Early terrestrial ecosystems record a fascinating transition in the history of life. Animals and plants had previously lived only in the oceans, but, starting approximately 470 million years ago, began to colonize the previously barren continents. This paper provides an introduction to this period in life’s history, first presenting background information, before focusing on one animal group, the arthropods. It gives examples of the organisms living in early terrestrial communities and then outlines a suite of adaptations necessary for survival in harsh terrestrial environments. Emphasis is placed on the role of uncertainty in science; this is an integral part of the scientific process, yet is often seized upon by god-of-the-gaps creationist arguments. We hope to illustrate the importance of both uncertainty and scientists’ freedom to express doubt while a consensus is being built.
The impetus for this paper comes from a media report on the research of Garwood et al. (2009). The piece in question—in one of the more widely circulated but less universally respected newspapers of the UK—outlined the three-dimensional reconstruction of Carboniferous arachnids. Though the reporting was for the most part scientifically accurate, the associated online comments section provided unfortunate contrast. The first entry was a typically trivial and superficial anti-evolutionist’s jibe regarding these arachnids: “they look just like spiders do today. 300 million years and no change. […] Kind of hard on the old evolution theory isn’t it?” When the comment’s author was asked to expand on his beliefs, the response was an entirely predictable: “Why do I have to come up with an alternative for your useless theory?”
This altercation encapsulates perfectly a common creationist mindset, one based on cursory (and often incorrect) observations coupled with complete ignorance (or at best patchy understanding) of the scientific context framing an argument. See, for example, the myriad arguments introduced in Part III of Scott (2009). It further relies upon a god-of-the-gaps argument, the belief that in the case of unanswered questions the proponent’s personal worldview wins by default. No alternatives nor evidence supporting the proponent’s perspective are required (Pennock 2007). The comment is flawed on a number of counts. Not least, the arachnid group in question, the trigonotarbids (Fig. 1), were indeed quite different from spiders in that they lacked the ability to spin silk (Shear 2000a) and possessed a segmented posterior body region (likely inherited from their last shared common ancestor with spiders; Dunlop 1997). Furthermore, as we shall see later in this article, a degree of morphological stasis over 300 million years is in no way antithetical to the theory of evolution. The comment is also unfortunate because the early terrestrial (land-based) animal communities in which this trigonotarbid lived provide us with resounding evidence for evolution. They also offer an excellent example of the unanswered questions and uncertainties inherent to—and a driving force in—scientific inquiry. It is these uncertainties that the arguments of antievolutionists seize upon. If they succeeded, this would stifle the colorful world of scientific discovery and reduce it to a Manichaen palette of unquestioning certainty and unknowable unknowns (the dualism of Nelson 1999).
With this in mind, we hope that this paper will not only introduce these fossil communities and outline their evolution, but also demonstrate that ambiguity in science is neither detrimental nor a weakness. Rather it is a vital part of our field, which stimulates debate and drives further research and discoveries.
The paper is split into sections—the next will introduce terrestrial life as a whole during this period in the Earth’s history before we focus on one group of animals in particular, the arthropods. We will then introduce examples of early terrestrial fossils that run the gamut from entirely extinct groups to those that are largely unchanged compared to their modern relatives, living in ecosystems that closely resemble those today. We will finish by introducing some of the adaptations these animals have evolved for a life on land.
Terrestrial Palaeozoic Life
The Paleozoic Era lasts from the beginning of the Cambrian Period (542 million years ago; Gradstein et al. 2009), known for its famous explosion of marine animals, to the end of the Permian Period (251 million years ago); marked by the greatest mass extinction ever known (Sahney and Benton 2008). Prior to the Paleozoic, the only life on land was unicellular, a fact that—until recently—could only be inferred from indirect evidence (Rasmussen et al. 2009; Prave 2002). However, current research is revealing unexpectedly diverse terrestrial communities revealed in one billion-year-old cellular fossils (Strother et al. 2011). It was during the Paleozoic Era that plants (first known from microfossils called cryptospores that appear in the mid-Ordovician, about 470 million years ago; Wellman and Gray 2000) and animals (known from Silurian fossils, at least 423 million years ago; Wilson and Anderson 2004) began to colonize the land. Land plants started as small, non-vascular mosses and liverworts (bryophytes; Edwards 2000), but by the Late Silurian, simple plants with axial organization and terminal sporangia (spore-bearing structures) were becoming common (e.g., Cooksonia; Kenrick and Crane 1997). During the Late Paleozoic—the Devonian (416–359 million years ago) and Carboniferous (359–299 million years ago) periods—the first widespread forest ecosystems became established (DiMichele et al. 2007). Although quite different from modern forests, by the Carboniferous, these were diverse (DiMichele 2001) and included early tree-like relatives of extant club mosses (lycopsids) and horsetails (Calamites), and a wide variety of ferns (Falcon-Lang and Miller 2007). These forests were home to a wide range of animals, which had first ventured on to land in the preceding 100 million years. One group of these were early ancestors of all terrestrial vertebrates, which had first ventured on to land during the Devonian (probably between 385 and 360 million years ago). Paleozoic fossils record this transition from fish to land-dwelling limbed organisms (tetrapods; Clack 2009) and also span the split between true amphibians and other vertebrates (mammals and reptiles/birds; Clack 2006; Coates et al. 2008). Many early tetrapods were still aquatic, and probably lived within rivers and other freshwater environments, with the possible occasional foray onto land (Benton 2005). Fully terrestrial species were common by the Carboniferous Period, however, and the earliest true reptiles had evolved by the end of the Paleozoic, in the form of small- to medium-sized insect eaters (Modesto et al. 2009).
The majority of animal diversity and abundance in Paleozoic terrestrial communities can be found in the arthropods (a group which has, in fact, been dominant in terms of animal species diversity for all of the past 520 million years; Edgecombe 2010). The phylum Arthropoda is a group of animals united by, amongst other traits: external and internal body segmentation with regional specialization (tagmosis, e.g., a thorax with legs and wings versus a limbless abdomen in the case of insects); an exoskeleton composed of articulated plates, hardened through calcification or sclerotization (protein cross-linking); body segments that primitively bear paired, articulated appendages; growth via molting (ecdysis); a pair of lateral facetted (compound) eyes that are innervated by the first of three segments that comprise the brain; and an open circulatory system featuring a dorsal heart with lateral valves (Grimaldi and Engel 2005). The unique features of arthropods indicate that they are a monophyletic group (descendants of a common ancestor that possessed the diagnostic features of the group). Arthropoda (Fig. 2) includes the extinct trilobites, the insects, the myriapods (millipedes, centipedes, and relatives), the crustaceans (e.g., crabs, lobsters, shrimp), and the chelicerates (arachnids, such as spiders, scorpions and mites, and horseshoe crabs). Their abundance makes arthropods ecologically vital; for example, myriapods are important processors of leaf litter in forests, and termites consume large quantities of cellulose (Crawford 1992; Higashi et al. 1992). Without arthropods, the life and ecosystems of the Earth would be radically different. Their astounding diversity (constituting in excess of 75% of all described living species; Brusca and Brusca 2003) can help elucidate the patterns and processes of evolution. For example, the study of trilobites was central to the development of punctuated equilibrium as a model for evolutionary change (Eldredge and Gould 1972; Gould and Eldredge 1977), and the fruit fly Drosophila was the “model organism” used in much of the pioneering work on genetics in the early twentieth century as well as unraveling the genetics of development in the late twentieth century. It is for these reasons that the following discussion of terrestrial Paleozoic life and evolution will focus on the Arthopoda.
The Palaeozoic Fossil Record of Terrestrial Arthropods
The first terrestrial arthropods predated tetrapods by tens of millions of years (Shear and Selden 2001). Evidence of animal life on land before the first known arthropod body fossils can be found in the form of preserved traces that are likely to have been created by macroscopic organisms. Identifying the animal that made trackways or burrows is not always straightforward. For example, burrows assigned to the ichnogenus Scoyenia from Late Ordovician (ca 447 million years ago) rocks in Pennsylvania (Retallack and Feakes 1987) had been interpreted as having been made by millipedes (Retallack 2001), but this has been disputed based on how living millipedes burrow (Wilson 2006) and also because the sediments show evidence of a marine rather than terrestrial origin (Davies et al. 2010). The best candidates for trackways of Ordovician age that were made by an identifiable group of terrestrial arthropods occur in Late Ordovician rocks in Cumbria, UK, in ash and sandstones that were deposited subaerially (Johnson et al. 1994). A comparison with the locomotory traces of living “pin cushion” millipedes showed that the stepping gait of the Cumbrian Ordovician trackways is consistent with them having been made by an early millipede (Wilson 2006).
The first body fossil evidence of the animals responsible for such tracks dates from the Silurian Period (444–416 million years ago). Several millipedes have recently come to light from Stonehaven, UK (approximately 423 million years ago), including one species, Pneumodesmus newmanii, that provides the first evidence for air breathing in any form of animal (Wilson and Anderson 2004). This can be seen in spiracles (or, more biblically, stigmata)—openings into the tracheal (breathing) system which are a terrestrial feature by definition. Another of the Silurian millipedes has a paired structure on the anterior part of the trunk, in the usual segmental position and with a characteristic form of a gonopod, a modified pair of legs that male millipedes use to transfer sperm to the female’s genital opening (Fig. 3; Wilson and Anderson 2004). The Silurian fossils thus provide direct evidence for a similar reproductive mode as their extant relatives.
The majority of fossils from around this time, however, are not discovered by simply splitting rocks in the field, but rather are found in acid macerate residues. These are “leftovers” from the acid digestion of rocks, to which the arthropod cuticle (exoskeleton), composed of chitin, is resistant. The earliest deposit from which this technique has recovered identifiable organisms is found in Ludford Lane, Shropshire, UK (approximately 417 million years ago) where both arachnids and centipedes are known (Jeram et al. 1990). A wider range of arthropods are recovered using this method from Middle Devonian (388 million years ago) rocks of Gilboa, New York. These include a number of different arachnids, including mites and pseudoscorpions (Shear et al. 1987; Norton et al. 1988; Schawaller et al. 1991; Selden et al. 1991), centipedes (Shear and Bonamo 1988), and possible fragments of insect exoskeleton (Shear et al. 1984).
Another famous Devonian (approximately 396 million years ago on the basis of radiometric dating, though spores suggest a slightly older age in the Early Devonian; Rice et al. 1995; Wellman et al. 2006) fossil locality is the Rhynie Chert, near Aberdeen, in Scotland. These translucent rocks were formed in a hydrothermal hot spring setting in which silica-rich water inundated and silicified nearby vegetation, including a number of the animals—all arthropods—creating a near-perfect record of this early terrestrial ecosystem (Trewin et al. 2003). The incredibly well-preserved fossils are studied in slides made from the rock and often display the internal anatomy (e.g., book lungs, the respiratory organs of arachnids; Kamenz et al. 2008). Animals described to date include arachnids (Fayers et al. 2005), primitively flightless hexapods (springtails and a bristletail or silverfish), as well as true insects (Fayers and Trewin 2005; Engel and Grimaldi 2004), centipedes (Shear et al. 1998), and freshwater Crustacea, including extinct relatives of fairy shrimp and tadpole shrimp (Trewin and Fayers 2007). Another fossil locality from the Early Devonian is Germany’s Alken-an-der-Mosel, from which a range of different arthropods, including several kinds of arachnids and relatives of millipedes called eoarthropleurids, were described by the Norwegian paleontologist Leif Størmer (1970; 1972; 1973; 1974; 1976), but few other deposits preserve anything more than isolated individuals. Despite the important anatomical, ecological, and temporal data provided by the Silurian and Devonian fossil deposits, the first widespread and well-preserved record of terrestrial ecosystems dates from approximately 20 million years later, in deposits of the Upper Carboniferous Period (Shear 2000b). During this period, a mountain-building event, the Variscan Orogeny, contributed to the assembly of the supercontinent Pangea (Cocks and Torsvik 2006). Despite glaciations at the poles, a wide zone carpeted with thick forests and vegetation spanned the tropics and even some higher latitudes (Cleal and Thomas 2005). These forests supported diverse ecosystems (Shear and Kukalová-Peck 1990). Many of them were in effect mires, wet environments in which organic matter accumulates (DiMichele 2001), and flooding was widespread (Falcon-Lang 2000; Plotnick et al. 2009). The resulting waterlogged boggy sediments create ideal conditions for the preservation of fossils within siderite (FeCO3) nodules and also for the formation of coal (Curtis and Coleman 1986). As a result, coal from this period is found throughout North America and Europe. In fact, the Carboniferous was responsible for fuelling the industrial revolution on both continents (Chandler Jr 1972; Hartwell 1967). Thus, a number of factors created ideal conditions for both the widespread preservation of fossils during the Carboniferous and the exploitation of these deposits by geologists more than 300 million years later. As a result, they provide one of the most important windows into early terrestrial ecosystems.
Fossils from these early ecosystems record a number of arthropod groups at different grades of organization, which we will briefly compare here. Some are entirely extinct groups, such as the aforementioned arachnids, the trigonotarbids (Fig. 4a; Dunlop et al. 2008a). These are known from exceptionally well-preserved Rhynie Chert fossils and appear to have been amongst the most abundant arachnids in Carboniferous coal forests (Garwood and Dunlop 2011). The presence of two pairs of lungs on the same body segments as some extant forms provides a strong argument that they are most closely related to a group known as the tetrapulmonate arachnids, which includes the spiders, whip scorpions, whip spiders, and short-tailed whipscorpions (Dunlop 2010). Indeed, the fine structure of the book lungs from a Devonian trigonotarbid, examined using three-dimensional reconstruction techniques, is shared with living tetrapulmonates (Kamenz et al. 2008). The youngest fossil member of the group dates from 290 million years ago (Rößler et al. 2003). Thus, the trigonotarbids are an entirely extinct group, an evolutionary dead end, but one that shares a common ancestor with spiders and other arachnids with two pairs of lungs.
The earliest centipedes exhibit features that allow them to be classified in some of the major groups that have survived until today. The oldest of these, from the Late Silurian of the Welsh Borderlands in England, belong to a genus, Crussolum, that is better known from various body parts in the Early and Middle Devonian (as for many examples in this article, the Devonian fossils come from the Rhynie cherts in Scotland and Gilboa in New York State—Fig. 4b has an example; Anderson and Trewin 2003; Shear and Bonamo 1988). Crussolum is unambiguously a member of Scutigeromorpha, a group that includes 100 living species that mostly live in the tropics and subtropics, but best known from the “house centipede,” Scutigera coleoptrata, an introduced species in many temperate parts of the world (Fig. 2c). Crussolum shares with the extant scutigeromorphs such features as a pentagonal cross-section of the leg with each of the ridges that runs along the leg segments bearing a file of spines and thickened setae, but it lacks a few details that all of the living scutigeromorphs share with each other. For example, though the fossils have the first pair of trunk legs modified into a functional part of the head (and housing the venom apparatus in all living centipedes), they do not have long “spine bristles” in fixed positions that are seen in all the living species. This mix of primitive and advanced characters in Crussolum is described using a convention called “stem groups”; Crussolum belongs to the stem group of Scutigeromorpha. This means that the species is more closely related to Scutigeromorpha than to any other living centipede group, but it branched earlier than the most recent common ancestor of all living scutigeromorph species.
Amongst the earliest winged insects—and very common in the Carboniferous—were the Blattoptera, or “roachoids” (Fig. 4d). As the name suggests, these were similar to modern-day cockroaches. For example, they possessed hardened, protective forewings and a pronotum (a head shield originating at the first segment of the thorax), but unlike true cockroaches, they had a long needle-like ovipositor for laying eggs (Grimaldi and Engel 2005). The reason they are known as “roachoid” fossils is because—while they are superficially similar to cockroaches in appearance—they predate the split between the mantises and the cockroaches and termites (the termites are actually highly derived, eusocial cockroaches; Inward et al. 2007). As such, these weren’t an evolutionary dead end; collectively, “roachoids” represent a grade at the base of the evolutionary tree for Dictyoptera, the formal name for the mantises (and cockroaches + termites), making them another example of a stem group form. It is likely that some of the later Carboniferous fossils postdate the evolutionary divergence of the extant lineages of Dictyoptera, and they would accordingly belong to the stem groups of either the mantises or the cockroach/termite branch (Béthoux et al. 2009).
Scorpions are the earliest known arachnids and have a significant Paleozoic fossil record (Fig. 4e; Dunlop et al. 2008b). While debate remains regarding whether their earliest representatives were aquatic or terrestrial (Dunlop and Webster 1999; Kamenz et al. 2008), by the Carboniferous, there is little question the scorpions were land-dwelling (Jeram 1994a). Even by the Early Devonian, fragments of the book lungs of fossil scorpions indicate air breathing (Shear et al. 1996). All modern scorpions belong to a group known as the orthosterns, which possess spiracles within the plates on the scorpions’ underside rather than at their margin as seen in some of the oldest fossil species. The oldest members of this group are Carboniferous in age (Fig. 4e; Vogel and Durden 1966; Jeram 1994b; Legg et al. 2011), and the oldest known member of an extant family is at least 50 million years younger (Lourenço and Gall 2004). Thus, later Paleozoic scorpions probably fall in the stem group of modern families, but postdate the last common ancestor of the orthosternous scorpions. We can hence say that the origin of extant scorpions lies in the Carboniferous Period.
Perhaps some of the most impressive terrestrial Paleozoic fossils, however, are those of harvestmen (Fig. 4c): arachnids of the order Opiliones, which have a small fused body and often extremely long legs (Machado et al. 2007). The best fossils are once again those of the Rhynie cherts, which preserve the internal anatomy, including specimens that have the reproductive organs of either males or females (Dunlop et al. 2003). Their morphology suggests that they are essentially modern in form. The fact that the Devonian species was placed in one of the four major living groups of Opiliones (Dunlop et al. 2004) implies that harvestmen were amongst the earliest branching arachnids and corroborates recent molecular work suggesting a relatively early Paleozoic radiation in the group (Giribet et al. 2010). Furthermore, the fact that they have remained morphologically largely unchanged for over 400 million years suggests that they exemplify evolutionary stasis. Why this is the case remains unclear, but this uncertainty regarding the cause of stasis in no way undermines evolution as a god-of-the-gaps proponent would suggest. Stasis within species is expected in a number of evolutionary models (Eldredge and Gould 1972; Sheldon 1996; Benton and Pearson 2001). Thus, in higher-level taxonomic groups with relatively low rates of speciation, we may expect elements of stasis (see discussion: Gould 2002, p. 936; Cavalier-Smith 2006, p. 999; and stasis in ecological assemblages: DiMichele et al. 2004). It is noteworthy, however, that stasis in taxonomic groups above the species level is the exception rather than the rule, as the above examples demonstrate. The fact that such stasis exists presents us with a compelling opportunity to explain its presence—it does not allow a non-naturalistic view to win by default.
Only nine of 58 extinct and extant animal phyla have terrestrial representatives (Labandeira and Beall 1990), largely because land presents a new and hostile environment for a marine organism (Selden and Jeram 1989; Selden and Edwards 1990). As a result, life on land requires a suite of adaptations. The presence of such changes to accommodate a new mode of life provides excellent evidence for evolution; they have a clear functional significance, and a number have evolved separately in different lineages (Raven 1985). To reiterate, the earliest known terrestrial animals were arthropods (Little 1983)—members of the Myriapoda (millipedes, centipedes, and their kin), Arachnida (spiders, scorpions, and relatives), and Hexapoda (insects and three smaller, primitively wingless groups). In this, the final section of the paper, we shall provide an overview of the adaptations present in terrestrial arthropod groups and then outline why their convergent evolution (independent origins in different lineages) has sometimes complicated efforts to assess arthropod relationships (Edgecombe 2010).
Of the problems associated with terrestrial life, perhaps the biggest is that of water retention (Hadley 1994). Water is a vital solvent for life, and minimizing water loss and ensuring its availability is vital for terrestrial organisms (Little 1983). A major part of the fight to avoid desiccation is the arthropods’ exoskeleton, the outermost layer of which (the epicuticle) is waxy and waterproof (Fig. 5a; Cody et al. 2011). This proofing is caused by lipids (hydrocarbons, in this case including paraffin-like molecules, wax esters, fatty acids, and ketones) both within the epicuticle and deposited on its surface (Hadley 1986). As well as waterproofing an organism, this very successfully prevents evaporation. As we shall see below, terrestrial arthropods employ a variety of independently derived respiratory systems. Despite these independent origins, all are internal, an arrangement which serves to lessen water loss (Brusca and Brusca 2003). Additionally, all possess spiracles (Fig. 5b)—the structures that provide the earliest evidence for fully terrestrial life in millipedes. Spiracles act as an opening through the cuticle into respiratory structures, and—despite independent origins—those of insects (Gullan and Cranston 2010), myriapods (Shear and Edgecombe 2010), and chelicerates (Levi 1967) have associated musculature to regulate gas entry and exit, and minimize water loss through the moist respiratory structures. This is even the case where the respiratory organs—introduced below—differ greatly, for example, between the book lungs of scorpions (Polis 1990) and the tracheal system of insects (Grimaldi and Engel 2005).
Another major source of water loss in organisms is excretion. When animals digest protein, excess nitrogen is produced and is usually liberated in the form of ammonia (NH3), a toxic compound that requires rapid dilution or removal (Brusca and Brusca 2003). Dilution demands abundant water and is thus unsuitable for terrestrial organisms, for whom water is a precious resource. Thus, most terrestrial organisms convert ammonia into more complex yet less toxic compounds; in vertebrates, like us, urea, but in arthropods uric acid is more common, which is often precipitated in solid form (Raven 1985). In arthropods, this waste is removed with the aid of two types of organs.
Nephridia are organs found on one or a few anterior body segments of all arthropod groups. The closest living relatives of arthropods, the velvet worms (Onychophora), have a pair of nephridia on most body segments, and they resemble those of many aquatic animals (Fig. 6a) in being composed of an excretory duct starting at the animal’s exterior (opening to a pore at the inner base of each leg in velvet worms) and ending with a funnel-shaped, hair-lined opening into the body. The hairs direct fluid into the duct (Ruppert et al. 2003). As this moves through, the reabsorption and secretion of cells lining the duct modify the liquid, concentrating waste products (Ruppert and Smith 1988; Campiglia and Maddrell 1986; Bartolomaeus 1992). Waste is excreted to the exterior through the terminal opening, known as the nephridopore. Nephridia of arthropods, in the form of coxal glands, antennal glands, maxillary glands, or labial kidneys (depending on where they are located), differ in being internally closed and the funnel is not ciliated. Nephridial organs are thought to have been present in the last common ancestor of all arthropods (known as a plesiomorphic trait).
Most terrestrial arthropods also possess or wholly replace nephridia with structures known as Malpighian tubules, which allow efficient waste removal. These are blind ducts which open at one end into the gut and remain unattached at the other end (Fig. 6b). They float and move around in arthropods’ blood-filled body cavity (or hemocoel) and absorb waste products. As the waste moves down the tubule, water is reabsorbed, until crystals of uric acid are formed, and in the hindgut, further reabsorption occurs in a structure known as the rectal gland (Roberts 1986). The above description is based upon the Malpighian tubules of insects, and each individual can have hundreds of these (Brusca and Brusca 2003). However, very similar structures have been independently derived in both myriapods, which have just one or two depending on the group (Hopkin and Read 1992; Lewis 2007), and terrestrial chelicerates, which have several branching tubules (Barnes et al. 2001). Water loss can further be reduced through behavior—arthropods at risk of desiccation will often live in humid and moist environments to the extent that some extract moisture from the substrate (Crawford and Cloudsley-Thompson 1971). Many desert-dwelling species avoid periods of high temperatures by becoming inactive in burrows (Hadley 1974).
Another major issue with life on land is that of respiration, or gas exchange (Raven 1985). This cannot be done through increasing the permeability of the exoskeleton, which would allow significant water loss. As we have seen, this is a significant consideration, and all but the smallest terrestrial arthropods have specialized gas exchange structures (Selden and Edwards 1990). These come in two flavors. The first—found in arachnids—are the book lungs: stacked, blood-filled lamellae extending into an air-filled cavity (Fig. 7a). This cavity (the atrium) opens to the outside through the spiracles (Scholtz and Kamenz 2006), and the thin lamellae provide a high surface area to allow gas exchange. The second type of respiratory structures, which probably evolved convergently in insects and myriapods (Grimaldi 2010), are known as tracheae (Fig. 7b). These are branching cuticle-lined tubules opening externally through the spiracles and terminating internally in the blood, or organ tissues (Barnes et al. 2001). This is an efficient system, allowing direct gas exchange with the internal organs and blood—so much so that a similar system has secondarily evolved from book lungs in some spiders (Schmitz and Perry 2001). Comparable structures called pseudotrachea are also found in woodlice, which are crustaceans of the order Isopoda (Edney 1968).
A less immediately apparent issue is that of reproduction—for arthropods in the marine realm, releasing eggs and sperm into the sea for external fertilization is a viable approach for reproduction (Selden and Jeram 1989). This is not as effective in the terrestrial realm, however, and internal fertilization is usually preferred. Associated with this is a wide range of complex sperm transfer techniques—for example, the use of packages of sperm known as spermatophores is common, protecting them (to an extent) from the harsh terrestrial environment. A bewilderingly vast array of sometimes complex courtship behaviors has developed in terrestrial arthropods (Choe and Crespi 1997). While there are myriad possible causes for this adaptation (Bastock 2007), in part this could be to ensure the successful transfer of spermatophores (for example, in the whip spiders, Fig. 2a; Weygoldt 2002). Direct sperm transfer in the form of copulation bypasses the risk of environmental damage in many more derived forms (Selden and Edwards 1990). Young are often helped with parental brooding during embryonic development or after birth (Labandeira and Beall 1990).
Locomotion and Senses
While life on land presents a plethora of other challenges, the last we will look at here stem from the physical differences between water and air. These can have a significant impact on an organism’s morphology, given that water has greater buoyancy than air (Selden and Jeram 1989). To support themselves, terrestrial organisms require rigid skeletal elements, and the arthropods had a preexisting advantage in their presence of an exoskeleton (Raven 1985). Terrestrial arthropods also generally adopt a more stable hanging stance, standing on the underside of their limbs whose ends are at a low angle to the ground (a plantigrade tarsus; Størmer 1970; Fig. 8a). There are also a huge number of sensory adaptations to this new medium, for example, the trichobothria of scorpions (Fig. 8b)—long, thin hairs originating in a cup-shaped depression that can sense very slight air vibrations (Reissland and Görner 1985). This aids prey location and orientation relative to wind, but would not work in a fluid medium (Krapf 1986; Meßlinger 1987). Superficially similar trichobothria are also present in some myriapods (Haupt 1979); the distant relationship between these myriapods and arachnids indicates a convergent evolution of trichobothria.
As a result of this suite of adaptations—and a host of further physiological changes—arthropods are successful terrestrial organisms. So successful, in fact, that whether judged by number of species or individuals, they are thriving desert inhabitants (Edney 1967) and are vital members of these harshest terrestrial ecosystems (Whitford 2000).
All of these evolutionary adaptations increase fitness in terrestrial environments, and as such, their parallel (convergent) evolution in multiple lineages under the same selective pressure is expected. However, they also effectively demonstrate a major cause of uncertainty amongst arthropod workers—the traditional basis for assessing evolutionary relationships is morphology (Darwin 1859; Skelton 1993). Thus, assessing whether structures are homologous (share a common origin) or homoplasious (the result of convergence) is vital to understanding a group’s relationships (Edgecombe 2009). This is rarely clear-cut, however. To use examples we have seen already, insects and myriapods share tracheae and Malphighian tubules, and these features were traditionally ascribed to inheritance from common ancestry because insects and myriapods were considered sister taxa in a group known as the Atelocerata (Snodgrass 1938; Klass and Kristensen 2001; Bitsch and Bitsch 2004; see also discussion in Shultz and Regier 2000 and Dohle 1998). They further share a suite of other characters, including single-branched appendages and a head comprising an antennal segment, a limbless (intercalary) segment, and then two segments bearing mouthparts. However, DNA analysis has never supported this grouping, with many different kinds of genetic data all agreeing instead that the insects share a common ancestor with the crustaceans (insects and crustaceans collectively forming a group called the Tetraconata; Jenner 2010). This is now largely accepted and has been corroborated by many features of the brain, eyes, and nervous system development that are unique to insects and crustaceans but not shared by myriapods (Edgecombe 2010). The evolutionary picture provided by the genes and nervous system suggests that tracheae and Malphighian tubules in insects and myriapods are an example of convergent evolution in two terrestrial lineages. However, the new consensus on an insect–crustacean relationship emerged from 20 years of research (including enormous technological and theoretical advances in molecular biology and new techniques of investigating anatomy) and through frank discussion of the opposing arguments.
This process of altering hypotheses on the basis of increased evidence is central to the science, yet such advances rely on uncertainty and debate. If god-of-the-gaps creationist opposition makes scientists reluctant to express their doubts on a subject—such as the issue of arthropod relationships outlined here—these advances would be slower-to-nonexistent. Due to the nature of evolution, ambiguity is ubiquitous; the outlined example of similarity as a result of either a common evolutionary origin or later convergence is just one of many sources of debate. It is for this reason that myriad unanswered questions regarding arthropod phylogeny remain, some at a fairly basic level. To present unanswered questions as a weakness, or pretend they undermine evidence, is disingenuous and incorrect. Rather, the possibility of new evidence, resulting in paradigm shifts and a greater understanding of the history of life, is one of the most exciting elements of science.
Anderson LI, Trewin NH. An Early Devonian arthropod fauna from the Windyfield Cherts, Aberdeenshire, Scotland. Palaeontology. 2003;46(3):467–509.
Barnes RSK, Calow PP, Olive PJW, Golding DW, Spicer JI. The invertebrates: a synthesis. Oxford: Wiley-Blackwell; 2001.
Bartolomaeus T. Protonephridia and metanephridia—their relation within the Bilateria. J Zool Syst Evol Research 1992;30:21–45.
Bastock M. Courtship: an ethological study. New Jersey: Transaction Publishers; 2007.
Bell WJ, Adiyodi KG. The American cockroach. London: Chapman and Hall; 1982.
Benton MJ. Vertebrate palaeontology: third edition. Oxford: Blackwell Publishing; 2005.
Benton MJ, Pearson PN. Speciation in the fossil record. Trends Ecol Evol. 2001;16(7):405–11.
Béthoux O, Klass KD, Schneider JW. Tackling the Protoblattoidea problem: revision of Protoblattinopsis stubblefieldi (Dictyoptera; Late Carboniferous). European J Entomol. 2009;106:145–52.
Bitsch C, Bitsch J. Phylogenetic relationships of basal hexapods among the mandibulate arthropods: a cladistic analysis based on comparative morphological characters. Zool Scr. 2004;33(6):511–50.
Brusca RC, Brusca GJ. Invertebrates—second edition. Sunderland: Sinauer Associates; 2003.
Campiglia SS, Maddrell SHP. Ion absorption by the distal tubules of onychophoran nephridia. J Exp Biol. 1986;121:43–54.
Cavalier-Smith T. Cell evolution and Earth history: stasis and revolution. Philos Trans R Soc Lond Ser B: Biol Sci. 2006;361(1470):969–1006.
Chandler Jr AD. Anthracite coal and the beginnings of the Industrial Revolution in the United States. Bus Hist Rev. 1972;46(2):147–81.
Choe JC, Crespi BJ. The evolution of mating systems in insects and arachnids. Cambridge: Cambridge University Press; 1997.
Clack JA. The emergence of early tetrapods. Palaeogeogr Palaeoclimatol Palaeoecol. 2006;232(2–4):167–89.
Clack JA. The fin to limb transition: new data, interpretations, and hypotheses from paleontology and developmental biology. Annu Rev Earth Planet Sci. 2009;37(1):163–79.
Cleal CJ, Thomas BA. Palaeozoic tropical rainforests and their effect on global climates: is the past the key to the present? Geobiology. 2005;3(1):13–31.
Coates MI, Ruta M, Friedman M. Ever since Owen: changing perspectives on the early evolution of tetrapods. Annu Rev Ecol Evol Syst. 2008;39:571–92.
Cocks LRM, Torsvik TH. European geography in a global context from the Vendian to the end of the Palaeozoic. Geol Soc Lond, Memoirs. 2006;32(1):83–95.
Cody GD, Gupta NS, Briggs DEG, Kilcoyne ALD, Summons RE, Kenig F, et al. Molecular signature of chitin–protein complex in Paleozoic arthropods. Geology. 2011;39(3):255–8.
Crawford CS. Millipedes as model detritivores. Berichte der Naturwissenschaftlich. 1992;10:277–88.
Crawford CS, Cloudsley-Thompson JL. Water relations and desiccation-avoiding behavior in the vinegaroon Mastigoproctus giganteus (Arachnida: Uropygi). Entomologia Experimentalis et Applicata. 1971;14(1):99–106.
Curtis CD, Coleman ML. On the precipitation of early diagenetic calcite, dolomite and siderite concretions in complex depositional sequences. In: Gautier DL, editor. Roles of organic matter in sediment diagenesis. Society of Economic Paleontologists and Mineralogists Special Publication 38; 1986. p. 23–33.
Darwin C. On the origin of species by means of natural selection, or the preservation of favoured races in the struggle for life. London: John Murray; 1859.
Davies NS, Rygel MC, Gibling MR. Marine influence in the Upper Ordovician Juniata Formation (Potters Mills, Pennsylvania): implications for the history of life on land. Palaios. 2010;25(8):527–39.
DiMichele WA. Chapter 1.3.8.—Carboniferous coal-swamp forests. In: Briggs DEG, Crowther PR, editors. Palaeobiology II. Oxford: Wiley Blackwell; 2001. p. 79–82.
DiMichele WA, Behrensmeyer AK, Olszewski TD, Labandeira CC, Pandolfi JM, Wing SL, et al. Long-term stasis in ecological assemblages: evidence from the fossil record. Annu Rev Ecol Evol Syst. 2004;35(1):285–322.
DiMichele WA, Falcon-Lang HJ, John Nelson W, Elrick SD, Ames PR. Ecological gradients within a Pennsylvanian mire forest. Geology. 2007;35(5):415–8.
Dohle W. Myriapod-insect relationships as opposed to an insect–crustacean sister group relationship. In: Fortey RA, Thomas RH, editors. Arthropod relationships. London: Chapman & Hall; 1998. p. 305–15.
Dunlop JA. The origins of tetrapulmonate book lungs and their significance for chelicerate phylogeny. In: Selden PA, editor. Proceedings of the 17th European Colloquium of Arachnology, Edinburgh 1997. Burnham Beeches: British Arachnological Society; 1997. p. 9–16.
Dunlop JA. Geological history and phylogeny of Chelicerata. Arthropod Struct Dev. 2010;39(2–3):124–42.
Dunlop JA, Webster M. Fossil evidence, terrestrialization and arachnid phylogeny. J Arachnol. 1999;27(1):86–93.
Dunlop JA, Anderson LI, Kerp H, Hass H. Preserved organs of Devonian harvestmen. Nature. 2003;425:916.
Dunlop JA, Anderson LI, Kerp H, Hass H. A harvestman (Arachnida: Opiliones) from the Early Devonian Rhynie cherts, Aberdeenshire, Scotland. Trans Royal Soc Edinburgh, Earth Sci. 2004;94(4):341–54.
Dunlop JA, Tetlie OE, Penney D, Anderson LI. How many species of fossil arachnids are there? J Arachnol. 2008a;36(2):267–72.
Dunlop JA, Tetlie OE, Prendini L. Reinterpretation of the Silurian scorpion Proscorpius osborni (Whitfield): integrating data from Palaeozoic and recent scorpions. Palaeontology. 2008b;51(2):303–20.
Edgecombe GD. Palaeontological and molecular evidence linking arthropods, onychophorans, and other Ecdysozoa. Evol: Educ Outreach. 2009;2(2):178–90.
Edgecombe GD. Arthropod phylogeny: an overview from the perspectives of morphology, molecular data and the fossil record. Arthropod Struct Dev. 2010;39:74–87.
Edney EB. Water balance in desert arthropods. Science. 1967;156(3778):1059–66.
Edney EB. Transition from water to land in isopod crustaceans. Amer Zool. 1968;8(3):309–26.
Edwards D. The role of mid-Palaeozoic mesofossils in the detection of early bryophytes. Philos Trans R Soc Lond Ser B: Biol Sci. 2000;355:733–54.
Eldredge N, Gould SJ. Punctuated equilibria: an alternative to phyletic gradualism. In: Schopf TJ, editor. Models in paleobiology. San Francisco: Freeman, Cooper & Co.; 1972. p. 82–115.
Engel MS, Grimaldi DA. New light shed on the oldest insect. Nature. 2004;427:627–30.
Falcon-Lang HJ. Fire ecology of the Carboniferous tropical zone. Palaeogeogr Palaeoclimatol Palaeoecol. 2000;164:339–55.
Falcon-Lang HJ, Miller RF. Palaeoenvironments and palaeoecology of the Early Pennsylvanian Lancaster Formation (‘Fern Ledges’) of Saint John, New Brunswick, Canada. J Geol Soc Lond. 2007;164(5):945–57.
Fayers SR, Trewin NH. A hexapod from the Early Devonian Windyfield chert, Rhynie, Scotland. Palaeontology. 2005;48(5):1117–30.
Fayers SR, Dunlop JA, Trewin NH. A new Early Devonian trigonotarbid arachnid from the Windyfield Chert, Rhynie, Scotland. J Syst Palaeontol. 2005;2(4):269–84.
Garwood RJ, Dunlop JA. Morphology and systematics of Anthracomartidae (Arachnida: Trigonotarbida). Palaeontology. 2011;54(1):145–61.
Garwood RJ, Sutton MD. X-ray micro-tomography of Carboniferous stem-Dictyoptera: new insights into early insects. Biol Lett. 2010;6:699–702.
Garwood RJ, Dunlop JA, Sutton MD. High-fidelity X-ray micro-tomography reconstruction of siderite-hosted Carboniferous arachnids. Biol Lett. 2009;5:841–4.
Giribet G, Vogt L, González AP, Abel PG, Prashant S, Kury AB. A multilocus approach to harvestman (Arachnida: Opiliones) phylogeny with emphasis on biogeography and the systematics of Laniatores. Cladistics. 2010;26(4):408–37.
Gould SJ. The structure of evolutionary theory. Cambridge: Belknap; 2002.
Gould SJ, Eldredge N. Punctuated equilibria: the tempo and mode of evolution reconsidered. Paleobiology. 1977;3(2):115–51.
Gradstein FM, Ogg JG, Smith AG. International stratigraphic chart. Cambridge: Cambridge University Press; 2009.
Grimaldi DA. 400 million years on six legs: on the origin and early evolution of Hexapoda. Arthropod Struct Dev. 2010;39:191–203.
Grimaldi DA, Engel MS. Evolution of the insects. Cambridge: Cambridge University Press; 2005.
Gullan PJ, Cranston PS. The insects: an outline of entomology—fourth edition. Oxford: Blackwell; 2010.
Hadley NF. Adaptational biology of desert scorpions. J Arachnol. 1974;2:11–23.
Hadley NF. The arthropod cuticle. Sci Am. 1986;255:104–12.
Hadley NF. Water relations of terrestrial arthropods. London: Academic; 1994.
Hartwell M. The First Industrial Revolution. The American Economic Review, vol. 57. Cambridge: Cambridge University Press; 1967.
Haupt J. Phylogenetic aspects of recent studies on myriapod sense organs. In: Camatini M, editor. Myriapod biology. London: Academic; 1979. p. 391–406.
Higashi M, Abe T, Burns TP. Carbon–nitrogen balance and termite ecology. Proc R Soc Lond Ser B: Biol Sci. 1992;249(1326):303–8.
Hopkin SP, Read HJ. The biology of millipedes. Oxford: Oxford University Press; 1992.
Inward D, Beccaloni G, Eggleton P. Death of an order: a comprehensive molecular phylogenetic study confirms that termites are eusocial cockroaches. Biol Lett. 2007;3:331–5.
Jenner RA. Higher-level crustacean phylogeny: consensus and conflicting hypotheses. Arthropod Struct Dev. 2010;39:143–53.
Jeram AJ. Scorpions from the Viséan of East Kirkton, West Lothian, Scotland, with a revision of the infraorder Mesoscorpionina. Trans Royal Soc Edinburgh, Earth Sci. 1994a;84:283–99.
Jeram AJ. Carboniferous Orthosterni and their relationship to living scorpions. Palaeontology. 1994b;37(3):513–50.
Jeram AJ, Selden PA, Edwards D. Land animals in the Silurian: Arachnids and myriapods from Shropshire, England. Science. 1990;250:658–61.
Johnson EW, Briggs DEG, Suthren RJ, Wright JL, Tunnicliff SP. Non-marine arthropod traces from the subaerial Ordovician Borrowdale volcanic group, English Lake District. Geol Mag. 1994;131(3):395–406.
Kamenz C, Dunlop JA, Scholtz G, Kerp H, Hass H. Microanatomy of Early Devonian book lungs. Biol Lett. 2008;4:212–5.
Kenrick P, Crane PR. The origin and early evolution of plants on land. Nature. 1997;389:33–9.
Klass KD, Kristensen NP. The ground plan and affinities of hexapods: recent progress and open problems. Annales de la Société Entomologique de France. 2001;37(1–2):265–98.
Krapf D. Verhaltensphysiologishe Untersuchungen zum Beutefang von Skorpionen mit besonderer Berücksichtigung der Trichobothrien. PhD thesis, University of Würzburg; 1986.
Labandeira CC, Beall BS. Arthropod terrestriality. In: Culver SJ, editor. Arthropod palaeobiology. Short Courses in Palaeontology Number Three. Knoxville: Palaeontological Society; 1990. p. 214–32.
Legg DA, Garwood RJ, Dunlop JA, and Sutton MD. A taxonomic revision of Orthosternous scorpions from the English Coal-Measures aided by X-ray micro-tomography. Palaeontologia Electronica; 2011 (in press).
Levi HW. Adapations of respiratory systems of spiders. Evolution. 1967;21(3):571–83.
Lewis JGE. The biology of centipedes. Cambridge: Cambridge University Press; 2007.
Little C. The colonisation of land: origins and adaptations of terrestrial animals. Cambridge: Cambridge University Press; 1983.
Lourenço WR, Gall JC. Fossil scorpions from the Buntsandstein (Early Triassic) of France. Comptes Rendus Palevol. 2004;3(5):369–78.
Machado G, Pinto-da-Rocha R, Giribet G. What are harvestmen? In: Pinto-da-Rocha R, Machado G, Giribet G, editors. Harvestmen: the biology of Opiliones. Cambridge: Harvard University Press; 2007. p. 1–13.
Meßlinger K. Fine structure of scorpion trichobothria (Arachnida, Scorpiones). Zoomorphology. 1987;107(1):49–57.
Modesto SP, Hirst S, Reisz RR. Arthropod remains in the oral cavities of fossil reptiles support inference of early insectivory. Biol Lett. 2009;5:838–40.
Nelson CE. On the persistence of unicorns: the trade-off between content and critical thinking revisited. In: Pescosolido BA, Aminzade R, editors. The social worlds of higher education: handbook for teaching in a new century. Thousand Oaks: Pine Forge Press; 1999. p. 168–84.
Norton RA, Bonamo PM, Grierson JD, Shear WA. Oribatid mite fossils from a terrestrial Devonian deposit near Gilboa, New York. J Paleontol. 1988;62(2):259–69.
Pennock RT. God of the gaps: the argument from ignorance and the limits of methodological naturalism. In: Petto AJ, Godfrey LR, editors. Scientists confront intelligent design and creationism. New York: W.W. Norton; 2007. p. 309–38.
Plotnick RE, Kenig F, Scott AC, Glasspool IJ, Eble CF, Lang WJ. Pennsylvanian paleokarst and cave fills from northern Illinois, USA: a window into Late Carboniferous environments and landscapes. PALAIOS. 2009;24(10):627–37.
Polis GA. The biology of scorpions. Palo Alto: Stanford University Press; 1990.
Prave AR. Life on land in the Proterozoic: evidence from the Torridonian rocks of northwest Scotland. Geology. 2002;30:811–4.
Rasmussen B, Blake TS, Fletcher IR, Kilburn MR. Evidence for microbial life in synsedimentary cavities from 2.75 Ga terrestrial environments. Geology. 2009;37(5):423–6.
Raven JA. Comparative physiology of plant and arthropod land adaptation. Philos Trans R Soc Lond Ser B: Biol Sci. 1985;309(1138):273–88.
Reissland A, Görner P. Trichobothria. In: Barth FG, editor. Neurobiology of arachnids. Berlin: Springer; 1985. p. 138–61.
Retallack GJ. Scoyenia burrows from Ordovician palaeosols of the Juniata Formation in Pennsylvania. Palaeontology. 2001;44(2):209–35.
Retallack GJ, Feakes C. Trace fossil evidence for Late Ordovician animals on land. Science. 1987;235:61–3.
Rice CM, Ashcroft WA, Batten DJ, Boyce AJ, Caulfield JBD, Fallick AE, et al. A Devonian auriferous hot spring system, Rhynie, Scotland. J Geol Soc Lond. 1995;152(2):229–50.
Roberts MBV. Biology: a functional approach—fourth Edition. Cheltenham: Nelson Thornes; 1986.
Rößler R, Dunlop JA, Schneider JW. A redescription of some poorly known Rotliegend arachnids from the Lower Permian (Asselian) of the Ilfeld and Thuringian Forest Basins, Germany. Paläontologische Zeitschrift. 2003;77(2):417–27.
Ruppert EE, Smith PR. The functional organization of filtration nephridia. Biol Rev. 1988;63(2):231–58.
Ruppert EE, Fox R, Barnes RD. Invertebrate zoology: a functional evolutionary approach—seventh edition. Pacific Grove: Brooks/Cole; 2003.
Sahney S, Benton MJ. Recovery from the most profound mass extinction of all time. Proc R Soc Lond Ser B: Biol Sci. 2008;275:759–65.
Schawaller W, Shear WA, Bonamo PM. The first Paleozoic pseudoscorpions (Arachnida, Pseudoscorpionida). Am Mus Novit. 1991;3009:1–17.
Schmitz A, Perry SF. Bimodal breathing in jumping spiders: morphometric partitioning of the lungs and tracheae in Salticus scenicus (Arachnida, Araneae, Salticidae). J Exp Biol. 2001;204(24):4321–34.
Scholtz G, Kamenz C. The book lungs of Scorpiones and Tetrapulmonata (Chelicerata, Arachnida): evidence for homology and a single terrestrialisation event of a common arachnid ancestor. Zoology. 2006;109:2–13.
Scott EC. Evolution vs. creationism: an introduction—second edition. Westport: Greenwood Press; 2009.
Selden PA, Edwards D. Colonisation of the land. In: Allen KC, Briggs DEG, editors. Evolution and the fossil record. London: Belhaven Press; 1990. p. 122–52.
Selden PA, Jeram AJ. Palaeophysiology of terrestrialisation in the Chelicerata. Trans Royal Soc Edinburgh, Earth Sci. 1989;80:303–10.
Selden PA, Shear WA, Bonamo PM. A spider and other arachnids from the Devonian of New York, and reinterpretations of Devonian Araneae. Palaeontology. 1991;34(2):241–81.
Shear WA. Gigantocharinus szatmaryi, a new trigonotarbid arachnid from the Late Devonian of North America (Chelicerata: Arachnida: Trigonotarbida). J Paleontol. 2000a;74(1):25–31.
Shear WA. The early development of terrestrial ecosystems. Nature. 2000b;351:283–9.
Shear WA, Bonamo PM. Devonobiomorpha, a new order of centipeds (Chilopoda) from the Middle Devonian of Gilboa, New York State, USA, and the phylogeny of centiped orders. Am Mus Novit. 1988;2927:1–30.
Shear WA, Edgecombe GD. The geological record and phylogeny of the Myriapoda. Arthropod Struct Dev. 2010;39:174–90.
Shear WA, Kukalová-Peck J. The ecology of Paleozoic terrestrial arthropods: the fossil evidence. Can J Zool. 1990;68(9):1807–34.
Shear WA, Selden PA. Rustling in the undergrowth: animals in early terrestrial ecosystems. In: Gensel PG, Edwards D, editors. Plants invade the land: evolutionary and environmental perspectives. New York: Columbia University Press; 2001. p. 29–51.
Shear WA, Bonamo PM, Grierson JD, Rolfe WDI, Smith EL, Norton RA. Early land animals in North America: Evidence from Devonian age arthropods from Gilboa, New York. Science 1984;224(4648):492–4.
Shear WA, Selden PA, Rolfe WDI, Bonamo PM, Grierson JD. New terrestrial arachnids from the Devonian of Gilboa, New York (Arachnida: Trigonotarbida). Am Mus Novit. 1987;2901:1–74.
Shear WA, Gensel PG, Jeram AJ. Fossils of large terrestrial arthropods from the Lower Devonian of Canada. Nature. 1996;384:555–87.
Shear WA, Jeram AJ, Selden PA. Centiped legs (Arthropoda, Chilopoda, Scutigeromorpha) from the Silurian and Devonian of Britain and the Devonian of North America. Am Mus Novit. 1998;3231:1–16.
Sheldon P. Plus ça change—a model for stasis and evolution in different environments. Palaeogeogr Palaeoclimatol Palaeoecol. 1996;127:209–27.
Shultz JW, Regier JC. Phylogenetic analysis of arthropods using two nuclear protein-encoding genes supports a crustacean/hexapod clade. Proc R Soc Lond Series B: Biol Sci. 2000;267:1011–9.
Skelton P. Evolution: a biological and palaeontological approach. New Jersey: Prentice Hall; 1993.
Snodgrass RE. Evolution of the Annelida: Onychophora and Arthropoda. Smithson Misc Collect. 1938;97(6):1–159.
Størmer L. Arthropods from the Lower Devonian (Lower Emsian) of Alken an der Mosel, Germany. Part 1: Arachnida. Senckenbergiana Lethaea. 1970;51:335–69.
Størmer L. Arthropods from the Lower Devonian (Lower Emsian) of Alken an der Mosel, Germany. Part 2: Xiphosura. Senckenbergiana Lethaea. 1972;53:1–29.
Størmer L. Arthropods from the Lower Devonian (Lower Emsian) of Alken an der Mosel, Germany. Part 3: Eurypterida, Hughmilleriidae. Senckenbergiana Lethaea. 1973;54:119–205.
Størmer L. Arthropods from the Lower Devonian (Lower Emsian) of Alken an der Mosel, Germany. Part 4: Eurypterida, Drepanopteridae, and other groups. Senckenbergiana Lethaea. 1974;54:359–451.
Størmer L. Arthropods from the Lower Devonian (Lower Emsian) of Alken an der Mosel, Germany. Part 5. Myriapods and additional forms, with general remarks on the fauna and problems regarding invasion of land by arthropods. Senckenbergiana Lethaea. 1976;57:87–183.
Størmer L. Gigantoscorpio willsi, a new scorpion from the Lower Carboniferous of Scotland and its associated preying microorganisms. Skrifter Utgitt av Det Norske Videnskaps–Akademi I Oslo I. Mathematisk-Naturvidenskabelig Klasse 1963; 8:1–171.
Strother PK, Battison L, Brasier MD, Wellman CH. Earth’s earliest non-marine eukaryotes. Nature. 2011;473:505–9.
Trewin NH, Fayers SR. A new crustacean from the Early Devonian Rhynie Chert, Aberdeenshire, Scotland. Trans Royal Soc Edinburgh, Earth Sci. 2007;93(4):355–82.
Trewin NH, Fayers SR, Kelman R. Subaqueous silicification of the contents of small ponds in an Early Devonian hot-spring complex, Rhynie, Scotland. Can J Earth Sci. 2003;40(11):1697–712.
Vogel BR, Durden CJ. The occurrence of stigmata in a Carboniferous scorpion. J Paleontol. 1966;40(3):655–8.
Wellman CH, Gray J. The microfossil record of early land plants. Philos Trans R Soc Lond Series B: Biol Sci. 2000;355(1398):717–31.
Wellman CH, Kerp H, Hass H. Spores of the Rhynie chert plant Aglaophyton (Rhynia) major (Kidston and Lang) D.S. Edwards, 1986. Rev Palaeobot Palynol. 2006;142(3–4):229–50.
Weygoldt P. Fighting, courtship, and spermatophore morphology of the whip spider Musicodamon atlanteus Fage, 1939 (Phrynichidae) (Chelicerata, Amblypygi). Zoologischer Anzeiger. 2002;241(3):245–54.
Whitford WG. Keystone arthropods as webmasters in desert ecosystems. In: Coleman DC, Hendrix PF, editors. Invertebrates as webmasters in ecosystems. Wallingford: CABI; 2000. p. 25–41.
Wilson HM. Juliformian millipedes from the Lower Devonian of Euramerica: implications for the timing of millipede cladogenesis in the Paleozoic. J Paleontol. 2006;80:638–49.
Wilson HM, Anderson LI. Morphology and taxonomy of Paleozoic millipedes (Diplopoda:Chilognatha: Archipolypoda) from Scotland. J Paleontol. 2004;78(1):169–84.
About this article
Cite this article
Garwood, R.J., Edgecombe, G.D. Early Terrestrial Animals, Evolution, and Uncertainty. Evo Edu Outreach 4, 489–501 (2011). https://doi.org/10.1007/s12052-011-0357-y
- Palaeozoic ecosystems