erived
from the Greek word for living together, symbiosis
refers to a close and prolonged association between 2 or
more organisms of different species that may last
for the lifetime of 1 or all partners. The
definition of symbiosis is not universally agreed upon;
in this review, it will be considered in its broadest
sense, encompassing associations varying widely in
intimacy and types of interaction. Symbioses can be
mutualistic (all partners benefiting), commensalistic
(one benefiting and the others unharmed), or parasitic,
although many symbiotic associations are complex or
poorly understood and do not fit neatly into 1 category
(1). A continuum can be envisioned that spans a dynamic
bridge from antagonism to cooperation. Relationships may
shift gradually or abruptly along the continuum (Figure
1). Many
pathogens and parasites clearly fulfill the definition of
symbiosis. Those of relatively low virulence (in most
healthy hosts), such as intestinal worms, herpesviruses, Chlamydia
bacteria, and Helicobacter pylori, may colonize a
host for much of the host's lifetime. Those of high
virulence can become symbiotic only if virulence is
limited to a subset of the host population or if there is
a long period before host death, as with HIV-1. An
asymptomatic carrier state, as in the case of some
hepatitis viruses, also allows a high pathogen to become
symbiotic with its host for much of the host's lifetime.
Commensal organisms are symbionts that are believed to
do little or no harm to the host and provide no benefits.
Examples include some of the hundreds of species of
bacteria colonizing the mouth and gastrointestinal tract.
Many bacteria, including tiny mycoplasmas, may be
commensals colonizing the skin and mucous membranes of
healthy persons. Tiny ectoparasites colonize the skin of
animals and usually do little or no harm.
It was thought until recently that the malaria
parasite was a commensal of mosquitoes, doing the insects
no harm. This presumption may be naive; a study has shown
that mosquitoes with malaria parasites bite more often
and more aggressively than they need to for their own
blood meal (2). Like many other hosts, the mosquitoes
appear to be manipulated by the parasites to behave in a
manner benefiting the parasite. Perhaps parasites don't
treat their vectors with kindness after all,
as we once thought.
At the opposite end of the spectrum from
pathogenicity, mutualisms are extraordinary in
their variety and ubiquity and will constitute the
principal kind of symbiosis covered in this review.
Where a symbiont settles along the continuum depends
on ever-changing variables. There is no
normal or abnormal place on the
continuum.
Symbiotic relationships exist everywhere we look; they
are beginning to seem like the very essence of biology.
They occur between the most distantly related organisms,
such as bacteria and eukaryotic cells, as well as between
closely related species, such as ants. Relationships
encompass all degrees of intimacy, from the tight
symbioses of mitochondria with their host eukaryotic
cells to the more loosely crafted partnerships between
entirely separate organisms. Examples covered in this
review range from marine invertebrates with their
symbiotic algae to the gastrointestinal tracts of animals
with their associated microbial symbionts.
CORALS AND OTHER MARINE INVERTEBRATES
Coral reefs, the most massive structures on earth
built by biological organisms other than humans, consist
of a foundation of limestone (calcium carbonate, or CaCO3)
laid down by a thin living veneer of coral tissue that
covers the surface (Figure
2) and by limestone from a few other reef
organisms, such as coralline algae. Eniwetok Atoll in the
Pacific was drilled to determine the thickness of the
limestone, and the drill entered basalt bedrock at a
depth of 1283 m, indicating a structural reef >1 km
tall atop volcanic bedrock. This finding confirmed the
subsidence theory, which states that a slowly sinking
island supports a reef that is limited in its upward
growth by the sea surface. Coral reefs exist over large
areas of shallow tropical seas; the Great Barrier Reef of
Australia extends continuously for >2000 km.
In complexity, the reef may have its closest
terrestrial counterpart in the tropical rain forest. Both
evoke an image of exuberant fertility and biomass, and
both depend on sunlight filtered down through a
stratified structure. Associations at successive levels
consist of organisms with needs matching the prevailing
illumination and shelter.
Reef construction is driven by photosynthesis. Most
reef-building corals are hosts to unicellular
photosynthetic algae that live inside their cells (Figure 3).
These algae are collectively called zooxanthellae,
a colorful term that has survived the winnowing influence
of a fastidious taxonomy. Zooxanthellae are mostly
dinoflagellate algae of a single genus, Symbiodinium,
and achieve striking concentrations of a million algal
cells per cm3 of coral tissue. The chloroplasts inside
the algae, once free-living cyanobacteria which
themselves have become symbionts, provide the service of
photosynthesis, making glucose, glycerol, and amino acids
which are useful to both the algal cell and the coral
host. These photosynthesizing algae, inside the very
cells of the coral, have been shown to be vital to the
high rates of calcification seen in reef-building corals.
Calcification rates on sunny days may be 2 to 3 times
higher than rates on cloudy days. Many corals can form
reefs only when they maintain a viable dinoflagellate
population in their tissues.
During the day, when the symbiotic algae are bathed in
sunlight, most reef-building corals keep their polyps
closed (Figure 4).
After dark they open their polyps and actively feed on
zooplankton, which are relatively scarce in tropical
waters.
In contrast to the cold, nutrient-rich waters of
higher latitudes, tropical waters are warm and buoyant,
tending not to sink to depth and be replaced by bottom
water. Sinking and replacement, called overturn, stirs up
bottom sediments and brings nutrients to the surface
waters, triggering plankton growth. Because overturn is
hindered in the tropics, the waters around coral reefs
are usually low in nutrient and plankton content and have
been called deserts.
Photosynthetic products from the symbiotic algae close
the nutrient gap (3). Symbionts may release virtually all
of these products to host tissues. This is often
sufficient to fuel the entire respiratory carbon
requirements of the host, making the coral independent of
the food sources available in the ambient water.
Under stressful conditions, such as unusually warm
water, coral bleaching may occur, in which
corals expel their algae and lose their green color (4).
The partnership is thus dynamic and provisional, the
coral host tolerating its partner only under stress-free
conditions. Bleaching may sometimes involve exchange of 1
algal type with another, a kind of choosiness on the part
of the coral enabling adaptation to a changing
environment.
Symbiodinium algae can live independently of
corals in seawater. When corals reproduce vegetatively
the algal symbionts spread with the growing coral, but
when corals reproduce sexually by broadcasting gametes
into the water, the algae are delivered in the eggs in
some species and obtained later from the seawater in
others, after dispersal from the parent colony.
Human activities are killing coral reefs around the
world by drowning them in freshwater runoff, pollution,
and sediment. Loss of coral reef habitat will have
potentially disastrous consequences for the conservation
of global biodiversity.
Single-celled algae enter into symbiotic relationships
with many other marine animals, including sea anemones,
jellyfish, soft corals, mollusks, and tunicates. Like
corals, the giant clam Tridacna, which can attain
a length of 1.5 m, may owe its huge size and rapid growth
to light-enhanced calcification. The marine world abounds
in symbiotic partnerships of great variety; the closer we
look, the more we find.
Lichens
Lichens grow in the leftover spots of the natural
world that are too harsh or limited for most other
organisms (Figure
5). They are pioneers on bare rock, lava
flows, cleared soil, dead wood, and newly emerged
volcanic islands in the sea. Capable of shutting down
metabolically under unfavorable conditions, they can
survive extremes of heat, cold, and drought.
With >=15,000 species, lichens are a successful
partnership between a fungus, on the one hand, and either
an algal or a cyanobacterial species on the other, and
sometimes both. The fungal partner usually constitutes
90% to 95% of the lichen biomass and encloses the cells
of the photosynthetic symbiont within a network of
filaments (Figure
6). The nonphotosynthetic fungus provides
a sturdy structure, while the algae and
cyanobacteria contribute the products of
photosynthesis; cyanobacteria also fix atmospheric
nitrogen and contribute this element to the partnership.
Over 500 species of lichens contain both algal and
cyanobacterial symbionts.
The thallus (leaflike or threadlike structure) of a
lichen forms only when the fungus encounters an algal or
cyanobacterial candidate; the developmental program is
present in the genome of the fungus, but without the
symbiont the genes remain turned off.
Lichens reproduce vegetatively by breaking off
particles, or soredia, composed of fungal threads and
algae. They also reproduce by spores produced in fruiting
bodies made by the fungus; when these spores germinate,
they must capture new algal or cyanobacterial cells to
form new lichens. They may even steal them
from other lichens.
Molecular studies show that lichens have evolved many
times, arising from parasitic, mutualistic, and
free-living fungi (5). The case for mutualism in some
lichens is supported by the finding that neither partner
by itself enjoys the same survival success in extreme
environments. Yet a free-living fungus may overtake a
colony of the cyanobacterium Nostoc and
incorporate it into a lichen; the fungal partner appears
to be parasitizing the bacterium. Some lichens thus
appear to be a case of controlled parasitism,
with the hostages providing a measured resistance but no
dramatic standoff. This interpretation could be changed,
however, if we discover that a chemical
dialogue between the 2 species initiates the
symbiosis.
A lesson to be learned from lichens is that neither
mutualism nor parasitism should be considered endpoints
in the evolution of symbiotic relations. As indicated
earlier, there is no normal or
abnormal point on the continuum.
Words such as cooperation,
partnership, and service have
been criticized as teleological, hinting of purpose. The
term service, for example, might be replaced
by the more scientific but cumbersome label
capability acquired by symbiosis. The choice
is arbitrary; the shorter terms are useful descriptive
shortcuts, as long as we understand their limitations and
explain that we are not imputing a goal or purpose.
Symbiotic partners are responding to each other only as a
part of their environment, no differently than a
free-living organism responds to its environment. Natural
selection moves genes into the future without consulting
a dictionary.
Lichens also present a challenge to our concept of individuality.
Is the lichen itself an individual organism or a
composite of 2 species? Do we view it as 1 or 2
organisms? The 2 partners can often be teased apart and
survive without the other in less harsh environments. Yet
lichens have been given scientific names, betraying our
bias toward individuality.
If natural selection acts fundamentally at the level
of genes, it also acts on a composite organism. One
lichen species, for example, may outcompete another.
CHEMOSYNTHESIS: TUBEWORMS IN HYDROTHERMAL VENT
ECOSYSTEMS
The mid ocean ridge system slices through the Pacific,
Atlantic, Indian, and Southern Oceans and is home to most
of the hydrothermal vent sites that have been studied.
Miles down, these strange ecosystems have been known only
since the 1970s.
Near ridge systems, cold, dense water on the ocean
floor percolates into the earth's crust and is heated by
magma just below the surface, making it less dense and
more buoyant. Now as hot as 400?C (752?F), the water
surges up through the sea floor into the deep ocean,
where the surrounding water is nearly freezing. Minerals
dissolved in the plume precipitate to form chimneys
called black smokers, which discharge thick
clouds of suspended minerals into the water. A thriving
community of animals surrounds the vent while it is
active; destined to cool eventually, the vent and its
living community will die. It behooves vent animals to
produce young which disperse regularly across the ocean
floor, where some will chance upon other vent ecosystems
during their ephemeral existence.
An extraordinary animal in these ecosystems is the
giant tubeworm, a 3-foot-long invertebrate housed in its
own 6-foot-tall tube and rooted near the black smokers.
As adults, these tubeworms have no mouth, gut, or anus,
obtaining all their energy and food from intracellular
symbiotic bacteria that live in the highly
vascularized tissue filling the bulk of their body
cavity. The worms have a unique hemoglobin in their blood
that binds oxygen and sulfide and transports both from
the surrounding seawater to the bacteria, which number a
billion cells per gram of worm tissue. Carbon isotope
data show that the tubeworms depend on carbon compounds
synthesized by the bacteria as the main source of their
nutrition (6).
The bioenergetics of the bacteria are as follows:
hydrogen sulfide plus oxygen yields sulfate plus energy.
The energy is utilized to synthesize organic molecules
from the carbon dioxide in vent water and seawater. The
key part of this energy equation is the oxidation of
sulfide to obtain energy; this is chemosynthesis
instead of photosynthesis. It achieves the same thing as
photosynthesis, making organic molecules out of carbon
dioxide, but gains energy from a chemical reaction
instead of from photons and captures carbon dioxide from
water instead of air.
The cozy picture we once had of hydrothermal vents as
warm oases in a frigid ocean has changed a bit. The vent
field is a harsh environment with shifting currents,
scalding water, near-freezing water, and water
alternately rich and poor in sulfide and oxygen. Changes
occur over seconds to hours. This makes it easier to
appreciate the real oasis found by the bacteria in the
protected bodies of the host tubeworms, where they enjoy
a stable shelter from thermal and chemical extremes, a
place where they won't be swept away into the rest of the
ocean, and a table to feast at, where a special variety
of hemoglobin delivers sulfide, oxygen, and carbon
dioxide right to their front door. It is not surprising
that the bacteria deliver attractive benefits to the
worms. As a result, we have a remarkable mutualism that
provides survival benefits to both parties in a harsh and
primitive environment with special dangers and
special resources.
Hydrothermal vent ecosystems are models of very old
and sheltered environments that may have been the least
perturbed places on earth during mass extinctions.
Asteroid impact, surface volcanism, and other causes of
mass extinctions may have left the vent biota alone. In
these migrating hotspots on the ocean floor, we may have
the ancestors of some of the earliest life forms.
Living closer to the sea surface, other marine
invertebrates such as bivalve mollusks have also
established symbioses with chemosynthetic bacteria, where
sulfide and oxygen are present in the water perfusing the
sediments. Sulfur-oxidizing epibacteria have been found
on nematodes living in marine sands, at the oxic-anoxic
interface; the nematodes appear to derive their nutrition
by feeding directly on their symbionts, and they track
the chemocline (chemical gradient in the water column) to
provide their symbionts with both sulfide and oxygen. The
closer we look at marine organisms, the more symbioses we
find, each one more strange than the last.
NITROGEN FIXATION
The nitrogen in proteins of every living thing comes
ultimately from thin air. Yet that freely circulating
dinitrogen molecule is glued together by a triple bond
that is nearly impossible to break, and it must be broken
for atmospheric nitrogen to become available to living
organisms.
Lightning provides a tiny amount of atomic nitrogen.
More is freed up by microorganisms that break down dead
organisms and their excreta. But a select few bacteria
have evolved the secret of how to pull it right out of
the air all the time, by means of nitrogenase
enzymes. These enzymes break the triple bond of N2
and allow reduction of nitrogen to ammonia, which is used
by plants to synthesize amino acids. Some of these
nitrogen-fixing bacteria form partnerships with green
plants, which provide them with a specialized shelter
called the root nodule. The nodule provides the
low-oxygen environment needed for reducing nitrogen to
ammonia.
The collective term rhizobia (from one of
their genera, Rhizobium) has been given to those
soil bacteria that form symbioses with most plants in the
legume family. Legumes include soybean, alfalfa, clover,
pea, peanut, mesquite, mimosa, and acacia (Figure 7);
with the help of symbiotic rhizobia in their root
nodules, most legumes can grow in poor soils without
addition of nitrogen-containing fertilizers.
A sprouting legume enters into a reciprocal
molecular conversation with soil rhizobia (7, 8). The
first step is the release of a molecular signal by the
legume, which induces a bacterial gene to synthesize a
morphogen. The morphogen triggers the formation of root
nodules in a narrow infection zone located just behind
the growing root tip. The bacteria invade these
developing nodules through infection threads laid
down by the plant (Figure
8). The 2 partners have coevolved in the
context of a mutualistic symbiosis, manipulating each
other with chemical signals. To the best of our knowledge
both partners derive benefits, natural selection having
favored reciprocal changes in both.
The plant host nevertheless regulates the infection
by means of feedback inhibition of nodulation. A mutant
legume that fails to regulate infection has been found,
and its roots are virtually taken over by the bacteria,
to the detriment of the plant.
Plants make their own oxygen, so it was surprising
when a hemoglobin was found in plants. The hemoglobin
found in root nodules of legumes is called leghemoglobin
(leg for legume); it is now believed that this
protein supplies oxygen to the bacteria while keeping it
away from the nitrogen-fixing machinery to which it is
toxic (9). Like hemoglobin, leghemoglobin is red, and
nodules are often pink when opened.
Rhizobia reproduce slowly for long periods in the
soil, but if they encounter a compatible legume they
begin to multiply rapidly; successful infection by a
single bacterium can initiate formation of a nodule
containing >10 million bacterial progeny. The root
nodule is like a lichen: it is a structure unique to the
symbiosis, formed only when the potential partners
encounter each other (10).
Rhizobia are the primary nitrogen fixers on land. In
the oceans the job is done mainly by an extraordinary
class of microorganisms that alone on earth perform both
photosynthesis and nitrogen fixation: cyanobacteria. It
is remarkable that a single organism can perform both
functions, because photosynthesis generates oxygen, and
nitrogen fixation must be carried out in a low-oxygen
environment. Cyanobacteria have specialized, walled-off
cells called heterocysts in which nitrogen fixation is
carried out.
Cyanobacteria also fix nitrogen inside leaf cavities
of the aquatic fern Azolla, which floats on the
water in our cypress swamps (Figure 9)
and has for centuries been added as green
manure to rice paddies in Asia; fish are often
added to these rice-Azolla systems and feed on the
Azolla. Azolla is also added to animal feed
as a protein supplement.
Occasional nitrogen-fixing symbioses occur between
bacteria and animals. Wood-feeding termites
provide a home for nitrogen-fixing bacteria in their
anaerobic hindgut and benefit from the ammonia synthesis
because the wood consumed by the termites is low in
nitrogen.
For high agricultural yields, we enrich soil with
still more nitrogen by adding nitrate in the form of
fertilizer or feces. In the 1800s whole cliffs of guano
were transported by sailing ships to New York from
islands where seabirds nested. Early methods for
synthesizing nitrate were motivated by its use in
gunpowder. In 1909 the Haber-Bosch process, which
harvests nitrogen right out of the air and converts it to
ammonia, revolutionized the agricultural world; this
process was nominated in a recent Nature
millennium essay as the most important invention of the
20th century. (An unmixed blessing? It has been estimated
that without the Haber-Bosch process almost two fifths of
the world's population would not be here.)
Vaclav Smil writes:
For several decades,
virtually all the fixed nitrogen added to the fields
of China, Egypt and Indonesia has come from synthetic
fertilizers. When you travel in Hunan or Jiangsu,
through the Nile Delta or the manicured landscapes of
Java, remember that the children running around or
leading docile water buffalo got their body proteins,
via the urea their parents spread on the fields, from
the Haber-Bosch synthesis of ammonia (11).
NEMATODE-BACTERIA SYMBIOSIS
Some tiny parasitic nematodes have evolved a
remarkable skill: they farm bacteria for food, using the
body (larva) of their parasitized insect host as the
soil in which to cultivate the bacteria. The
bacteria feed on the larva, killing it, and the nematodes
feed on the bacteria. The bacteria are both symbionts and
food and have never been found apart from their nematode
hosts.
The larval body is preserved from invasion by other
bacteria by antibacterial compounds produced by the
nematodes, to which its own symbiotic bacteria are
resistant.
When the nematodes reproduce, thousands of juveniles
leave to locate new larval hosts, carrying some of the
bacteria in their own gut.
The ability of these nematodes to kill insect larvae
has not been overlooked by the global agricultural
community (12, 13). Species from 2 genera of
insect-parasitic nematodes, Steinernema and Heterorhabditis,
are sprayed on crops around the world to control the
larvae of plant-eating insects and are valued as natural
biological pesticides.
LUMINESCENCE ORGANS
If you scuba dive in Hawaii at dusk, you might see
some tiny Hawaiian bobtail squid, only 1 1/2 inches long,
which emerge to forage as the light fades. If you were
beneath them looking up, you might lose sight of them
because their undersides glow dimly with the deep blue
light of millions of luminescent bacteria, housed in
special light organs. In the downwelling light from above
they are almost invisible to predators from below. The
bacteria providing this ventral bioluminescent
countershading, as it is called, glow with the colors
of moonlight and starlight.
A single Hawaiian bobtail squid maintains about a
billion cells of Vibrio fischeri, a gram-negative
luminous bacterium related to V. cholerae, in the
extracellular epithelial crypts of 2 light organs called
photophores, which branch out over the underside of the
squid. Shutters constructed of borrowed flaps of the ink
sac modulate the amount of light emitted by the light
organs.
Unlike our intestines, which shelter >400 species
of bacteria, the light organs of the squid use only 1
species of bacterial symbiont, which also exists as part
of the bacterioplankton. A baby squid hatches without the
symbionts but acquires them within hours from the
surrounding seawater. It accepts only 1 species,
rejecting all others offered to it in controlled
experiments. V. fischeri occurs as only about
0.001% of the bacteria in the water column, yet only this
particular species colonizes the light organs. The
juvenile squid has appendages covered with cilia that
waft the bacteria into the light organs, where they
multiply rapidly. Within hours, both the bacteria and the
squid undergo specific developmental changes in response
to the symbiosis: the bacteria begin to produce a high
level of bioluminescence (greater, in fact, than the
level that can be achieved by these cells in laboratory
culture) and the light organs begin to differentiate,
forming a lens and reflecting surface. After 4 days the
collecting structures undergo apoptosis and disappear.
This is a rare example of a specific body structure used
only for acquisition of symbionts, which regresses after
symbiosis is achieved (14).
Clearly the 2 organisms are communicating in
some way and are inducing changes in each other's gene
expression. This is reminiscent of the chemical
cross-talk between nitrogen-fixing bacteria and their
legume host, which provides the bacteria with an
infection thread. Also like legumes, the squid controls
overgrowth of its bacterial symbiont by elaborating an
antimicrobial protein and by dumping some of the bacteria
every morning.
The squid provides a nutrient-rich environment for
this heterotrophic bacterium, and the host acquires luminescence
rather than a nutritional benefit.
When foraging over sand in shallow water, where
twilight or moonlight provides light for predators
swimming above, bobtail squid carry a sand cover over the
top of their bodies, mimicking the substrate.
The luminous Vibrio bacteria elaborate a
substance which is believed to signal the squid to
provide nutrients. The chemical is related to the toxin
elaborated by their close relative V. cholerae. Does
cholera toxin, so lethal in mammalian hosts, represent a
bacterial signal gone wrong? Or was the gene co-opted to
code for a toxin that spreads cholera bacteria by means
of copious diarrhea, with host death a small price for
the bacteria to pay?
Luminescent bacteria provide many other hosts with the
gift of light (15). Examples include the following:
- Anglerfishes, deep-sea
predators throughout the world ocean, attract
prey in dimly lit waters with a lure; some lures
are brightly lit by bacterial symbionts.
- Flashlight fishes, plankton
feeders in shallow tropical waters, have large
suborbital light organs called photophores. They
use the light for several purposes: to see, to
communicate, to lure prey, and to confuse
predators. One species, Photoblepharon,
forms a galaxy of glowing lights on shallow reefs
in the Red Sea. The light organ of Photoblepharon
has a fold of skin that can be raised to block
light emission. A disturbed fish closes the light
organ and darts off, sometimes using a
blink-and-run tactic: light up on the zig, go
dark on the zag.
GASTROINTESTINAL "FLORA"
The final example of symbiosis is in many ways the
most remarkable--that between animals and the
microorganisms that live in their gut. The terms
flora and microflora are
misnomers, as gut microorganisms are not plants; yet the
terms are firmly established in biology and medicine.
The gastrointestinal tract is an ecosystem
maintained by both host and colonizing symbiotic
microorganisms. The latter, which enjoy a homeostatic
environment supplied with regular food, provide useful
services to their host in return: breakdown of cellulose
cell walls of plant food (especially important for strict
herbivores, but also important for omnivores like
humans), synthesis of vitamins (especially vitamin K),
development and maintenance of the gastrointestinal
mucosa and mucosal immune system, and protection against
enteric pathogens.
Approximately half of the contents of the human colon
is microbial biomass. This ecosystem is so complex that
it has been called an organ in itself, unique in that it
comprises billions of diverse cells engaged in anaerobic
fermentation. The cells are not our own but belong to
hundreds of species of microorganisms, yet they have
coevolved intimately with us and other animals in this
unique habitat.
The gut flora of vertebrates and invertebrates extends
across phyletic lines and represents one of the most
widespread and ancient of symbioses. In the evolution
of animals, these microbial symbionts enabled spectacular
evolutionary radiations based on dietary specializations.
Herbivores may specialize on grasses, leaves, or fruit;
meat-eaters on flesh, small invertebrates, or eggs;
omnivores on multiple food sources; and other specialists
on plankton, tree sap, wood, fungi, microorganisms, even
blood. This extraordinary diversity of food choices would
not be possible without gut microorganisms.
The most abundantly distributed carbohydrate in the
world is polysaccharide cellulose. Along with a few other
compounds cellulose forms the primary component of plant
cell walls. It is extremely insoluble and refractory to
chemical attack. Some invertebrates possess endogenous
cellulases, but even those that do usually require
microbial activity as well. No vertebrates have yet been
found with endogenous cellulases; this is a surprising
fact, in light of the reliance of so many vertebrates
upon plant material in their diet. The symbiotic gut
flora have taken center stage in releasing the protein
inside plant cells and breaking down cellulose to
energy-rich carbohydrates and short-chain fatty acids.
The term fermentation refers to the biochemical
pathway by which carbohydrates are broken down anaerobically,
using enzymes. The principal products of carbohydrate
fermentation are short-chain fatty acids (acetate,
propionate, and butyrate), which are important in
nutrition because they are a source of energy for
skeletal and cardiac muscle and the brain. The gut
microflora also synthesizes amino acids (from ammonia)
and protein, which are utilized by both the
microorganisms themselves and the host (16).
The 2 regions of the vertebrate gastrointestinal tract
that have undergone the most specialization for microbial
fermentation are the stomach and the large intestine
(including the cecum). Stomach fermenters are called
foregut fermenters; colon fermenters are
called hindgut fermenters.
Ruminants, which are foregut fermenters,
have a superior ability to convert cellulose into
digestible carbohydrates and short-chain fatty acids and
to free up the protein confined within cellulose cell
walls (Figure
10). Other animals can also break down
cellulose by virtue of their gut microflora, but
ruminants are masters at extracting the maximum yield
from a given amount of plant food. Much more fiber is
left undigested by a nonruminant, as can be seen by
comparing the coarse dung of a zebra, rhino, or elephant
with the fine-grained dung of any ruminant (17).
The rumination process is mechanically and
biochemically complex. The animal feeds until the rumen
is full, then settles down to ruminate, either lying or
standing, and chews the cud, which consists of the
coarsest plant particles. Rhythmic contractions of the
stomach stir the contents. Rumen microbes break down the
cellulose, later becoming a major source of protein for
the host as they pass through the digestive tract.
Ruminants can also recycle urea, thereby retaining
nitrogen which the bacteria use to synthesize the
essential amino acids that nonruminants must acquire from
their food. As an added bonus, recycling urea cuts down
on urine excretion, conserving water (17).
The ruminant esophagus is designed for controlled
regurgitation, as it is in other mammals and birds which
regurgitate food to feed their young. Methane and carbon
dioxide are produced continuously, and the
esophagogastric junction allows regular eructation,
without which the grazing ruminant would literally
explode. A cow can produce as much as a liter of gas per
minute; about half is methane, half carbon dioxide.
(Because methane and carbon dioxide are greenhouse gases,
eructation contributes to global warming.)
There is one drawback to rumination: if the protein
content falls to below 6%, the slow passage of food
through the ruminant gut precludes adequate nutrition.
The greater throughput of nonruminants allows
survival on low-protein food, simply by virtue of eating
more. A nonruminant like a zebra, for example, may
extract only two thirds as much protein from a given
quantity of food as a wildebeest (a ruminant), but by
processing twice as much in a given time, it will
assimilate four thirds that of a wildebeest (Figure 11).
The difference between ruminants and nonruminants can
be seen on the Serengeti Plains under hardship
conditions. Three mammal species make the annual
migration between the Ngorongoro Crater highlands in
Tanzania and the Masai Mara of Kenya: Burchell's zebras,
which (like horses) are nonruminants, and
wildebeests and Thomson's gazelles, which are ruminants.
When food is abundant but of low quality, such as an
expanse of tall, stringy grasses, zebras will typically
be found grazing those grasses (Figure 12),
as they can process a large quantity in a short time.
When food is scarce but of higher quality, such as short
green sprouts after a fire or the first rains,
wildebeests and gazelles are most efficient at obtaining
a maximum of nutrients from those sources, as the
rumination process allows recycling and thorough
extraction. At times a grazing succession is
seen, in which the zebras graze down the tall, dry grass
and the ruminants follow afterward and feed on the
exposed lower-story grasses.
Most herbivorous mammals are nonruminants, and
their principal site of microbial fermentation is usually
the hindgut instead of the stomach. Hippos are an
exception, with a complex, compartmentalized stomach with
diverticula. Hoatzins are leaf-eating birds with
elaborate foregut fermentation (18) (Figure 13a).
Many animals have a large cecum, which is a blind
pouch off of the large intestine (Figure 13b).
Birds often have paired ceca, with a complex morphology
adapted to different feeding ecologies (19). The cecum
provides a diversion away from the rapid mainstream
passage of digesta, where microorganisms can digest
cellulose more completely and synthesize vitamins and
proteins and where nutrients can be absorbed. The cecum
may enable some animals to switch between insect and
plant foods, exploiting unpredictable environments.
Most meat-eating mammals have an amazingly
simple gut when compared with herbivores. The
stomach is simple and the colon unspecialized. A long
small intestine is adapted to the readily digested animal
food and is the major site of absorption of animal
proteins, carbohydrates, and fats. Insect-eaters also
have a relatively simple and unspecialized gut. Even in
carnivores such as foxes, bears, and raccoons, which
include fruits and other plant material in their diet,
the gut anatomy continues to reflect the easily digested
animal food.
The human gastrointestinal tract (Figure 13c)
is intermediate between that of herbivores and
carnivores, with a simple stomach, unremarkable length of
small intestine, small cecum, and a moderately large
colon where fermentation of plant material takes place.
Humans and apes are believed to have evolved from a
common plant-eating ancestor; humans added animal protein
to their diet, reaping nutritional advantages enjoyed by
carnivores while retaining some features of digestive
anatomy characteristic of herbivores (20, 21).
The small bowel normally contains few microorganisms.
Jejunal cultures fail to identify any bacterial growth in
about one third of healthy human volunteers. A dramatic
change in the enteric flora occurs across the ileocecal
valve, where the number of microorganisms explodes upward
to 109 to 1012 organisms per gram
of colonic contents, constituting up to 50% of fecal
matter by weight. In intestinal stasis, the bacterial
count rises even higher. Forty genera of bacteria,
represented by at least 400 species, can be cultured from
the feces of a healthy human.
An ecosystem with >400 species of bacteria, plus
protists and fungi, constitutes a jungle of competitive
species and individuals. Some species are mutualists,
others commensals, still others potential pathogens. The
species composition of this jungle changes remarkably
little over the life of a healthy host.
The mouth is part of the gastrointestinal tract, and
its microbial diversity is no less extraordinary. Many
species are thought to be commensals, and a small number
are opportunistic pathogens. Dental caries, gingivitis,
and periodontitis are thought to be caused in part by
opportunistic bacteria. Nearly 500 bacterial strains have
been recovered from just beneath the gums, a well-studied
microbial niche (22).
At birth the human alimentary canal is sterile, like
that of animals raised in a germ-free environment.
Enteric bacteria colonize the newborn infant in an
oral-to-anal direction. About 3 or 4 weeks after
birth the flora characteristic for the individual host is
fairly well established and, except under unusual
circumstances, does not change significantly thereafter.
Studies with germ-free newborn animals show that the
indigenous bacterial flora is essential for the
completion of intestinal epithelial cell differentiation
and the maturation of the mucosal immune system.
The normal gastrointestinal flora can be disturbed by
illness, ingestion of pathogens, and antibiotic
administration. Diarrheal diseases and colitis may be
accompanied by an overgrowth of species such as Clostridium
difficile or Escherichia coli, present in
smaller numbers in the normal flora. Overgrowth of some
species may also result in malabsorption syndromes.
Paradoxically, overgrowth of some components of the
colonic flora may result in competitive uptake of vitamin
B12 by bacteria, interfering with absorption
of the vitamin by the intestinal mucosa (23).
An exceptional gut symbiont, present in at least half
the human population, may be friend or foe: Helicobacter
pylori. This bacterium lives for decades in the
extreme environment of the stomach and is responsible for
one of the most widespread chronic bacterial infections
known in humans (24). H. pylori infection is a
serious, chronic, transmissible infectious disease in
which clinical illness follows a long asymptomatic
interval, usually of many years. Infection typically
begins in childhood and illness appears in adulthood,
often late in life. H. pylori is believed to play
a causative role in most duodenal and gastric ulcers and
is associated with chronic gastritis and an increased
risk of gastric adenocarcinoma. Yet it elaborates an
antibiotic which may help control colonization of the gut
by foreign microbes. The great genetic variability of H.
pylori, with its tendency to exchange genetic
information among strains, makes it difficult for us to
assign it a place on the continuum; there is probably
considerable host variability as well.
Is the normal intestinal flora ever highly pathogenic?
In the case of colon perforation, as from a penetrating
abdominal wound, the answer is clearly yes. A balanced
mix of microbial species then responds to a new
environment, some multiplying as high pathogens at the
opposite end of the spectrum.
CONCLUSION
Symbioses are everywhere we look in nature, usually
between organisms far removed from each other
phylogenetically. Unlike adaptation to the nonliving
environment, adaptation to another species can produce
reciprocal evolutionary responses that either thwart or
reinforce the adaptation. Interactions move dynamically
along the continuum in either direction, toward or away
from mutualism.
Some symbioses are more intimate than others. Some are
intracellular, some are extracellular, and still others
occur between separate partners. Some symbioses are
facultative, others obligate, and this characteristic may
change through the life cycle of the host.
Our tentative assignment of a relationship to a place
on the continuum is subject to regular change as we learn
more. Often the interactions are too poorly known or too
complex to allow a precise assignment. Mutualisms, for
example, may not be perfectly egalitarian; a
fluctuating asymmetry in the provision of benefits is
probably typical. As new symbioses are discovered, an
understanding of one partner requires an understanding of
the other and of their joint evolutionary history.
An Economics 101 model for mutualisms has
been proposed: if a species is especially good at
acquiring a resource, it may pay to specialize in that
resource and trade for a second. Two unrelated species
may thus collaborate in a partnership that provides the
best of both worlds.
The biologist Daniel Janzen has asked: Are mutualisms
delicately balanced antagonisms? Do they represent
reciprocal parasitisms, that is,
mutually exploitative interactions with underlying
conflicts of interest? If genes are selfish,
are partners of a mutualism also fundamentally selfish?
We can use any terms we choose, as long as we understand
that natural selection is moving genes into the future
differentially, just as with nonsymbiotic organisms.
Most terms we use will probably have an anthropomorphic
slant.
Functions (services) provided by one
partner, discussed in this review, include the following:
- Photosynthesis
- Chemosynthesis
- Nitrogen fixation
- Luminescence
- Nutrition (gut
flora--cellulose breakdown, vitamins, maintenance
of intestinal ecosystem)
A future review will expand the coverage of this
article to include mitochondria, chloroplasts, microbial
pathogens symbiotic with humans, and partnerships between
entirely separate organisms, such as ants and plants,
ants and fungi, one ant species and another, and plants
and their pollinators.
John Donne wrote, No man is an island. It
appears that most other organisms aren't either but
instead weave intimate and complex tapestries with other
life forms.
Acknowledgments
Miriam Muallem, librarian at Medical City Dallas
Hospital, provided invaluable help and guidance with
reference material; Judith L. Bronstein offered important
insights into evolutionary aspects of mutualisms; Richard
D. Estes provided data on mammalian digestive strategies;
and Mary Beth Dimijian and William S. Woodfin, MD,
provided valuable editing advice.
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