into many species, just as dinosaurs did.

Life in the ocean developed according to a similar scenario. The warm and humid climate maintained high sea levels. This has contributed to an increase in the biodiversity of marine species.

All tropical areas of the Earth were covered with water, so climatic conditions were pretty much ideal for the variety of life.

As before, these are almost ideal conditions would have to end sooner or later. This time, the mass extinction that ended the Cretaceous period and then the entire Mesozoic era is thought to have been caused by one or more large meteors crashing into the Earth. The ash and dust released into the atmosphere blocked the sun, slowly killing off all the lush plant life that had accumulated on the land.

Likewise, most of the species in the ocean also disappeared during this time. As there were fewer and fewer plants, herbivores also gradually died out. Everything went extinct: from insects to large birds and mammals and, of course, dinosaurs. Only small animals that were able to adapt and survive in conditions of little food were able to see the beginning of the Cenozoic era.

Sources

Mesozoic deposits- sediments, sediments formed during the Mesozoic era. Mesozoic deposits include the Triassic, Jurassic and Cretaceous systems (periods).

In Mordovia, only Jurassic and Cretaceous sedimentary rocks are present. In the Triassic period (248 - 213 million years), the territory of Mordovia was dry land and sediments were not deposited. During the Jurassic period (213 - 144 million years), throughout the entire territory of the republic there was a sea in which clays, sands, and, less commonly, phosphorite nodules and carbonaceous shales accumulated.

Jurassic deposits reach the surface on 20 - 25% of the area (mainly along river valleys), with a thickness of 80 - 140 m. Associated with them are deposits of minerals - oil shale and phosphorites. During the Cretaceous period (144 - 65 million years), the sea continued to exist, and sediments of this age come to the surface on 60 - 65% of the territory in all regions of the Republic of Mordovia.

They are represented by 2 groups - Lower and Upper Cretaceous. On the eroded surface of Jurassic deposits (oil shale and dark clays) lie Lower Cretaceous: phosphorite conglomerate, greenish-gray and black clays and sands with a total thickness of up to 110 m. Upper Cretaceous deposits consist of light gray and white chalk, marl, opoka and make up the Cretaceous mountains in the southeastern regions of the Republic of Mordovia.

Thin layers are marked by green glauconitic and phosphorite-bearing sands. In other layers there are nodules and nodules of phosphorites, fossilized remains of organisms (belemnites, popularly called “devil’s fingers”). The total thickness is approximately 80 m.

Mesozoic era

The Atemarskoye and Kulyasovskoye chalk deposits and the Alekseevskoye deposit of cement raw materials are confined to the Upper Cretaceous deposits.

[edit] Source

A. A. Mukhin. Alekseevsky cement plant quarry. 1965

Mesozoic era

The Mesozoic era began approximately 250 and ended 65 million years ago. It lasted 185 million years. The Mesozoic era is divided into the Triassic, Jurassic and Cretaceous periods with a total duration of 173 million years. The deposits of these periods constitute the corresponding systems, which together form the Mesozoic group.

The Mesozoic is known primarily as the era of dinosaurs. These giant reptiles overshadow all other groups of living beings.

But you shouldn’t forget about others. After all, it was the Mesozoic - the time when real mammals, birds, and flowering plants appeared - that actually formed the modern biosphere.

And if in the first period of the Mesozoic - the Triassic, there were still many animals on Earth from Paleozoic groups that were able to survive the Permian catastrophe, then in the last period - the Cretaceous, almost all those families that flourished in the Cenozoic era had already formed.

The Mesozoic era was a transitional period in the development of the earth's crust and life. It can be called the geological and biological Middle Ages.
The beginning of the Mesozoic era coincided with the end of the Variscan mountain-building processes; it ended with the beginning of the last powerful tectonic revolution - the Alpine folding.

IN Southern Hemisphere in the Mesozoic, the collapse of the ancient continent of Gondwana was completed, but in general the Mesozoic era here was an era of relative calm, only occasionally and briefly disrupted by light folding.

The early stage of development of the plant kingdom - paleophyte, was characterized by the dominance of algae, psilophytes and seed ferns. The rapid development of more highly developed gymnosperms, which characterizes the “plant Middle Ages” (mesophyte), began in the Late Permian era and ended at the beginning of the Late Cretaceous era, when the first angiosperms, or flowering plants (Angiospermae), began to spread.

The Cenophyte began in the Late Cretaceous - modern period development of the plant kingdom.

This made their resettlement quite difficult. The development of seeds allowed plants to lose such close dependence on water. The ovules could now be fertilized by pollen carried by the wind or insects, and water thus no longer determined reproduction. In addition, unlike a single-celled spore with its relatively small supply of nutrients, the seed has a multicellular structure and is able to provide food for a young plant in the early stages of development for longer.

Under unfavorable conditions, the seed for a long time may remain viable. Having a durable shell, it reliably protects the embryo from external dangers. All these advantages gave seed plants good chances in the struggle for existence. The ovule (ovum) of the first seed plants was unprotected and developed on special leaves; the seed that emerged from it also did not have an outer shell.

Among the most numerous and most curious gymnosperms of the beginning of the Mesozoic era we find the Cycas, or sago. Their stems were straight and columnar, similar to tree trunks, or short and tuberous; they bore large, long and usually feathery leaves
(for example, the genus Pterophyllum, whose name means “feathery leaves”).

Outwardly, they looked like tree ferns or palm trees.
In addition to the cycads, great importance in the mesophyte they acquired Bennettitales, represented by trees or shrubs. They mostly resemble true cycads, but their seed begins to develop a tough shell, which gives Bennettites an angiosperm-like appearance.

There are other signs of adaptation of Bennettites to conditions of a drier climate.

In the Triassic, new forms came to the fore.

Conifers are spreading quickly, and among them are firs, cypresses, and yews. Among the ginkgos, the genus Baiera is widespread. The leaves of these plants had the shape of a fan-shaped plate, deeply dissected into narrow lobes. Ferns have taken over damp, shady places along the banks of small bodies of water (Hausmannia and other Dipteraidae). Forms that grow on rocks (Gleicheniacae) are also known among ferns. Horsetails (Equisetites, Phyllotheca, Schizoneura) grew in the swamps, but did not reach the size of their Paleozoic ancestors.
In the middle mesophyte (Jurassic period), the mesophytic flora reached the culmination point of its development.

The hot tropical climate in what is now the temperate zone was ideal for tree ferns to thrive, while smaller fern species and herbaceous plants preferred the temperate zone. Among the plants of this time, gymnosperms continue to play a dominant role
(primarily cycads).

The Cretaceous period is marked by rare changes in vegetation.

The flora of the Lower Cretaceous still resembles in composition the vegetation of the Jurassic period. Gymnosperms are still widespread, but their dominance ends at the end of this time.

Even in the Lower Cretaceous, the most progressive plants suddenly appeared - angiosperms, the predominance of which characterizes the era of new plant life, or Cenophyte.

Angiosperms, or flowering plants (Angiospermae), occupy the highest level of the evolutionary ladder of the plant world.

Their seeds are enclosed in a durable shell; there are specialized reproductive organs (stamen and pistil) assembled into a flower with bright petals and a calyx. Flowering plants appear somewhere in the first half of the Cretaceous period, most likely in a cold and dry mountain climate with large temperature differences.
With the gradual cooling that marked the Cretaceous, they captured more and more new areas on the plains.

Quickly adapting to their new environment, they evolved at amazing speed. Fossils of the first true angiosperms are found in the Lower Cretaceous rocks of Western Greenland, and a little later also in Europe and Asia. In a relatively short time, they spread throughout the Earth and reached great diversity.

From the end of the Early Cretaceous era, the balance of forces began to change in favor of angiosperms, and by the beginning of the Upper Cretaceous their superiority became widespread. Cretaceous angiosperms belonged to the evergreen, tropical or subtropical types, among them were eucalyptus, magnolia, sassafras, tulip trees, Japanese quince trees, brown laurels, walnut trees, plane trees, and oleanders. These heat-loving trees coexisted with the typical flora of the temperate zone: oaks, beeches, willows, and birches.

For gymnosperms, this was a time of surrender. Some species have survived to this day, but their total numbers have been declining all these centuries. A definite exception is conifers, which are still found in abundance today.
In the Mesozoic, plants made a great leap forward, surpassing animals in terms of development rates.

Mesozoic invertebrates were already approaching modern ones in character.

A prominent place among them was occupied by cephalopods, to which modern squids and octopuses belong. The Mesozoic representatives of this group included ammonites with a shell twisted into a “ram’s horn”, and belemnites, the inner shell of which was cigar-shaped and overgrown with the flesh of the body - the mantle.

Belemnite shells are popularly known as “devil’s fingers.” Ammonites were found in such numbers in the Mesozoic that their shells are found in almost all marine sediments of this time.

Ammonites appeared in the Silurian, they experienced their first flowering in the Devonian, but reached their highest diversity in the Mesozoic. In the Triassic alone, over 400 new genera of ammonites arose.

Particularly characteristic of the Triassic were ceratids, which were widespread in the Upper Triassic marine basin of Central Europe, the deposits of which in Germany are known as shell limestone.

By the end of the Triassic, most ancient groups of ammonites died out, but representatives of the Phylloceratida survived in Tethys, the giant Mesozoic Mediterranean Sea. This group developed so rapidly in the Jurassic that the ammonites of this time surpassed the Triassic in the variety of forms.

During the Cretaceous, cephalopods, both ammonites and belemnites, remained numerous, but during the Late Cretaceous the number of species in both groups began to decline. Among the ammonites at this time, aberrant forms appeared with an incompletely twisted hook-shaped shell (Scaphites), with a shell elongated in a straight line (Baculites) and with a shell irregular shape(Heteroceras).

These aberrant forms appeared, apparently, as a result of changes in the course of individual development and narrow specialization. The terminal Upper Cretaceous forms of some branches of ammonites are distinguished by sharply increased shell sizes. In the genus Parapachydiscus, for example, the shell diameter reaches 2.5 m.

The mentioned belemnites also acquired great importance in the Mesozoic.

Some of their genera, for example, Actinocamax and Belenmitella, are important fossils and are successfully used for stratigraphic division and accurate determination of the age of marine sediments.
At the end of the Mesozoic, all ammonites and belemnites became extinct.

Of the cephalopods with an external shell, only the genus Nautilus has survived to this day. More widespread in modern seas are forms with internal shells - octopuses, cuttlefish and squids, distantly related to belemnites.
The Mesozoic era was a time of unstoppable expansion of vertebrates. Of the Paleozoic fishes, only a few passed into the Mesozoic, as did the genus Xenacanthus, the last representative freshwater sharks Paleozoic, known from freshwater sediments of the Australian Triassic.

Sea sharks continued to evolve throughout the Mesozoic; Most modern genera were already represented in the Cretaceous seas, in particular, Carcharias, Carcharodon, lsurus, etc.

Ray-finned fish, which arose at the end of the Silurian, initially lived only in freshwater bodies of water, but with the Permian they began to enter the seas, where they multiplied unusually and from the Triassic to the present day they retained a dominant position.
Reptiles became most widespread in the Mesozoic, becoming truly the dominant class of this era.

In the course of evolution, a variety of genera and species of reptiles appeared, often of very impressive size. Among them were the largest and most bizarre land animals the earth has ever bore.

As already mentioned, in terms of anatomical structure, the most ancient reptiles were close to labyrinthodonts. The oldest and most primitive reptiles were the clumsy cotylosaurs (Cotylosauria), which appeared already at the beginning of the Middle Carboniferous and became extinct by the end of the Triassic. Among cotylosaurs, both small animal-eating and relatively large herbivorous forms (pareiasaurs) are known.

The descendants of cotylosaurs gave rise to the entire diversity of the reptile world. One of the most interesting groups of reptiles that developed from cotylosaurs were the beast-like animals (Synapsida, or Theromorpha), their primitive representatives (pelycosaurs) have been known since the end of the Middle Carboniferous. In the mid-Permian period, pelycosaurs, known mainly from North America, are dying out, but in the Old World they are replaced by more progressive forms that form the order Therapsida.
The predatory theriodonts (Theriodontia) included in it are already very similar to primitive mammals, and it is no coincidence - it was from them that the first mammals developed by the end of the Triassic.

During the Triassic period, many new groups of reptiles appeared.

These are turtles, and are well adapted to sea ​​life ichthyosaurs (“fish lizards”), outwardly resembling dolphins, and placodonts, clumsy armored animals with powerful flattened teeth adapted for crushing shells, and also plesiosaurs that lived in the seas, having a relatively small head, a more or less elongated neck, a wide body, flipper-like pairs limbs and short tail; Plesiosaurs vaguely resemble giant shellless turtles.

In the Jurassic, plesiosaurs, like ichthyosaurs, reached their peak. Both of these groups remained very numerous in the Early Cretaceous era, being extremely characteristic predators of the Mesozoic seas.
From an evolutionary point of view, one of the most important groups of Mesozoic reptiles were thecodonts, small predatory reptiles of the Triassic period, which gave rise to the most diverse groups - crocodiles, dinosaurs, flying lizards, and, finally, birds.

However, the most remarkable group of Mesozoic reptiles were the well-known dinosaurs.

They developed from thecodonts back in the Triassic and took a dominant position on Earth in the Jurassic and Cretaceous. Dinosaurs are represented by two groups, completely separate - saurischia (Saurischia) and ornithischia (Ornithischia). In the Jurassic, real monsters could be found among dinosaurs, up to 25-30 m long (with tail) and weighing up to 50 tons. Of these giants, the most famous forms are Brontosaurus, Diplodocus and Brachiosaurus.

And in the Cretaceous period the evolutionary progress of dinosaurs continued. Of the European dinosaurs of this time, bipedal iguanodonts are widely known; in America, four-legged horned dinosaurs (Triceratops) Styracosaurus, etc.), somewhat reminiscent of modern rhinoceroses, became widespread.

Also interesting are the relatively small armored dinosaurs (Ankylosauria), covered with a massive bony shell. All named forms were herbivores, as well as giant duck-billed dinosaurs (Anatosaurus, Trachodon, etc.), which walked on two legs.

In the chalk they reached their peak and carnivorous dinosaurs, the most remarkable of which were such forms as Tyrannosaurus rex, whose length exceeded 15 m, Gorgosaurus and Tarbosaurus.

All of these forms, which turned out to be the greatest land predatory animals in the entire history of the Earth, walked on two legs.

At the end of the Triassic, thecodonts also gave rise to the first crocodiles, which became abundant only in the Jurassic period (Steneosaurus and others). In the Jurassic period, flying lizards appeared - pterosaurs (Pterosauria), also descended from thecodonts.
Among the flying dinosaurs of the Jurassic, the most famous are Rhamphorhynchus and Pterodactylus; among the Cretaceous forms, the most interesting is the relatively very large Pteranodon.

Flying lizards became extinct by the end of the Cretaceous.
In the Cretaceous seas, giant predatory mosasaurian lizards, exceeding 10 m in length, became widespread. Among modern lizards, they are closest to monitor lizards, but differ from them, in particular, in their flipper-like limbs.

By the end of the Cretaceous, the first snakes (Ophidia) appeared, apparently descended from lizards that led a burrowing lifestyle.
Towards the end of the Cretaceous, there was a mass extinction of characteristic Mesozoic groups of reptiles, including dinosaurs, ichthyosaurs, plesiosaurs, pterosaurs and mosasaurs.

Representatives of the class of birds (Aves) first appear in Jurassic deposits.

Brief information about the Mesozoic era

The remains of Archaeopteryx, the well-known and so far only known first bird, were found in lithographic shales of the Upper Jurassic, near the Bavarian city of Solnhofen (Germany). During the Cretaceous period, the evolution of birds proceeded at a rapid pace; The characteristic genera of this time were Ichthyornis and Hesperornis, which still had serrated jaws.

The first mammals (Mattalia), modest animals no larger than a mouse, descended from animal-like reptiles in the Late Triassic.

Throughout the Mesozoic they remained few in number and by the end of the era the original genera were largely extinct.

The most ancient group of mammals were the triconodonts (Triconodonta), to which the most famous of the Triassic mammals, Morganucodon, belongs. Appears in the Jurassic
a number of new groups of mammals - Symmetrodonta, Docodonta, Multituberculata and Eupantotheria.

Of all the named groups, only the Multituberculata survived the Mesozoic, the last representative of which died out in the Eocene. Polytuberculates were the most specialized of the Mesozoic mammals, convergently they had some similarities with rodents.

The ancestors of the main groups of modern mammals - marsupials (Marsupialia) and placentals (Placentalia) were Eupantotheria. Both marsupials and placentals appeared in the Late Cretaceous. The most ancient group of placentals are insectivores (insectivora), which have survived to this day.

Which was followed by . The Mesozoic Era is sometimes called the "Age of the Dinosaurs" because these animals were the dominant species throughout much of the Mesozoic.

After the Permian mass extinction wiped out more than 95% of ocean life and 70% of land species, the new Mesozoic era began about 250 million years ago. It consisted of the following three periods:

Triassic period, or Triassic (252-201 million years ago)

The first big changes were noticed in the type that dominated the Earth. Most of the flora that survived the Permian extinction were seed-bearing plants such as gymnosperms.

Cretaceous period, or Cretaceous (145-66 million years ago)

The last period of the Mesozoic was called the Cretaceous. The growth of flowering land plants occurred. They were helped by newly appeared bees and warm climatic conditions. Coniferous plants were still numerous during the Cretaceous.

In terms of Cretaceous marine animals, sharks and rays became commonplace. , survivors of the Permian extinction, such as sea ​​stars, were also abundant during the Cretaceous.

On land, the first small mammals began to develop during the Cretaceous period. First marsupials appeared, and then other mammals. Appeared more birds and there were more reptiles. The dominance of dinosaurs continued, and the number of carnivorous species increased.

At the end of the Cretaceous and Mesozoic, another thing happened. This extinction is commonly called the K-T extinction (Cretaceous-Paleogene extinction). It destroyed all dinosaurs except birds and many other life forms on Earth.

There are different versions as to why the mass disappearance occurred. Most scientists agree that there was some kind of catastrophic event that caused this extinction. Various hypotheses include massive volcanic eruptions that released huge amounts of dust into the atmosphere, reducing the amount of sunlight reaching the Earth's surface and thereby causing the death of photosynthetic organisms such as plants and those that depended on them. Others believe that a meteorite fell to Earth and the dust covered it. sunlight. Because the plants and animals that fed on them died out, this meant that predators such as carnivorous dinosaurs also died due to lack of food.

The Mesozoic era began approximately 250 and ended 65 million years ago. It lasted 185 million years. The Mesozoic is known primarily as the era of dinosaurs. These giant reptiles overshadow all other groups of living beings. But you shouldn’t forget about others. After all, it was the Mesozoic - the time when real mammals, birds, and flowering plants appeared - that actually formed the modern biosphere. And if in the first period of the Mesozoic - the Triassic, there were still many animals on Earth from Paleozoic groups that were able to survive the Permian catastrophe, then in the last period - the Cretaceous, almost all those families that flourished in the Cenozoic era had already formed.

In the Mesozoic, not only dinosaurs arose, but also other groups of reptiles, which are often mistakenly considered dinosaurs - aquatic reptiles (ichthyosaurs and plesiosaurs), flying reptiles (pterosaurs), lepidosaurs - lizards, among which were aquatic forms - mosasaurs. Snakes evolved from lizards - they also appeared in the Mesozoic - the time of their emergence is generally known, but paleontologists argue about the environment in which this occurred - in water or on land.

Sharks flourished in the seas, and they also lived in freshwater bodies. Mesozoic - the heyday of two groups cephalopods– ammonites and belemnites. But in their shadow, the nautiluses, which arose in the early Paleozoic and still exist today, lived well, and the familiar squids and octopuses arose.

In the Mesozoic, modern mammals arose, first marsupials and then placentals. In the Cretaceous period, groups of ungulates, insectivores, predators and primates had already emerged.

Interestingly, modern amphibians - frogs, toads and salamanders - also arose in the Mesozoic, presumably in the Jurassic period. So, despite the antiquity of amphibians in general, modern amphibians are a relatively young group.

Throughout the Mesozoic, vertebrates sought to master a new environment for themselves - the air. The first reptiles were able to take off - first small pterosaurs - rhamphorhynchus, then larger pterodactyls. Somewhere on the border of the Jurassic and Cretaceous, reptiles took to the air - small feathered dinosaurs, capable, if not of flight, then certainly of gliding, and the descendants of reptiles - birds - enantiornis and true fan-tailed birds.

A real revolution in the biosphere occurred with the advent of angiosperms - flowering plants. This resulted in an increase in the diversity of insects that became flower pollinators. The gradual spread of flowering plants has changed the appearance of terrestrial ecosystems.

The Mesozoic ended with the famous mass extinction, better known as the “extinction of the dinosaurs.” The reasons for this extinction are not clear, but the more we learn about the events that took place at the end of the Cretaceous, the less convincing the popular hypothesis of a meteorite catastrophe becomes. The Earth's biosphere was changing and the ecosystems of the Late Cretaceous were very different from the ecosystems of the Jurassic period. A huge number of species became extinct throughout the Cretaceous period, and not at all at its end - they simply did not survive the catastrophe. At the same time, evidence is emerging that in some places the typical Mesozoic fauna still existed at the very beginning of the next era - the Cenozoic. So for now, it is not possible to unequivocally answer the question about the causes of the extinction that occurred at the end of the Mesozoic. It is only clear that if some kind of catastrophe did occur, it only pushed the changes that had already begun

I present to your attention a small collection of fossilized mineralized wood that I have accumulated over many years of collecting. Something was found by me, something was donated (to all those who gave a low bow and health, may the hand of the giver not become scarce), something was bought. It should be said right away that wood appeared a very long time ago. The earliest of known to science fossil woody plants were discovered in 2011 in the Canadian province of New Brunswick, where between 400 and 395 million years ago... >>>

The Mesozoic is an era of tectonic, climatic and evolutionary activity. The formation of the main contours of modern continents and mountain building on the periphery of the Pacific, Atlantic and Indian oceans is taking place; the division of land facilitated speciation and other important evolutionary events. The climate was warm throughout the entire time period, which also played an important role in the evolution and formation of new animal species. By the end of the era, the bulk of the species diversity of life approached its modern state.

Geological periods

• Triassic period (252.2 ± 0.5 - 201.3 ± 0.2)
• Jurassic (201.3 ± 0.2 - 145.0 ± 0.8)
• Cretaceous period (145.0 ± 0.8 - 66.0).

The lower (between the Permian and Triassic periods, that is, between the Paleozoic and Mesozoic) boundary is marked by the Permo-Triassic mass extinction, which resulted in the death of approximately 90-96% of marine fauna and 70% of land vertebrates. The upper limit is set at the Cretaceous-Paleogene boundary, when another very large extinction of many groups of plants and animals occurred, most often attributed to the impact of a giant asteroid (Chicxulub crater on the Yucatan Peninsula) and the subsequent “asteroid winter”. Approximately 50% of all species became extinct, including all flightless dinosaurs.

Tectonics and paleogeography

Compared to the vigorous mountain building of the late Paleozoic, Mesozoic tectonic deformation can be considered relatively mild. The era was characterized primarily by the division of the supercontinent Pangea into a northern continent, Laurasia, and a southern continent, Gondwana. This process led to the formation of the Atlantic Ocean and passive continental margins, in particular most of the modern Atlantic coast(e.g. east coast of North America). Extensive transgressions that prevailed in the Mesozoic led to the emergence of numerous inland seas.

By the end of the Mesozoic, the continents had practically taken on their modern shape. Laurasia was divided into Eurasia and North America, Gondwana into South America, Africa, Australia, Antarctica and the Indian subcontinent, the collision of which with the Asian continental plate caused intense orogenesis with the uplift of the Himalayan mountains.

Africa

At the beginning of the Mesozoic era, Africa was still part of the supercontinent Pangea and had a relatively common fauna with it, which was dominated by theropods, prosauropods and primitive ornithischian dinosaurs (by the end of the Triassic).

Late Triassic fossils are found throughout Africa, but are more common in the south than in the north of the continent. As is known, the time line separating the Triassic from the Jurassic period is marked by a global catastrophe with mass extinction of species (Triassic-Jurassic extinction), but the African layers of this time remain poorly studied today.

Early Jurassic fossil deposits are distributed similarly to Late Triassic deposits, with more frequent exposures in the south of the continent and fewer deposits towards the north. Throughout the Jurassic period, iconic dinosaur groups such as sauropods and ornithopods increasingly spread across Africa. The paleontological layers of the mid-Jurassic period in Africa are poorly represented and also poorly studied.

Late Jurassic strata are also poorly represented here, with the exception of the impressive Tendeguru Jurassic assemblage in Tanzania, whose fossils are very similar to those found in the paleobiotic Morrison Formation of western North America and date to the same period.

In the mid-Mesozoic, about 150-160 million years ago, Madagascar separated from Africa, while remaining connected to India and the rest of Gondwanaland. Abelisaurs and titanosaurs have been discovered among the fossils of Madagascar.

During the Early Cretaceous era, a part of the landmass that made up India and Madagascar separated from Gondwana. In the Late Cretaceous, the divergence of India and Madagascar began, which continued until the achievement of modern outlines.

Unlike Madagascar, mainland Africa was tectonically relatively stable throughout the Mesozoic. And yet, despite its stability, significant changes occurred in its position relative to other continents as Pangea continued to break apart. By the beginning of the Late Cretaceous period, South America separated from Africa, thereby completing the formation of the Atlantic Ocean in its southern part. This event had a huge impact on the global climate by changing ocean currents.

During the Cretaceous, Africa was inhabited by allosauroids and spinosaurids. The African theropod Spinosaurus turned out to be one of the largest carnivores that lived on Earth. Among the herbivores in the ancient ecosystems of those times, titanosaurs occupied an important place.

Cretaceous fossil deposits are more common than Jurassic deposits, but often cannot be radiometrically dated, making it difficult to determine their exact age. Paleontologist Louis Jacobs, who has spent considerable time in field work in Malawi, argues that African fossil deposits “need more careful excavation” and are sure to prove “fertile ... for scientific discoveries.”

Climate

Over the past 1.1 billion years, Earth's history has seen three successive ice age-warming cycles, called Wilson cycles. Longer warm periods were characterized by a uniform climate, a greater diversity of flora and fauna, and a predominance of carbonate sediments and evaporites. Cold periods with glaciations at the poles were accompanied by a decrease in biodiversity, terrigenous and glacial sediments. The reason for cyclicity is considered to be the periodic process of connecting continents into a single continent (Pangea) and its subsequent disintegration.

The Mesozoic era is the warmest period in the Phanerozoic history of the Earth. It almost completely coincided with the period of global warming, which began in the Triassic period and ended already in the Cenozoic era with a small ice age, which continues to this day. For 180 million years, even in the subpolar regions there was no stable ice cover. The climate was mostly warm and even, without significant temperature gradients, although climatic zonation existed in the northern hemisphere. A large number of greenhouse gases in the atmosphere contributed to the uniform distribution of heat. The equatorial regions were characterized by a tropical climate (Tethys-Panthalassa region) with average annual temperature 25–30°C. Up to 45-50° N The subtropical region (Peritethys) extended, followed by the warm-temperate boreal zone, and the subpolar regions were characterized by a cool-temperate climate.

During the Mesozoic there was warm climate, mostly dry in the first half of the era and wet in the second. Small cooling in the late Jurassic and the first half of the Cretaceous, strong warming in the middle of the Cretaceous (the so-called Cretaceous temperature maximum), around the same time the equatorial climate zone appears.

Flora and fauna

Giant ferns, tree horsetails, and mosses are dying out. In the Triassic, gymnosperms, especially conifers, flourished. In the Jurassic period, seed ferns died out and the first angiosperms appeared (so far represented only by woody forms), which gradually spread to all continents. This is due to a number of advantages; angiosperms have a highly developed conducting system, which ensures reliable cross-pollination, the embryo is supplied with food reserves (due to double fertilization, a triploid endosperm develops) and is protected by membranes, etc.

In the animal world, insects and reptiles flourish. Reptiles occupy a dominant position and are represented a large number forms In the Jurassic period, flying lizards appear and conquer the air. In the Cretaceous period, the specialization of reptiles continued, they reached enormous sizes. The mass of some of the dinosaurs reached 50 tons.

The parallel evolution of flowering plants and pollinating insects begins. At the end of the Cretaceous period, cooling sets in and the area of ​​semi-aquatic vegetation decreases. Herbivores are dying out, followed by carnivorous dinosaurs. Large reptiles are saved only in tropical zone(crocodiles). Due to the extinction of many reptiles, a rapid adaptive radiation of birds and mammals begins, occupying the vacated ecological niches. Many forms of invertebrates and sea lizards are dying out in the seas.

Birds, according to most paleontologists, descended from one of the groups of dinosaurs. The complete separation of arterial and venous blood flows caused them to be warm-blooded. They spread widely over land and gave rise to many forms, including flightless giants.

The emergence of mammals is associated with a number of large aromorphoses that arose in one of the subclasses of reptiles. Aromorphoses: a highly developed nervous system, especially the cerebral cortex, which ensured adaptation to living conditions through changes in behavior, movement of the limbs from the sides under the body, the emergence of organs that ensure the development of the embryo in the mother’s body and subsequent feeding with milk, the appearance of fur, complete separation of the circulatory system, the appearance of alveolar lungs, which increase the intensity of gas exchange and, as a consequence, the overall level of metabolism.

Mammals appeared in the Triassic, but could not compete with dinosaurs and for 100 million years occupied a subordinate position in the ecological systems of that time.

Scheme of the evolution of flora and fauna in the Mesozoic era.

Literature

• Iordansky N. N. Development of life on earth. - M.: Education, 1981.
• Koronovsky N.V., Khain V.E., Yasamanov N.A. Historical geology: Textbook. - M.: Academy, 2006.
• Ushakov S.A., Yasamanov N.A. Continental drift and climates of the Earth. - M.: Mysl, 1984.
• Yasamanov N.A. Ancient climates of the Earth. - L.: Gidrometeoizdat, 1985.
• Yasamanov N.A. Popular paleogeography. - M.: Mysl, 1985.

Links

	Portal "Mesozoic"
	Mesozoic on Wikimedia Commons

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Mesozoic… Spelling dictionary-reference book

The Mesozoic era is divided into the Triassic, Jurassic and Cretaceous periods.

After the intense mountain building of the Carboniferous and Permian periods, the Triassic period is characterized by relative tectonic quiescence. Only at the end of the Triassic, on the border with the Jurassic, does the ancient Cimmerian phase of the Mesozoic fold appear

frequency. Volcanic processes in the Triassic are quite active, but their centers move to the Pacific geosynclinal belts and to the region of the Mediterranean geosyncline. In addition, the formation of traps continues on the Siberian Platform (Tunguska Basin).

Both the Permian and Triassic were characterized by a strong reduction in the area of ​​epicontinental seas. Vast areas of modern continents are almost devoid of Triassic marine sediments. The climate is continental. The fauna takes on the appearance that later became characteristic of the Mesozoic era as a whole. The sea is dominated by cephalopods (ammonites) and elasmobranch molluscs; sea ​​lizards appear, already dominating the land. Among the plants, gymnosperms predominate (cycads, conifers and gingcaes).

Triassic deposits are poor in minerals (coal, building materials).

The Jurassic period is tectonically more intense. At the beginning of the Jurassic, the Old Cimmerian, and at the end of the New Cimmerian, phases of Mesozoic (Pacific) folding appeared. Within the northern continental platforms and areas previously subject to mountain building, deep faults develop and depressions form in the northern hemisphere. In the southern hemisphere, the continent of Gondwana begins to disintegrate. Volcanism is actively manifested in geosynclinal belts.

Unlike the Triassic, the Jurassic is characterized by transgressions. Thanks to them, the climate becomes less continental. During this period, further development of the flora of gymnosperms occurs.

The significant development of the fauna was expressed in a noticeable increase and specialization of species of marine and terrestrial animals. The development of lizards continues (predatory, herbivorous, marine, terrestrial, flying), the first species of birds and mammals appear. The sea is dominated by cephalopod ammonites, new species of sea urchins, lilies, etc. appear.

The main minerals found in Jurassic deposits are: oil, gas, oil shale, coal, phosphorites, iron ores, bauxite and a number of others.

In the Cretaceous period, intense mountain building occurred, which was called the Laramie phase of Mesozoic folding. The Laramie orogeny developed with greatest force at the boundary of the Lower and Upper Cretaceous, when extensive geosynclines arose in the Pacific geosynclines. mountainous countries. In the Mediterranean belt, this phase was preliminary and preceded the main orogenesis, which developed later in the Cenozoic era.

For the southern hemisphere, in addition to mountain building in the Andes, the Cretaceous period was marked by further fractures of the Gondwana continent, the submergence of large areas of land and the formation of the Indian Ocean and South Atlantic depressions. Fractures of the earth's crust and mountain building were accompanied by the manifestation of volcanism.

The fauna of the Cretaceous period was dominated by reptiles and many species of birds appeared. There are still a few mammals. The sea continues to be dominated by ammonites and elasmobranch mollusks, sea urchins, lilies, corals, and foraminifera are widely developed, from the shells of which (partially) the formation of layers of white writing chalk occurred. The flora of the Lower Cretaceous is of a typical Mesozoic character. In it, gymnosperms continued to predominate, but in the Upper Cretaceous era, the dominant role passed to angiosperms, close to modern ones.

On the territory of the platforms, Cretaceous deposits are distributed approximately in the same place as Jurassic ones, and contain the same complex of minerals.

Considering the Mesozoic era as a whole, it should be noted that “it was marked by new manifestations of orogenic phases, which were most developed in the Pacific geosynclinal belts, for which the Mesozoic era of orogenesis is often called the Pacific era. In the Mediterranean geosynclinal belt, this orogeny was preliminary. Young mountain structures joined as a result of the closure of geosynclines increased the size of rigid sections of the earth's crust. At the same time, mainly in the southern hemisphere, the opposite process began to develop - the collapse of the ancient continental mass of Gondwana. Volcanic activity was no less intense in the Mesozoic than in the Paleozoic. Great changes have occurred in the composition of flora and fauna. Among terrestrial animals, reptiles flourished and declined at the end of the Cretaceous period. Ammonites, belemnites and a number of other animals underwent the same development in the seas. In place of the gymnosperms that dominated the Mesozoic, an angiosperm flora appeared in the second half of the Cretaceous.

Of the mineral resources formed in the Mesozoic era, the most important are oil, gas, coal, phosphorites and various ores.