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Plant Physiol, March 2001, Vol. 125, pp. 1198-1205
UPDATE ON EVOLUTION
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INTRODUCTION |
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While some scientists have been
working to sequence and describe the human genome, with increasingly
dramatic results, another set of scientists has been quietly providing
a map of evolutionary history, a time line that shows how life has
evolved. Unlike the genome projects, which accumulate megabases of
sequence from many genes in one organism, evolutionary projects
accumulate megabases of sequence from the same handful of genes in many
organisms. The scientists who investigate the pattern of evolutionary
change are predominantly systematists, meaning, literally, those who study natural systems. Their work has three major goals. The first is
to decipher the evolutionary history, or phylogeny, commonly drawn as a
cladogram or branching diagram. Once that is accomplished, the second
goal is to determine for each speciation event what sorts of changes
must have occurred. The phylogeny allows us to define, for any point in
time, what characteristics were ancestral (analogous to "wild
type") and which were derived (analogous to "mutant"). If two
species have a particular characteristic, such as white flowers or
hairy leaves, then their ancestor is assumed to have had the same
characteristic. If two species had different characteristics, then we
look to their next closest relative to help determine the ancestral
condition. This sort of deduction is based on assumptions about the
likelihood of change and provides a hypothesis of evolutionary pattern,
which can in some cases then be tested experimentally. The third goal
of systematics is to create a formal classification that reflects
history. There are many ways to convert an evolutionary tree into a
hierarchical classification. The only hard and fast rule is that any
named group should include all the descendants of a particular
ancestor, i.e. should be a monophyletic group. This distinction between determining history and producing a classification is relatively recent. Until the last part of the 20th century,
classifications were assumed to represent history, and the two
investigations were conflated (Stevens, 1994
).
To determine the evolutionary history of a group of organisms, systematists have traditionally used morphological characteristics, which are often difficult to study and require extensive developmental and anatomical investigation to establish appropriate comparisons. Because of the difficulties inherent in studying form, many systematists now use DNA sequences to determine relationships among organisms. If large enough stretches of DNA can be compared for enough organisms, the phylogenetic relationships generally become clear. The need for large numbers of DNA sequences has led to collaborative groups of scientists who combine their data to reach a common goal. This is an unusual endeavor for systematists who traditionally have worked alone, each investigating a single group of organisms.
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EVOLUTIONARY TREE OF THE GRASS FAMILY (POACEAE OR GRAMINEAE) |
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The grass family is of particular interest to humans. Most people
on earth rely on grasses, including rice, wheat, and maize, for a major
portion of their diet. Domestic animals are raised on diets partly or
wholly of grasses. In addition, grasses form an important part of the
urban and suburban landscape in much of the world. Members of the
family also are ecological dominants, covering approximately 20% of
the earth's land surface (Shantz, 1954
).
The grass family includes approximately 10,000 species classified into
600 to 700 genera (Clayton and Renvoize, 1986
; Watson and Dallwitz,
1999
). The grasses are included with lilies, orchids, pineapples, and
palms in the group known as the monocotyledons, which includes all
flowering plants with a single seed leaf.
In the last couple of years, a clear picture has formed of the
evolutionary history of the grass family. This comes from
restriction site maps of the chloroplast genome (Soreng and Davis,
1998
), sequences of chloroplast genes, including ndhF (Clark
et al., 1995
), rpoC2 (Barker et al., 1999
), rbcL
(Barker et al., 1995
), matK (Hilu et al., 1999
),
rps4 (Nadot et al., 1994
), and sequences of several nuclear
genes, including phytochrome B (Mathews et al., 2000
), GBSSI
(Mason-Gamer et al., 1998
), ITS (Hsiao et al., 1999
), and 18S rDNA
(Hamby and Zimmer, 1988
). Although some of these studies have been
hampered by small sample sizes or insufficient numbers of variable
bases, all have reached similar conclusions about the order of events
in the evolution of the grasses. The data from seven of
these sources have been combined by a consortium of 13 researchers, who have called themselves the Grass Phylogeny Working
Group (GPWG; www.virtualherbarium.org/GPWG/), and have produced a
phylogeny (summarized in Fig. 1; see also
Fig. 2; GPWG, 2000). This picture of the
evolutionary history is strongly supported by bootstrap and decay
analyses, statistics that measure the extent to which the data support
the tree topology.
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The GPWG chose 59 representative species for study of the phylogeny.
These were chosen to represent all known major groups, plus a set of
species whose relationships were unknown. We took advantage of earlier
investigations that had studied sets of morphological characters across
hundreds of species. For example, the Russian cytogeneticist Avdulov
(1931)
reported on chromosome number and karyotype of many hundreds of
grasses and found that a large group of temperate grasses had much
larger chromosomes than other grasses, and fewer of them, with a base
number of x = 7. This group includes such familiar
species as wheat (Triticum), barley (Hordeum),
rye (Secale), and oats (Avena), as well as most
north temperate lawn and pasture grasses. The French anatomist Prat
(1932)
looked at the shape and structure of epidermal cells and found
that the subsidiary cells of the stomata in Avdulov's
x = 7 group have outer walls that are parallel rather
than curved. This group, defined by cytological and anatomical
characteristics, has also been found to represent a single lineage in
every DNA study to date (for summary, see Kellogg, 1998
; GPWG, 2000).
The GPWG therefore decided to represent it by only three genera,
Avena, Bromus, and Triticum, but it
includes also barley, rye, and all the cool season grasses commonly
placed in subfamily Pooideae.
The phylogeny correlates well with information from mapping of the
nuclear genome (Kellogg, 1998
). In the nuclear genome, genes are in a
similar order in all grasses (Gale and Devos, 1998
). Thus whole
chromosomes of rice can be lined up with chromosomes of wheat or maize.
Major re-arrangements have occurred, however, among blocks of linked
genes, and these correlate with the phylogeny. For example, in the
panicoid grasses maize (Zea), sugar cane
(Saccharum), sorghum (Sorghum), pearl millet
(Pennisetum), and foxtail millet (Setaria), the
linkage group corresponding to rice chromosome 10 is inserted into the
middle of what had been rice chromosome 3. The centromere of 3 is
apparently replaced by the centromere of 10, which is now the
centromere for the entire combined chromosome. Rice chromosome 9, similarly, has been inserted in rice 7. Other re-arrangements have
occurred in the subfamily Pooideae (Fig. 1), correlating with the
change in chromosome number to x = 7 and a marked
increase in genome size (Bennetzen and Kellogg, 1997
).
From the phylogeny, the GPWG has produced a revised classification, shown in part in Figure 1.
Names of plants are governed by the International Code of
Botanical Nomenclature
(http://www.bgbm.fu-berlin.de/iapt/nomenclature/code/default.htm), analogous to the standards developed for Arabidopsis or maize gene nomenclature (Meinke and Koornneef, 1997
) at
http://www.agron.missouri.edu/maize nomenclature.html#1996UPDATES
(Beavis et al., 1995
). All species must be placed in a genus, so a
species name consists of the familiar binomial. Genera are then
assembled into families, and the families are assembled into orders.
For convenience, a large family may be divided into subfamilies,
subfamilies into tribes, and tribes into subtribes. All these
intermediate ranks are used in the grass family because it is so big.
Subfamily names conventionally end in -oideae, tribes in -eae, and
subtribes in -inae. Some taxonomists are suggesting that a ranked
classification should be dropped as it may be cumbersome and confusing,
but this proposal has not yet received wide support.
Previous classifications were created using only characters that could be observed on pressed dried specimens. Molecular data have shown that some groups so delimited were accurate in reflecting evolutionary history, but some changes have been necessary.
Each group with a name is required to represent only a single lineage.
Given that criterion, we tried to make the named subfamilies as similar
as possible to those that previous workers had recognized. Thus, for
much of the family, the classification is similar to those presented by
Watson and Dallwitz (1999)
and Clayton and Renvoize (1986)
. The
Pooideae includes Avdulov's x = 7 group but is
expanded to include some genera whose relationships had only been
guessed at by previous workers. The Panicoideae, including maize,
sorghum, common millet, and foxtail millet, has been recognized since
the time of Robert Brown (1810
, 1814
), and remains largely unchanged;
its members all have paired flowers with the upper one generally
hermaphrodite and the lower one staminate or reduced. The
Chloridoideae, including finger millet and tef, was originally recognized by the structure of its microhairs and its
C4 anatomy. The Bambusoideae, including the woody
and herbaceous bamboos, is characterized by asymmetrically lobed
mesophyll cells (Zhang and Clark, 2000
). In its new circumscription, it
represents a much smaller group than it has in the past. Together these
four subfamilies account for nearly 90% of the species in the grasses.
The major point of discussion has been the disposition of the large group including the panicoids and chloridoids, known by the acronym PACC (panicoids, arundinoids, chloridoids, and centothecoids) in much of the recent literature. Although the entire group could have been designated a single large subfamily, the only morphological characteristic they share is a long internode in the embryo below the leaves around the point of attachment of the presumed cotyledon (mesocotyl), a character difficult to observe under most ordinary circumstances. The revised classification thus recognizes Chloridoideae and Panicoideae, as indicated in Figure 1. The remaining groups are given names or are left incertae sedis, i.e. "of uncertain placement."
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DINOSAURS DID NOT EAT GRASSES |
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The origin of the grasses can be dated by the appearance of grass
pollen in the fossil record. The grasses and their relatives have
distinctive pollen that is nearly spherical and with a single pore.
Grass pollen itself can be distinguished by minute channels or holes
that penetrate the outer, but not the inner, pollen wall (Linder and
Ferguson, 1985
). The earliest firm records of grass pollen are from the
Paleocene of South America and Africa, between 60 and 55 million years
ago (Jacobs et al., 1999
). This date is after the major extinction
events that ended the age of dinosaurs and the Cretaceous period.
Additional fossil pollen grains that may be grasses or may be grass
relatives have been found in Maastrichtian deposits of Africa and South
America (approximately 70 million years ago); these were fossilized
just before the end of the Cretaceous. Because of the way the pollen
was preserved, however, it is impossible to tell whether it had the
channels in the outer wall that are characteristic of the grasses
(Linder, 1987
; Jacobs et al., 1999
).
These pollen grains give upper and lower bounds for the date of the ancestor of the grasses (arrow in Fig. 1). Based on the fossil record, this ancestor lived before 55 million years ago but probably after 70 million years ago. This range of dates is used to calibrate molecular clocks, which are then used to calculate the times of other events in the history of the grasses (Box 3).
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WHAT HAPPENED WHEN THE GRASSES ORIGINATED |
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By comparing grasses with their closest relatives (outgroups), we
can infer what sorts of changes must have happened at the node with the
arrow, right around the end of the Cretaceous or the beginning of the
Tertiary period. A major change occurred in the timing of embryo
development. Most monocotyledonous plants have largely undifferentiated
embryos. Seed maturation begins after the embryo has formed a shoot
apical meristem, but the differentiation of cotyledon, leaves, root
meristem, and vasculature largely occurs after the seed is shed from
the parent plant. In the grasses, embryo development is accelerated
relative to seed maturation (Kellogg, 2000
).
At the same time there was a notable change in the structure of the
fruit. All the ancestors of the grasses had ovaries formed of three
fused carpels, each carpel forming one locule with one ovule (Kellogg
and Linder, 1995
). In many of the close relatives, and we presume in
the grass ancestors, two of those ovules abort and only one develops
(Dahlgren et al., 1985
; Linder, 1991
). In the grasses, only one locule
and one ovule ever form. As the ovule develops the outer integument
fuses with the inner ovary wall to form the distinctive fruit of the
grasses, known as the grain or caryopsis. This structure is unique
among the flowering plants.
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THE GRASS SPIKELET ORIGINATED IN SEVERAL STEPS |
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The most striking characteristic of grasses today is their floral and inflorescence structure. Grass flowers are generally arranged in little spikes, or spikelets; each spikelet consists of one or more flowers plus associated bracts (Fig. 3). In most species, the gynoecium has two stigmas and the androecium has three stamens. Outside the stamens, in the position of petals, are generally two flap-like structures, the lodicules, that become turgid and force the flower open at anthesis. Outside the lodicules is a structure similar to a prophyll, a two-keeled, leaf-like structure that normally appears on an axillary branch. The prophyll-like structure is the palea, and outside that is a bract-like structure (the lemma). Together these make up the floret. Florets are borne singly or in groups and are subtended by two more bracts (the glumes).
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The phylogeny shows that the spikelet must have originated in several steps (GPWG, 2000). The earliest grasses had three stigmas, a relict of the three fused carpels that they inherited from their ancestors; this number was reduced to two after the speciation event that led to Pharus. The earliest species also had, like their non-grass ancestors, six stamens. It is not clear from the phylogeny precisely when the shift from six to three occurred, but it must have been after the divergence of the Guaduella/Puelia group.
The ancestry and origin of the lodicules, palea, lemma, and glumes have
been the subject of a vast and largely inconclusive literature. Recent
work on lodicules in maize and rice has shown that they express
petal-identity genes (Ambrose et al., 2000
; Kyozuka et al., 2000
).
Because they are in the position of petals and because the early
grasses have three, rather than just two, it seems likely that
lodicules represent modifications of petals. However, the third
lodicule when present is inserted higher on the floral axis than the
other two, which has suggested to some authors that it has a different
evolutionary origin (for review, see Clifford, 1987
). It is curious
that neither Anomochloa nor Streptochaeta, the
earliest lineage of the grasses, has either petals or lodicules,
although Anomochloa has a ring of hairs outside the stamens
(Fig. 3). This means that either lodicules originated in the first
grasses and were lost in Anomochloa and
Streptochaeta or that they evolved after the grass family originated.
If lodicules are modifications of petals, could the palea and lemma be modifications of sepals? This has been suggested but will have to await additional genetic data. Anomochloa and Streptochaeta do not have structures that can be confidently called either lemmas or paleas. It thus seems likely that the conventional grass spikelet originated after the first grasses and characterizes most but not all of the family.
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WHAT HAPPENED BEFORE THE GRASSES ORIGINATED |
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Some characters associated with the success of the grass family
evolved long before the first grass appeared in the forest and thus
cannot be used to explain their current ecological dominance. The
grasses are wind-pollinated but so are all their relatives (Linder and
Kellogg, 1995
). From this we can infer that wind-pollination originated
millions of years before the grasses appeared on earth. Along with wind
pollination comes a reduction in perianth size and loss of pollen
stickiness (Linder, 1998
). All the relatives of the grasses similarly
accumulate silica somewhere in the plant so that silica accumulation
also must have originated well before the grasses themselves did. In
addition, a large set of monocotyledonous plants, including not only
the grasses, but also the gingers, pineapples, and palms, have cell
walls rich in ferulic acid. Ferulic acid in the cell walls must
therefore be an ancient characteristic preserved in the grasses.
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WHAT HAPPENED AFTER THE GRASSES ORIGINATED |
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Other "grass" characteristics originated long after the first
grasses (GPWG, 2000; Kellogg, 2000
). The most notable of these is
drought tolerance and the capacity to grow and thrive in dry open
habitats. The original grasses were plants of forest margins or deep
shade, characteristics that are retained today in
Anomochloa, Streptochaeta, Pharus,
Puelia, Guaduella, the bamboos, and the basal
pooid, Brachyelytrum. The phylogeny shows that the grasses persisted for many millions of years, and apparently did not diversify much in such habitats. The shift in habitat occurred at the points marked by O on Figure 1. This preceded the major diversification of the
family, detected in the fossil record by a marked increase in the
amount of grass pollen in the mid-Miocene epoch (Jacobs et al.,
1999
).
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MULTIPLE STARTING POINTS, SAME DESTINATION |
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The evolutionary tree can be used to determine major evolutionary
changes. One that has been especially well studied is
C4 photosynthesis, which is a complex addition to
the conventional C3 photosynthetic pathway (Kanai
and Edwards, 1999
; Fig. 4). In all
C4 species, the C3 pathway
is sequestered in the bundle sheath cells that surround the vascular
tissue; this is done in part by suppressing expression of ribulose 1,5 bisphosphate carboxylase/oxygenase (Rubisco) in the mesophyll.
Phosphoenol pyruvate carboxylase is then used to attach bicarbonate to
phosphoenolpyruvate (PEP), creating a four-carbon compound,
oxaloacetate (OAA).
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C4 grasses are the most common species in the
prairies of North America, the vast grasslands of Africa, and the
llanos and cerrados of South America. Studies of ancient ecosystems
have shown that these broad areas developed 5 to 6 million years
ago. The earliest record of C4
photosynthesis is based on isotopic ratios and is dated at 15 million
years ago (Kingston et al., 1994
; Latorre et al., 1997
), and the
earliest leaf fragment that can be confidently designated
C4 is dated at 12.5 million years ago (Nambudiri
et al., 1978
).
A molecular clock estimate, however, places the origin of the
predominantly C4 subfamily Panicoideae much
earlier at 25 to 32 million years ago (Gaut and Doebley, 1997
).
It is common to use numbers of mutations between two species to
estimate the time since they diverged. Statistical tests will determine
whether the rate of mutation is approximately constant over time. The
clock then must be calibrated with a fossil or a well-documented
geological event; this provides an estimate of number of mutations per
year. Given this calibration, the divergence of other species can then
be estimated. The discrepancy between the fossils and the molecular
clock could indicate that the clock was mis-calibrated or alternatively
that C4 grasses were originally quite rare and
thus are hard to find as fossils. The latter explanation suggests that
C4 grasses persisted as minor components of the flora for many years before they became ecologically dominant (Kellogg,
1999
).
Placing C4 photosynthesis on the evolutionary
tree shows that it originated multiple times among several closely
related subfamilies (Fig. 1; Kellogg, 1999
, 2000
). Extensive studies of
anatomy, histology, biochemistry, and gene expression have shown that
the C4 pathway did not evolve the same way each
time it originated (Sinha and Kellogg, 1996
).
Most studies of the biochemistry of C4 photosynthesis have proceeded on maize. Like most other C4 panicoids, maize has only one layer of cells surrounding its vascular bundles; this represents a loss of one layer of bundle sheath cells. In maize the OAA produced in the mesophyll is reduced to malate, which is moved into the bundle sheath, and one carbon is removed by NADP-malic enzyme. That carbon is picked up by Rubisco, and the remaining three-carbon compound is moved back to the mesophyll where it is phosphorylated to regenerate PEP.
In the Chloridoideae, on the other hand, all species are
C4 but have two layers of cells around the
vascular bundles, a characteristic that they share with all their
C3 ancestors. In these the OAA is aminated,
rather than reduced, and Asp is moved into the bundle sheath, where the
fourth carbon is removed by NAD-malic enzyme. Phosphorylation of the
three-carbon compound apparently occurs in the bundle sheath rather
than in the mesophyll (Sinha and Kellogg, 1996
).
The evolutionary tree thus shows that C4 has originated multiple times. This then led to more detailed investigations, which showed that gene-level changes apparently have happened differently each time.
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CONCLUSIONS |
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The collaborative work of the GPWG has resolved the broad outline of grass phylogeny, and we now know with considerable confidence which species are most closely related. This has produced a number of surprises, including the gradual evolution of the spikelet, the relatively late shift into open habitats, and the apparently recent diversification of the family. Additional systematic studies are continuing to place more and more grass species on phylogenetic trees providing an increasingly precise view of the order of evolutionary events.
This lays the groundwork for the main enterprise of evolutionary biology, that of understanding precisely what sorts of changes have occurred at critical junctures in evolutionary time, and therefore how evolution must have worked. For example, the close relationship of the chloridoid and panicoid grasses, along with other C4 species, suggests the possibility of underlying physiological similarities. Defining the derived states in terms of specific mutations will require new molecular tools, possibly of the sort now being developed for functional genomics. As such work proceeds, we will be able to define more and more precisely the genetic background that characterizes particular groups of grasses.
The phylogeny shows nested sets of species increasingly distantly related to the cereal crops. These certainly contain novel alleles or combinations of alleles that affect agronomically important phenotypes. The challenge of the future is to use the crop species as windows on the spectacular diversity produced by evolution and at the same time to use the thousands of wild grasses as tools to help understand the cereals.
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ACKNOWLEDGMENTS |
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Thanks to J. Barber, M. Beilstein, A. Doust, H. Davis, B. Gunn, S. Malcomber, S. Razafimandimbison, and P. Sweeney for helpful comments on the manuscript and for suggesting I take out the bit about the cat. Also, thanks to editor A. Hirsch and two anonymous reviewers for their comments.
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FOOTNOTES |
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Received November 7, 2000; accepted December 19, 2000.
1 This work was supported in part by the National Science Foundation (grant no. DEB-9815392).
* E-mail tkellogg{at}umsl.edu; fax 314-516-6233.
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J.-S. Kim, M. N. Islam-Faridi, P. E. Klein, D. M. Stelly, H. J. Price, R. R. Klein, and J. E. Mullet Comprehensive Molecular Cytogenetic Analysis of Sorghum Genome Architecture: Distribution of Euchromatin, Heterochromatin, Genes and Recombination in Comparison to Rice Genetics, December 1, 2005; 171(4): 1963 - 1976. [Abstract] [Full Text] [PDF] |