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A temperate deciduous forest, more precisely termed temperate broadleaf forest or temperate broadleaved forest, is a biome found in the eastern and western United States, Canada, central Mexico, southern South America, Europe, West Asia, China, Japan, North Korea, South Korea and parts of Russia. A temperate deciduous forest consists of trees that lose their leaves every year. Examples include oak, maple, beech, and elm.
Organisms and their adaptations
Many well-known animals live in this kind of forest. Some examples are the Eastern Gray Squirrel, bears, beavers, foxes, deer, rats, snakes, mice, wolves, raccoons, and large birds of prey like red-tailed hawks. These animals have unique adaptations suited for seasonal life. For example, some rodents store up fat, then hibernate during cold winters. Birds include the bald eagle, nightingale, cardinals, hawks, and the snowy owl.
The plants are adapted to survive in these conditions. For example, trees like the palm, white spruce, and the elm have leaves that absorb water and sunlight. The soaring branches do more than just provide shade for other creatures of this biome; they also provide nutrients necessary for the tree to live. Another example of adaptation: these trees shed their leaves in the winter. By shedding their leaves, they cannot transpire. Consequently, they are able to retain water for the winter. Plants also soak up nutrients from the soil. These plants shed their leaves in fall.
The temperate deciduous forest has a temperate climate, with summer highs of around 80 to 90 degrees Fahrenheit (27 to 32 degrees Celsius). Winter highs are around 30 to 55 degrees Fahrenheit (-1 to 15 degrees Celsius). Temperate forests get about 35 to 60 inches (900 to 1500 millimeters) of pate]
Humans have often colonized areas in the temperate deciduous forest. They have also harvested wood for timber. As a result, less than one quarter of original forests remain. Temperate forests have also been used for farming.
The temperate deciduous broadleaf forest (TDBF) is composed of broad-leaf angiosperm trees like the oaks, maples, and beeches familiar to many Americans and Europeans. The forests exist best in moderate climates that are neither too hot nor too cold and neither too wet nor too dry. In addition to the temperate zone, deciduous forests are found in tropical and sub-tropical climates in open savannas and/or in closed forests. While there are roughly thirty families and sixty-five genera in the TDBF, variation in the precise definition and defined area of the forest make absolute numbers impossible. With thousands of species, the TDBF is a highly diverse biome. Worldwide, there are five major groups of TDBFs. Within each group, botanists define TDBFs by the species that tend to occur in a given area. These collections of species, together with their environment, are called associations. Eastern North America today contains the most extensive TDBF. The forest reaches from about longitude 95Â°W (just west of the Mississippi River) to the Atlantic coast and from 30 to 45Â°N, thereby forming a quadrant that includes most of the northeastern quarter of the United States. The eastern United States TDBF was almost completely deforested for agricultural purposes by 1850. At that time, land was opened for agriculture in the Mississippi valley, and many farms were abandoned. Pines grew well in the remaining grassy fields, but after a catastrophic hurricane in 1937, the TDBF grew back. Today, there is much more TDBF in the United States than there was one hundred years ago (though still less than before the arrival of European settlers). There are nine generally recognized associations in the United States TDBF, each defined by differences in vegetation (see accompanying table). Though the species are representative of common dominants, many other species exist. TDBF associations are not completely separate. Many species, such as northern red oak and sugar maple, exist in more than one association. Nor are the boundaries between the associations sharp and easily identifiable. In particular, the Western Mesophytic association can be difficult to distinguish from its neighbors to the east (Mixed Mesophytic) and west (Oak-Hickory). Associations can change with time too. The Oak-Chestnut association is now almost completely devoid of chestnut, but many people still use the association name even though it is now mostly oak and maple. Association names in North America and elsewhere are most useful for distinguishing broad differences in forest type often associated with variation in soils, topography, and climate. The European TDBF, stretching through most of Europe (except for very hot and cold areas) from the Atlantic Ocean to the Ural Mountains, is the second-largest TDBF. Due to the moderating influences of the Gulf Stream, the TDBF exists as far as 60Â°N in northwestern Europe. Forests in Europe have been extensively modified by humans for more than two thousand years and are some of the most manipulated forests in the world. In the northern European TDBF, birch species are common, while in the middle European latitudes, beech (Fagus sylvatica ) is widely distributed and commercially valuable. Towards the south, various oak and maple species abound. As in North America, much of the once-cleared TDBF is now regrowing. The European TDBF is replaced by drought-resistant shrubs and evergreen broadleaf trees in the south and the boreal coniferous forest in the north. The last three TDBF areas are much smaller than the first two. East Asia, from 30Â° to 60Â°N and from central Japan to longitude 125Â°E in the northwest and longitude 115Â°E in the southwest, originally maintained very large forests. Today, even though the species mix is still very diverse, much of the East Asian forest outside of Japan is currently under cultivation and most existing forest fragments are protected refuges or in areas unsuitable for agriculture. Nearly all TDBF genera are present in East Asia, especially China. The Near East between 35Â° and 45Â°N, including areas around the eastern Black Sea and mountainous regions in Iran and near the Caspian Sea, supports a diverse TDBF. Finally, a narrow strip of South America including southern Chile and Argentina contain TDBF. Acacia caven and seven Nothofagus species are also found there. In nearly all cases, the deciduous trees of South America occur in mixtures with evergreen broadleaf species. Of the three major TDBFs, East Asia has by far the greatest diversity, followed by North America and Europe. East Asia was glaciated less severely than America and Europe, so most species were able to survive with little difficulty. In North America, the north-to-south orientation of major mountain ranges allowed species to migrate, and species diversity here is only slightly lower than in East Asia. In Europe, on the other hand, the east-to-west mountains caused the TDBF to be trapped by advancing glaciers. Many modern European TDBF species survived only in the Near East TDBF and migrated back after the glaciers retreated. Consequently, Europe has very low-species diversity. TDBFs are generally restricted to a warm temperate climate with four identifiable seasons in which the average temperature of the coldest month is between 3 and 18Â°C and the average temperature of the warmest month exceeds 10Â°C. The length of the frost-free period ranges from 120 to over 250 days. Precipitation is year-round and averages between 80 and 200 centimeters per year. Snowfall can range from nonexistent in the southeastern United States to extremely heavy in northern habitats. Climates that are wet and warm all year are occupied by tropical forest consisting of broadleaf evergreen trees. As climates become drier, as occurs at the western edge of the Oak-Hickory association, drought stresses are too extreme for TDBF and grasses become dominant. To the north of the major TDBF, extreme cold, short growing seasons and poor soils favor evergreen coniferous forests. TDBF soils tend to be deep and fertile and, unlike some soils in the northern coniferous forest, do not freeze year-round. For this reason, TDBFs have historically been popular for agricultural use. Deciduous leaves are the most distinctive feature of the TDBF. In the fall, spectacular reds, oranges, and yellows produce breathtaking displays across the TDBF. Why does this occur? During autumn, as temperatures cool and days shorten, trees send hormonal signals to their leaves causing them to turn colors and fall off the branch. First, leaves form a barrier between the leaf and the branch, known as the abscission layer. At the same time, chlorophyll, the compound that gathers light for photosynthesis, begins to degrade in the leaf. Many of the nutrients in the leaf are sucked back into the tree for next year's leaves. Chlorophyll is responsible for the usual green leaf color: once it is gone, yellow and orange pigments that were there all along become visible. Some of the sugar in the leaves of oaks and maples may be converted into red colors. Once the leaf is totally shut down and no longer conducting any photosynthesis, the abscission layer becomes very brittle. Any small breeze can snap the leaf off at this point. In the spring, using carbon from special storage cells in the trunk, trees grow a new batch of leaves. In an evolutionary adaptation designed to maximize the amount of light received, shrubs and small trees growing in the understory will begin growth before the overstory. The study of any recurring biological cycle and its connection to climate is called phenology. Patterns of bird migration and insect outbreaks are examples of phenological cycles. For centuries, scientists have been studying phenology in the TDBF. In the deciduous forest, phenology refers to the timing of spring leaf growth and fall leaf drop and their relationship to climatic variation. Observational evidence has shown that TDBF phenology is highly sensitive to variation in weather. Warm springs will cause leaves to grow earlier, sometimes by up to as much as one month. Conversely, plants respond to a cold fall by dropping th
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Answers:Heres a start you will need to research each category fungi --reproduce via spoors so that the wind can carry them to new habitats (ie logs, leaves, etc.) decomposers...can make their own food. (Instead, consumers must feed on other organisms, including producers and other consumers.Most animals, for example, eat plants or other animals that have fed on plants.) Decomposers feed on the tissues of dead or dying producers and consumers. Bacteria and fungi are common decomposers. saprophites(a bacteria--produces enzymes to digest the food externally then vacuum it such as fungi etc) lichen-- earthworms nematodes (soil invertebrates) The best wood rotters in the natural world are fungi (Barron, 26). The major wood rotters belong to the phyla Basidiomycota and Ascomycota. These fungi have the distinctive capacity to infiltrate and enzymatically digest the lignin, cellulose and hemicellulose components of the hardest wood. Roughly 80 billion tons of carbon are returned to the atmosphere each year as carbon dioxide through the biodegradation of woody material. Consequently, fungi play an important role in the carbon cycle (Barron, 27).
Answers:1.What is it? - A deciduous forest is one comprised primary of deciduous trees - those that lose their leaves once a year. A temperate deciduous forest is one that is in a temperate zone. 2.Where is it? - The temperate deciduous forest biome occupies most of the eastern part of the United States and a small strip of southern Ontario. 3.What types of plants and animals live in this biome? - American Beech Carpet Moss Common Lime Guelder Rose Lady Fern Northern Arrowwood Pecan Shagbark Hickory Tawny Milksap Mushroom White Birch White Oak American Bald Eagle American Black Bear Coyote Duckbill Platypus Eastern Chipmunk European Red Squirrel Fat Dormouse Least Weasel White-tailed Deer 4.What types of abiotic factors take place there? - Climate is a mix of temperature and precipitation. Deciduous forests have almost 14 inches of rain in the winter months and more than 18 inches of rain in the summer. The soil is very fertile. This biome is located between the polar regions and the tropics, so large air masses from both cold and warm areas of the Earth affect the climate. The leaves of deciduous trees are broad and quite light. This gives the leaves a bigger surface to capture sunlight to help produce food for the plant. 5.What are 3 interesting facts? - The largest tree in the world is found right here in the United States. You can find it in California. This giant sequoia tree is 275 feet tall and 95 feet around. Boy, that's HUGE! The largest forest in the world covers parts of Scandinavia and northern Russia. It has over 3.5 million square miles of land covered in trees! Most hardwood trees are used for firewood, construction, or art. Lots of forests are being cut down for farm land.
Answers:http://biomee.wikispaces.com/Deciduous+Forest?f=print Scroll down to Cycles.