Plants are a major group of life forms and include familiar
organisms such as trees, herbs,
bushes, grasses, vines,
ferns, mosses, and green algae. About
350,000 species of plants, defined as seed plants,
bryophytes, ferns and fern
allies, are estimated to exist currently. As of 2004, some 287,655 species had been identified, of which 258,650 are
flowering and 15,000 bryophytes. Green plants,
sometimes called metaphytes, obtain most of their energy from sunlight
via a process called photosynthesis.
Definition
Aristotle divided all living things between plants (which generally do not move), and
animals (which often are mobile to catch their food). In Linnaeus' system, these became
the Kingdoms Vegetabilia (later Metaphyta or Plantae)
and Animalia (also called Metazoa). Since then, it has become clear that the Plantae as originally defined included
several unrelated groups, and the fungi and several groups of algae were removed to new kingdoms. However, these are still often considered plants in many contexts, both
technical and popular. Indeed, an attempt to perfectly match "plant" with a single taxon is
problematic, because for most people the term "plant" is only vaguely related to the phylogenic concepts on which modern taxonomy and systematics are based.
When the name Plantae is applied to a specific taxon, it is usually referring to one of three concepts. From smallest to
largest in inclusiveness, these three groupings are:
- Land plants, also known as Embryophyta or
Metaphyta. As the narrowest of plant categories, this is further delineated below.
- Green plants -- also known as Viridiplantae, Viridiphyta or Chlorobionta -- comprise the above
Embryophytes, Charophyta (i.e., primitive stoneworts), and
Chlorophyta (i.e., green algae such as sea lettuce). It is this clade which is mainly the subject of this
article.
- Primoplantae -- also known as Plantae sensu
lato, Plastida, or Archaeplastida -- comprises
the green plants above, Rhodophyta (red algae) and
Glaucophyta (simple glaucophyte algae). As the broadest
plant clade, this comprises most of the eukaryotes that eons
ago acquired their chloroplasts directly by engulfing cyanobacteria.
Informally, other creatures that carry out photosynthesis are called plants as well, but they do not constitute a formal taxon
and represent species that are not closely related to true plants. There are around about 375,000 species (types) of plants, and
each year more are found and described by science.
Algae
-
The algae comprise several different groups of organisms that produce energy through
photosynthesis. However, most are not classified within the Kingdom Plantae but in the Kingdom Protista. Most conspicuous are the seaweeds, multicellular algae that may
roughly resemble terrestrial plants, but are classified among the green, red, and brown algae. These and other algal groups also include various
single-celled organisms.
The embryophytes developed from green algae (Chlorophyta); the two groups are
collectively referred to as the green plants or Viridiplantae. The Kingdom Plantae is often taken to mean this monophyletic grouping. With a few exceptions among the green algae, all such forms have cell walls containing
cellulose and chloroplasts containing chlorophylls a and b, and store food in the form of starch.
They undergo closed mitosis without centrioles, and typically
have mitochondria with flat cristae.
The chloroplasts of green plants are surrounded by two membranes, suggesting they
originated directly from endosymbiotic cyanobacteria. The same is true of the
red algae, and the two groups are generally believed to have a common origin (see
Archaeplastida). In contrast, most other algae have chloroplasts with three or four
membranes. They are not close relatives of the green plants, presumably in origin acquiring chloroplasts separately from ingested
or symbiotic green and red algae.
Fungi
-
Fungi are no longer considered to be plants, though they were previously included in the plant
kingdom. Unlike embryophytes and algae, fungi are not photosynthetic, but are saprotrophs:
obtaining food by breaking down and absorbing surrounding materials. Fungi are not plants, but were historically treated as
closely related to plants, and were considered to be in the purview of botanists. It has long been recognized that fungi are
evolutionarily closer to animals than to plants, but they still are covered more in depth in introductory botany courses and are
not necessarily touched upon in introductory zoology courses. Most fungi are formed by microscopic structures called
hyphae, which may or may not be divided into cells but contain eukaryotic nuclei. Fruiting bodies, of which mushrooms are most familiar, are the reproductive structures of fungi. They are not related to any of the
photosynthetic groups, but are close relatives of animals. Therefore, the
fungi are in a kingdom of their own.
Diversity
About 350,000 species of plants, defined as seed
plants, bryophytes, ferns and fern allies, are estimated to exist currently. As of 2004, some 287,655 species had been identified, of which
258,650 are flowering plants, 16,000 bryophytes,
11,000 ferns and 8,000 green algae.
Diversity of living plant divisions
| Informal group |
Division name |
Common name |
No. of living species |
| Green algae |
Chlorophyta |
green algae (chlorophytes) |
3,800 [2] |
| Charophyta |
green algae (desmids &
charophytes) |
4,000 - 6,000 [3] |
| Bryophytes |
Marchantiophyta |
liverworts |
6,000 - 8,000 [4] |
| Anthocerotophyta |
hornworts |
100 - 200 [5] |
| Bryophyta |
mosses |
10,000 [6] |
| Pteridophytes |
Lycopodiophyta |
club mosses |
1,200 [7] |
| Pteridophyta |
ferns, whisk ferns & horsetails |
11,000 [7] |
| Seed plants |
Cycadophyta |
cycads |
160 [8] |
| Ginkgophyta |
ginkgo |
1 [9] |
| Pinophyta |
conifers |
630 [7] |
| Gnetophyta |
gnetophytes |
70 [7] |
| Magnoliophyta |
flowering plants |
258,650 [10] |
Phylogeny
A proposed phylogeny of the Plantae after Kenrick and Crane[11] is as follows, with modification to the Pteridophyta from Smith et al.[12] The Prasinophyceae may be a
paraphyletic basal group to all green plants.
Embryophytes
-
Most familiar are the multicellular land plants, called embryophytes. They include the vascular plants, plants with full
systems of leaves, stems, and roots. They also include a few of their close relatives, often called bryophytes, of which mosses and liverworts are the most common.
All of these plants have eukaryotic cells with cell
walls composed of cellulose, and most obtain their energy through photosynthesis, using light and carbon
dioxide to synthesize food. About three hundred plant species do not photosynthesize but are parasites on other species of photosynthetic plants. Plants are distinguished from green algae, which represent a mode of photosynthetic life similar to the kind modern plants are believed to
have evolved from, by having specialized reproductive organs protected by non-reproductive tissues.
Bryophytes first appeared during the early Palaeozoic. They can only survive where moisture
is available for significant periods, although some species are desiccation tolerant. Most species of bryophyte remain small
throughout their life-cycle. This involves an alternation between two generations: a haploid
stage, called the gametophyte, and a diploid stage, called
the sporophyte. The sporophyte is short-lived and remains dependent on its parent
gametophyte.
Vascular plants first appeared during the Silurian period, and by the Devonian had diversified and spread into many different land environments. They have a number of adaptations
that allowed them to overcome the limitations of the bryophytes. These include a cuticle resistant to desiccation, and vascular
tissues which transport water throughout the organism. In most the sporophyte acts as a separate individual, while the
gametophyte remains small.
The first primitive seed plants, Pteridosperms (seed ferns) and Cordaites, both groups now extinct, appeared in the late
Devonian and diversified through the Carboniferous, with further evolution through the Permian
and Triassic periods. In these the gametophyte stage is completely reduced, and the sporophyte
begins life inside an enclosure called a seed, which develops while on the parent plant, and with
fertilisation by means of pollen grains. Whereas other vascular plants, such as ferns, reproduce
by means of spores and so need moisture to develop, some seed plants can survive and reproduce in extremely arid conditions.
Early seed plants are referred to as gymnosperms (naked seeds), as the seed embryo is not enclosed in a protective structure
at pollination, with the pollen landing directly on the embryo. Four surviving groups remain widespread now, particularly the
conifers, which are dominant trees in several biomes. The angiosperms, comprising the flowering plants, were the last
major group of plants to appear, emerging from within the gymnosperms during the Jurassic and
diversifying rapidly during the Cretaceous. These differ in that the seed embryo (angiosperm)
is enclosed, so the pollen has to grow a tube to penetrate the protective seed coat; they are the predominant group of flora in
most biomes today.
Fossils
-
Plant fossils include roots, wood, leaves, seeds, fruit, pollen, spores, phytoliths, and
amber (the fossilized resin produced by some plants). Fossil land plants are
recorded in terrestrial, lacustrine, fluvial and nearshore marine sediments. Pollen,
spores and algae (dinoflagellates and acritarchs) are used for dating sedimentary rock sequences. The remains of fossil plants are not as common as
fossil animals, although plant fossils are locally abundant in many regions worldwide.
The earliest fossils clearly assignable to Kingdom Plantae are fossil green algae from the Cambrian. These fossils resemble calcified multicellular members of the Dasycladales. Earlier Precambrian fossils are known which resemble
single-cell green algae, but definitive identity with that group of algae is uncertain.
The oldest known trace fossils of embryophytes date from the Ordovician, though such fossils are fragmentary. By the Silurian, fossils
of whole plants are preserved, including the lycophyte Baragwanathia longifolia. From the Devonian, detailed fossils of rhyniophytes have been found. Early fossils of these ancient plants show the individual cells within the
plant tissue. The Devonian period also saw the evolution of what many believe to be the first
modern tree, Archaeopteris. This fern-like tree combined a woody trunk with the
fronds of a fern, but produced no seeds.
The Coal Measures are a major source of Palaeozoic
plant fossils, with many groups of plants in existence at this time. The spoil heaps of coal mines are the best places to
collect; coal itself is the remains of fossilised plants, though structural detail of the plant
fossils is rarely visible in coal. In the Fossil Forest at Victoria Park in Glasgow,
Scotland, the stumps of Lepidodendron trees are
found in their original growth positions.
The fossilized remains of conifer and angiosperm roots, stems and branches may be locally abundant in lake and inshore
sedimentary rocks from the Mesozoic and Caenozoic eras.
Sequoia and its allies, magnolia, oak, and palms are often found.
Petrified wood is common in some parts of the world, and is most frequently found in
arid or desert areas where it is more readily exposed by erosion. Petrified wood is often
heavily silicified (the organic material replaced by silicon dioxide), and the
impregnated tissue is often preserved in fine detail. Such specimens may be cut and polished using lapidary equipment. Fossil forests of petrified wood have been found in all continents.
Fossils of seed ferns such as Glossopteris are widely distributed throughout
several continents of the southern hemisphere, a fact that gave support to
Alfred Wegener's early ideas regarding Continental
drift theory.
Life processes
Growth
Most of the solid material in a plant is taken from the atmosphere. Through a process known as photosynthesis, plants use the energy in sunlight to
convert carbon dioxide from the atmosphere into simple sugars. These sugars are then used as
building blocks and form the main structural component of the plant. Plants rely on soil primarily for support and water (in
quantitative terms), but also obtain nitrogen, phosphorus
and other crucial elemental nutrients. For the majority of plants to grow successfully they also require oxygen in the atmosphere
(for respiration in the dark) and oxygen around their roots. However, a few specialized vascular plants, such as Mangroves, can grow with their roots in anoxic conditions.
Factors affecting growth
The genotype of a plant affects its growth, for example selected varieties of wheat grow rapidly, maturing within 110 days,
whereas others, in the same environmental conditions, grow more slowly and mature within 155 days.[13]
Growth is also determined by environmental factors, such as temperature, available
water, available light, and available
nutrients in the soil. Any change in the availability of these external conditions will be
reflected in the plants growth.
Biotic factors (living organisms) also affect plant growth.
- Plants compete with other plants for space, water, light and nutrients. Plants can be so crowded that no single individual
makes normal growth.[13]
- Many plants rely on birds and insects to affect pollination.
- Grazing animals may completely affect vegetation.
- Soil fertility is influenced by the activity of bacteria and fungi.
- Bacteria, fungi, viruses, nematodes and insects can parasitise plants.
- Some plant roots require an association with fungi to maintain normal activity (mycorrhizal association).[13]
Simple plants like algae may have short life spans as individuals, but their populations are commonly seasonal. Other plants
may be organized according to their seasonal growth pattern:
- Annual: live and reproduce within one growing season.
- Biennial: live for two growing seasons; usually reproduce in second year.
- Perennial: live for many growing seasons; continue to reproduce once mature.
Among the vascular plants, perennials include both evergreens that keep their leaves the
entire year, and deciduous plants which lose their leaves for some part. In temperate and boreal climates, they generally lose their leaves during the
winter; many tropical plants lose their leaves during the dry season.
The growth rate of plants is extremely variable. Some mosses grow less than 0.001 mm/h, while most trees grow 0.025-0.250
mm/h. Some climbing species, such as kudzu, which do not need to produce thick supportive tissue,
may grow up to 12.5 mm/h.
Plants protect themselves from frost and dehydration
stress with antifreeze proteins, heat-shock
proteins and sugars (sucrose is common). LEA (Late Embryogenesis Abundant) protein expression is induced by stresses and protects other proteins from
aggregation as a result of desiccation and freezing.[14]
Internal distribution
Photographs showing
xylem elements in the shoot of a
fig tree
(
Ficus alba): crushed in
hydrochloric acid, between slides and cover
slips.
Nutrients and water from the soil and the organic compound produces in leaves are
distributed to specific areas in the plant through the xylem and phloem. The xylem draws water and nutrients up from the roots to the upper sections of the plant's body, and the
phloem conducts other materials, such as the glucose produced during photosynthesis, which gives the plant energy to keep growing and seeding.
The xylem consists of tracheids, which are dead hard-walled cells arranged to form tiny
tubes to function in water transport. A tracheid cell wall usually contains the polymer lignin.
The phloem however consists of living cells called sieve-tube members. Between the
sieve-tube members are sieve plates, which have pores to allow molecules to pass through. Sieve-tube members lack such organs as
nuclei or ribosomes, but cells next to them, the companion cells, function to keep the sieve-tube members alive.
Movement of nutrients, water, sugars and waste is effected by transpiration, conduction and absorption.
Transpiration
The most abundant compound in most plants is water, serving a large role in the various processes taking place. Transpiration is the main process a plant can call upon to move compounds within its tissues. The basic
minerals and nutrients a plant is composed of remain, generally, within the plant. Water, however, is constantly being lost from
the plant through its metabolic and photosynthetic
processes to the atmosphere.
Water is transpired from the plants leaves via stomata, carried there via leaf veins and vascular bundles within the plants cambium layer. The movement of water
out of the leaf stomata creates, when the leaves are considered collectively, a transpiration pull. The pull is created through
water surface tension within the plant cells. The draw of water upwards is assisted by
the movement of water into the roots via osmosis. This process also assists the plant in
absorbing nutrients from the soil as soluble salts, a process known as absorption.
Absorption
Xylem cells move water and nutrient solutions upwards towards other plant organs from the roots and fine root hairs. Living roots cells actively
absorb water in the absence of transpiration pull via osmosis creating root pressure. There are times when plants do not have
transpiration pull, usually due to lack of light or other environmental elements. Water in the plant tissues may move to the
roots to assist in passive absorption.
Conduction
Xylem and phloem tissues are involved in the conduction
processes within plants. The movement of foods throughout the plant takes place mainly in the phloem. Plant conduction (food
movement) is from an area of high food content, place of manufacture (photosynthesis) or
storage, to a place of food utilisation, or from a point of manufacture to storage tissues. Mineral salts are translocated in the
xylem tissues.[13]
Ecology
-
The photosynthesis conducted by land plants and algae is the ultimate source of energy
and organic material in nearly all ecosystems. Photosynthesis radically changed the composition of the early Earth's atmosphere,
which as a result is now 21% oxygen. Animals and most other organisms are aerobic, relying on oxygen; those that do not are confined to relatively rare anaerobic environments. Plants are the primary producers in
most terrestrial ecosystems and form the basis of the food web in those ecosystems. Many
animals rely on plants for shelter as well as oxygen and food.
Land plants are key components of the water cycle and several other biogeochemical cycles. Some plants have coevolved with
nitrogen fixing bacteria, making plants an important part of the nitrogen cycle. Plant roots play an essential role in soil development and
prevention of soil erosion.
Distribution
Plants are distributed worldwide in varying numbers. While
they inhabit a multitude of biomes and ecoregions, few can be
found beyond the tundras at the northernmost regions of continental shelves. At the southern extremes, plants have adapted tenaciously to the prevailing
conditions. (See Antarctic flora.)
Plants are often the dominant physical and structural component of habitats where they occur. Many of the Earth's
biomes are named for the type of vegetation because plants are the dominant organisms in those
biomes, such as grasslands and forests.
Ecological relationships
Numerous animals have coevolved with plants. Many animals pollinate flowers in exchange for food in the form of pollen or nectar. Many animals
disperse seeds, often by eating fruit and passing
the seeds in their feces. Myrmecophytes are plants that have coevolved with
ants. The plant provides a home, and sometimes food, for the ants. In exchange, the ants defend the
plant from herbivores and sometimes competing plants. Ant wastes provide organic
fertilizer.
The majority of plant species have various kinds of fungi associated with their root systems in a kind of mutualistic symbiosis known as mycorrhiza. The fungi help the plants gain water and mineral nutrients from the soil, while the plant gives
the fungi carbohydrates manufactured in photosynthesis. Some plants serve as homes for endophytic fungi that protect the plant from herbivores by producing toxins. The fungal endophyte,
Neotyphodium coenophialum, in tall fescue (Festuca arundinacea) does tremendous economic damage to the cattle
industry in the U.S.
Various forms of parasitism are also fairly common among plants, from the semi-parasitic mistletoe that merely takes some nutrients from its host, but still has photosynthetic leaves, to the fully
parasitic