FALL 1999
Grand Teton Mountain Range with Glaciers
Teton National Park, Wyoming
July 1999
Dr. Howard
September 20, 1999
COMPONENTS OF SEDIMENTARY ROCKS
Most of the Earth’s crust consists of sedimentary rock which is formed primarily by the lithification of sediments. These sediments include sand , silt and clay. Because soil is the breakdown of sedimentary rock, it follows that the components of soil include sand, silt and clay. The characteristics of these particles will be discussed later.
Examples of sedimentary rock:
Sandstone - formed by cementation of sand grains (any deposit of sand can lithify to sandstone) consists mostly of quartz and some feldspar
Shale - consists of silt and clay deposits that lithify on lake bottoms, at the ends of rivers in deltas, beside rivers in flood and on parts of ocean floor
Limestone - unlike other sedimentary rocks of ocean formed by lithification, limestone is formed by various chemical processes. One process is the cementation of algae, corals, and shells. Limestone is rich in calcite.
METAMORPHIC ROCKS
Rocks that have been changed from preexisting rocks by heat, pressure, or chemical processes within the Earth’s interior. New metamorphic rocks have textures different from those of the original rock.
Examples of Metamorphic rock:
Marble - formed by metamorphism of limestone-predominant mineral is calcite.
Slate - formed by metamorphism of shale - predominant minerals are biotite, muscovite, quartz
WEATHERING AS A SECOND FACTOR IN THE FORMATION OF SOIL
Weathering refers to the physical and chemical processes that break down rock at or near the Earth’s surface. After weathering has occurred these rock particles may be picked up and physically moved by streams or glaciers in the process known as erosion.
MECHANICAL WEATHERING (PHYSICAL DISINTEGRATION) *
Breaks up rock but does not change composition.
Examples of mechanical weathering include frost action, abrasion, pressure, release, plant growth and burrowing animals.
Frost acts by prying rocks apart. Most rocks contain a system of cracks called joints. Water that has trickled into the joints freezes and expands (obviously under appropriate temperatures) and in so doing wedges the rock apart, extends the joints, or breaks the rock into pieces.
Abrasion is the grinding away of rock by friction and impact by glaciers, waves, and wind. For example, as rock fragments are moved down a stream, they tumble against each other as well as against the stream bottom.
The growth of roots in cracks and burrowing animals can contribute to the physical disintegration of rocks by enlarging passageways for water and air which lead to chemical decomposition.
CHEMICAL WEATHERING (ROCK DECOMPOSITION) *
Transforms rocks and minerals exposed to water and air into new minerals.
ROLE OF OXYGEN IN CHEMICAL WEATHERING*
Because of its obvious abundance in the atmosphere and its chemical activity, oxygen is constantly combining with substances on the surface of the Earth.
EX: Oxygen combines with numerous iron-containing minerals to form a new iron - containing mineral : hematite
4Fe# + 302 ---> 2 Fe2 O3##
# Fe present in minerals such as biotite, olivine, pyroxenes
## Iron oxide -- This is the mineral hematite
If water is present (as it usually is) the water may combine with hematites to form limonite. Hematite and limonite are what give soil its reddish and yellowish colors.
ROLE OF ACID IN CHEMICAL WEATHERING*
Acid is an important cause of chemical weathering.
The hydrogen ions given off by acids disrupt the orderly arrangement of atoms within minerals. Essentially, the hydrogen ion substitutes for other positive ions within minerals and causes one mineral to be changed into another.
CARBONIC ACID*
The most important natural source of acid for rock weathering is dissolved carbon dioxide in water. 0.03% of the Earth’s atmosphere is carbon dioxide. When this carbon dioxide mixes with rain, the following reaction may occur:
CO2 + H2O ---> H2CO3 (Carbonic acid) + H+ (Hydrogen ion) + HCO3-
Thus, most rain is slightly acidic when it hits the ground and is able to decompose rocks on the Earth’s surface.
Soil usually has a higher content of carbon dioxide (up to 10%) because CO2 is produced by the respiration of soil organisms and by the decay of organic matter. Rainwater that has percolated through the soil may be quite acidic and reactive with minerals in unweathered rock below the Earth’s surface.
Examples of Chemical Weathering: *
1. Rainwater percolates through the soil.
2. It picks up CO2 from atmosphere and upper part of soil.
3. Water comes in contact with feldspar in lower part of soil.
4. Acidic water reacts with feldspar to alter it to clay mineral.
5. Hydrogen ion attaches feldspar and becomes incorporated into the clay mineral.
6. When hydrogen ion moves into feldspar, it releases potassium which moves into solution.
7. Bicarbonate ion also moves into solution.
8. Silica also moves into solution.
9. Weathering process is same regardless of type of feldspar. For example, Na-feldspar Ca-feldspar form sodium ions and calcium ions.
*Material from:
Plummer, C.C. et al: Physical Geology, 8th Ed., 1996. Boston. WCB/McGraw-Hill
Prairie Dandelions, Grasses and Rushes
around a Prairie Pothole in North Dakota
July 1999
September 24, 1999
Mrs. Wende
PUTTING PLANTS IN PERSPECTIVE
Just what is a plant? Generally, we call an organism a plant if :
1. It is a multi-cellular organism with cells that specialize to form tissues and organs
and…
2. Has cells with walls that contain cellulose
and…
3. Contains pigments, primarily chlorophyll, which can transform solar energy into organic compounds
and…
4. Has a life cycle that has two stages --- an asexual one and a sexual one. (This is called alternation of generation.)
and…
5. Protects developing embryos by covering them within the female reproductive organ which contains an outer layer of nutrient cells
Plants – the oldest living organisms on Earth – have been around even longer than dirt! With such a history, they exist in many diverse forms in our world today, ranging in size from microscopic algae to towering redwoods.
With such diversity comes a range of complexity. Single-celled algae start the family history. Next comes the liverworts, club mosses and ferns. Gymnosperms, which include all our coniferous plants, and angiosperms, the flowering plants, complete this chain of complexity.
Characteristics of Major Plant Divisions
Bryophytes
Ferns
Ginkos
Gymnosperms
Angiosperms
Additionally, angiosperms can be further divided into 2 classes, monocotyledons (monocots) and dicotyledons (dicots). Fossil records show that dicots developed first, followed by the monocots. The following table lists the differentiating characteristics of the two classes:
PARTS OF A PLANT
The example for this study is the division of angiosperms.
A. Roots
Roots (or, more specifically, the root system – the main root and all its branches) are important to a plant for three main reasons:
(You can find diagrams in your textbook on pages 114-15.)
Dicots
1. Epidermis – forms the outer layer of the root. It is only a single layer of cells. These cells form the root hairs.
2. Cortex – Next layer of cells, going inward. It is composed of irregular shaped cells called parenchyma. These cells are loosely packed, so that water and minerals can moves through the cortex area without entering into the cells. The function of cortex area: food storage
3. Endodermis – The next innermost layer is a single-cell layer that forms the boundary between the cortex and the inner vascular bundle. Cells here fit snugly, and contain substances that make the layer impermeable to water and mineral ions. (Only access to the vascular bundle is from the endodermal cells.)
4. Vascular cylinder or bundle – Cells here retain ability to divide and can give rise to secondary roots here. This area contains the vascular tissues:
Monocots
Roots in monocots differ from those in dicots by:
1. Not having as much secondary growth
2. Have a central tissue called pith, which is surrounded by alternating bundles of xylem and phloem throughout.
Specialized Roots
Some roots take on specific additional functions. These specialized tasks include:
1. Food storage roots -- sweet potatoes, yams. Parenchymal cells store large amounts of carbohydrates.
2. Water storage roots – Pumpkins and other plants that grow in arid regions.
3. Propagative roots – Produce adventitious buds (buds appearing in unusual places) along the root. Buds then develop into aerial stems. Ex – As seen in our own ecosystem: Canadian thistle, Tree of Heaven
B. Stems
Purposes for the stems of plants include:
Growth of stems is comparable to that of roots.
Primary growth comes from the apical meristem at the stem tip. This tissue is called shoot apical meristem. This tissue is within a terminal bud that is protected by a leaf primordia(an envelope of immature leaves. The terminal bud becomes dormant in cold weather in temperate areas, protected by bud scales. In the spring, these scales fall of and leave a scar.
Leaf primordia are produced by apical meristem at regular intervals. The area of a stem between these nodes is called internode area. When a stem grows, all growth takes place in the internode areas.
A young stem is called a shoot. In addition to the specialized leaf primordia found here, three other tissues arise from the primary meristematic tissue:
Stems are identified as:
1. Herbaceous (non-woody)
These stems exhibit only primary growth. The epidermis contains a waxy cuticle layer which prevents water loss from the plant. Phloem and xylem are arranged within bundles, with xylem located the most inward and phloem in the outer area. The cortex may be green and may carry out some photosynthesis, much like in leaves.
2. Woody
These stems have primary and secondary tissues. Primary tissues are formed each year from primary meristem. Secondary tissues develop during the second and subsequent years of growth from the lateral meristem. After secondary growth has continued for several years, it is no longer possible to make out individual vascular bundles. Instead, a woody stem has three separate areas -- bark, wood and pith – that have formed.
Cork, formed by cork cambrium, replaces the epidermis. Phloem can exist in this soft layer. In older trees, the heartwood no longer functions in water or nutrient transport, as its xylem cells have become clogged with substances like lignin, tannins and resins. These substances give the tree support and also act as antibacterial agents, prevents the growth of bacteria in these "dead" areas of the tree. Woody plants grow in girth due the presence of vascular cambrium and cork cambrium.
The growing/living layer of a woody stem is the sapwood. This tissue is weaker in its support of the tree, and makes up most of the stem thickness in younger trees. A layer of new sapwood is added to the outer edge of heartwood each year of growth, giving rise to the familiar tree rings.
Just as some roots perform specialized function, so do some stems. Some of these are:
1. Rhizomes – Horizontal stems that grow below the ground, usually near the surface of soil. EX - Irises, some grasses, some ferns
2. Runners and stolons -- Generally grow along the soil surface, above ground. EX – strawberries
3. Tubers – Produced by the accumulation of food at the tips of stolons. EX - Irish potatoes
4. Bulbs – Are actually large buds with a small stem at the lower end surrounded by fleshy leaves. EX – Onions, lilies, tulips
5. Corms – Similar to bulbs, with fewer fleshy leaves. EX – Crocus, gladiolus
C. Leaves
The main function for leaves on a plant is to carry out photosynthesis, an energy producing process in plants. Leaves receive water from roots via the stems.
Exterior Parts of a Leaf
Leaves may also protect flower buds (calyx); attach to objects (tendrils); and capture insects.
Leaf Arrangements on the Stem
(See page 115 in textbook)
Interior Structure of a Leaf
If we cut a leaf transversely and look at it under a microscope (and we will in a future lab session!) three distinct areas can be seen:
1. Epidermis : Single layer of cells that covers the entire leaf.
Epidermis on the "upper" side of a leaf – the side that faces the sun – has a waxy cuticle on it to prevent the leaf from drying out. This cuticle also prevents gas exchange from plant to atmosphere and vice versa.
However, the "lower" epidermis contains tiny pores, called stomata, through which gases can and do move in and out of the leaf. (Some plants have stomata on both sides, such as corn and alfalfa; some have stomata only on the upper surface, as water lilies. Some plants, like submerged underwater plants, lack stomata altogether.) These stomata range from 1,000 to 1.2 million per square centimeter of leaf surface. An average sunflower, such as we have in our ecosystem, can have 2 million stomata per leaf!
Each stomata is bordered by 2 small cells called guard cells. The guard cells regulate the opening and closing of stomata. When the guard cells are expanded by water, the swelling opens the stomata. When the amount of water decreases, the cells contract and close off the stomata, thus preventing any further loss of water.
2. Mesophyll
Most photosynthesis takes place here. Mesophyll has two regions:
3. Veins
Veins can be seen externally in leaves in a net-like pattern in dicots and in a parallel arrangement in monocots. Veins house the vascular bundles in leaves.
Specialized Leaves
1. Tendrils – climbing or clinging leaves. Seen in cucumbers, potatoes, squash, pumpkin
2. Spines, thorns and prickles – Reduces water loss in plants and protects from animals. Examples include mesquite and black locust trees
3. Storage leaves – These are modified leaves which can store water. Usually their parenchyma cells lack chlorophyll. Seen in succulent plants such as cacti.
4. Floral bracts – These are the "colored petals" of such flowers as the poinsettia and dogwood. The true "flower" is the small center portion of these arrangements.
5. Insect traps – Examples of these plants are the pitcher plant and Venus flycatcher.
REFERENCES
1. ----, The Way Nature Works, Macmillan. 1998.
2. Capon, Brian, Botany for Gardeners. Timber Press. 1990.
3. Mader, Sylvia S., Biology, 6th Edition McGraw-Hill. 1998.
4. Stern, Kingsley R., Introductory Plant Biology, 7th Edition. Wm. C. Brown Publishers. 1997