Abstract
We revisited the brachiopod fold hypothesis and investigated metamorphosis in the craniiform brachiopod Novocrania anomala. Larval development is lecithotrophic and the dorsal (brachial) valve is secreted by dorsal epithelia. We found that the juvenile ventral valve, which consists only of a thin layer that was previously described as periostracal, is not a valve and is not secreted by the same epithelia as the dorsal valve. It is secreted by the attachment area of the larva at the posterior-most tip of the posterior larval lobe. The same attachment area is used by larvae of rhynchonelliform brachiopods during metamorphosis to cement their pedicle to the substrate. N. anomala is therefore not initially attached by a valve but by material corresponding to pedicle cuticle. This is different to previous descriptions, which had led to speculations about a folding event in the evolution of Brachiopoda. We show that the “brachiopod fold hypothesis,” which argues that brachiopods are transversely “folded” across the ontogenetic anterior–posterior axis, should be rejected at least with respect to the craniiforms. The data now suggest that the Craniiformea may be a derived group within the Rhynchonelliformea. This interpretation suggests that the last common ancestor of the Craniiformea has lost the pedicle and the ventral valve in early juvenile development. Characters that have previously been considered to be shared between the Craniiformea and the Linguliformea (clade Inarticulata), such as a through-gut and missing hinge articulation, may thus be secondarily derived characters of the Craniiformea within the Rhynchonelliformea.
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Introduction
Brachiopoda is a marine animal phylum with a rich fossil record and approximately 370 recent species divided into the three clades, Craniiformea, Rhynchonelliformea, and Linguliformea (Williams et al. 1996; Zezina 2008). The evolution of the brachiopod body plan with two valves that enclose the soft tissue and a pedicle that attaches the animal to the substrate has puzzled researchers since the naming of the phylum by Duméril (1806). Brachiopods have since been deemed related to various phyla such as molluscs, bryozoans, and annelids and recently, based on molecular data, to nemerteans (Grey 1848; Huxley 1853; Morse 1870; Dunn et al. 2008).
Brachiopod internal relationships between the three clades, and the relation of brachiopods to phoronids, have not been completely resolved to date by molecular methods (Cohen et al. 1998; Cohen 2000, 2013; Cohen and Weydmann 2005; Sperling et al. 2011). Also, the comparative morphological analyses found an equal amount of characters shared among the Craniiformea and the Linguliformea (formerly the clade Inarticulata) and the Craniiformea and the Rhynchonelliformea (Carlson 1995). This has led to different outcomes in analyses concerning brachiopod internal phylogeny, depending on the chosen character polarities (Carlson 1995; Holmer et al. 1995; Williams et al. 1996). Characters shared among the craniiforms and the linguliforms include a through-gut, a circumferential mantle cavity, a muscular system consisting of oblique and two pairs of adductor muscles, as well as a transient median tentacle (Williams et al. 1996). Characters shared among the Craniiformea and the Rhynchonelliformea include a proteinaceous calcitic shell, a single row of tentacles on trocholophous lophophores, gonads suspended in mantle sinuses, and lecithotrophic larvae (Holmer et al. 1995; Williams et al. 1996).
There are various hypotheses about the evolution of the brachiopod body plan. During the years, four hypotheses have been put forward. 1. The ancestor of brachiopods was a tube-dwelling polychaete-like metameric worm with a hydraulic body construction (Gutmann et al. 1978). 2. The ancestor of brachiopods was an oligomerous worm with setae, protocoel, mesocoel, and three segments in the metacoel (Temereva and Malakhov 2011). 3. The ancestor of brachiopods was a halkieriid-like organism, comprising a worm-like body with sclerites and shells at the anterior and posterior end (Conway Morris and Peel 1995; Cohen et al. 2003). 4. Brachiopods evolved from sclerite-bearing, tube-dwelling, worm-like organisms such as the tommotiids Micrina, Eccentrotheca, and Paterimitra (Williams and Holmer 2002; Holmer et al. 2008, 2011; Skovsted et al. 2009a, b; Murdock et al. 2012).
In living brachiopods, members of each clade have a distinct mode of development. The larvae of Craniiformea are lecithotrophic, bilobed, with three pairs of dorsal setal bundles on the posterior lobe. The larvae of Rhynchonelliformea are lecithotrophic and have three lobes and four setal bundles at the mantle lobe, while the Linguliformea have planktotrophic, swimming juveniles (Nielsen 2005). Larvae of Craniiformea and Rhynchonelliformea metamorphose upon settlement. Swimming juveniles of Linguliformea do not undergo metamorphosis upon settlement because metamorphosis is mainly completed at the end of the embryonic stage in lingulids or shortly after hatching in the discinids (Lüter 2001, 2007; Popov et al. 2012). Hypotheses concerning the putative body plan of the ancestor of Brachiopoda often focus on the development of Novocrania anomala (Müller 1776) (previously assigned to several genera and therefore also referred to as Crania anomala or Neocrania anomala) (Lee and Brunton 1986, 2001), a member of the Craniiformea (Nielsen 1991; Popov et al. 1993; Conway Morris 1998; Cohen et al. 2003). It has been claimed that both valves in juveniles of N. anomala are secreted by mantle epithelia that originate at the dorsal side of the posterior lobe (Nielsen 1991). This notion has led to the conclusion that a “folding-event” happened during brachiopod evolution (Cohen et al. 2003; Malakhov and Kuzmina 2006). The concept was subsequently termed “brachiopod fold hypothesis,” according to which brachiopods are assumed to transversely “fold” across the larval anterior–posterior axis. According to this theory, the brachiopod body plan needs to be conceptually “unfolded” in order to make useful comparisons with the body plans of other animal phyla (Cohen et al. 2003). The body plan of Halkieria evangelista as a possible stem group brachiopod was used to support this view (Conway Morris and Peel 1995; Cohen et al. 2003). However, the hypothesis that H. evangelista represents a brachiopod stem species has since been questioned (Vinther and Nielsen 2005).
The metamorphosis of N. anomala was described in detail with the claim that prior to metamorphosis, “most larvae become inactive and lie curled together on the bottom with the pair of ventral muscles maximally contracted” (Nielsen 1991). We tested whether these curled, inactive larvae are able to metamorphose by live observation, the use of F-actin labeling, confocal laser scanning microscopy, and scanning electron microscopy.
Materials and methods
Collection of developmental stages
Adults of N. anomala were obtained by dredging in the vicinity of the Sven Lovén Centre for Marine Sciences, Gullmarsfjord, Sweden (58°15′921′′N, 11°25′103′′E), in September 2008. The rocks with attached N. anomala were kept in running seawater at 14 °C. Adults were removed from the rocks and dissected. Eggs and sperm were removed with pulled glass pipettes, washed, and left in filtered seawater in separate beaker glasses. Fertilized eggs were regularly checked for germinal vesicle breakdown. Sperm cells were monitored for motility under a compound microscope. When eggs were ready for fertilization (approximately 12 h after dissection), 2 ml of a highly diluted sperm suspension was added. Embryos and larvae were fixed at various stages from 4 h after fertilization (hpf) to 17 days after settlement in 4 % paraformaldehyde in 0.1 M phosphate buffer (PB) for 90 min. Thereafter, larvae were washed three times for 15 min each in 0.1 M PB and finally stored in 0.1 M PB containing 0.1 % NaN3 at 4 °C.
Scanning electron microscopy
For scanning electron microscopy, the specimens were dehydrated in a graded ethanol and acetone series, critical point dried, sputter coated with gold, and investigated using a Zeiss Supra 35VP scanning electron microscope.
Confocal laser scanning microscopy
The musculature was stained with phalloidin. Prior to staining, fixed larvae were washed in PB three times for 15 min each. Then, the larvae were incubated for 1 h in PB containing 0.2 % Triton X-100 (Sigma-Aldrich, St. Louis, MO, USA) to permeabilize the tissue, left overnight at 4 °C in 0.1 M PB containing 0.2 % Triton X-100 and 1:40 diluted Alexa Fluor 488 phalloidin (Invitrogen, Molecular Probes, Eugene, OR, USA), and subsequently washed in 0.1 M PB that was changed three times every 15 min. Finally, the specimens were embedded in Fluoromount G (Southern Biotech, Birmingham, AL, USA) on glass slides. Negative controls omitting the phalloidin dye were performed in order to test for autofluorescence and rendered no signal. The stained larvae and juveniles were analyzed with a Leica DM IRE2 fluorescence microscope equipped with a TCS SP2 AOBS laser scanning device (Leica Microsystems, Wetzlar, Germany). Animals were scanned with 0.16–0.49 μm step size, and the resulting image stacks were merged into maximum projection images. Light micrographs were recorded to allow overlay with the CLSM images for exact orientation and localization of the muscle systems within the animals.
Schematic drawings and figure plates
Drawings and micrographs were assembled with Photoshop CS3 and Illustrator CS3 software (Adobe, San Jose, CA, USA).
Results
Overview of larval development at 14 °C
Cleavage is radial and the first two divisions are holoblastic (Figs. 1a, b, 2a, b). The blastula is spherical (Fig. 2c) and invagination starts at around 18 h after fertilization (hpf) (Fig. 2d). The blastocoel disappears completely at the gastrula stage (Fig. 1c). Subsequently, the gastrula elongates and the blastopore comes to lie at the posteroventral side of the swimming larva (Figs. 1d, 2e). The elongated gastrula differentiates into two larval lobes, that is, an anterior lobe and a posterior lobe (Figs. 1e, f, 2f, g). Larval development is complete with the establishment of three pairs of dorsal setal bundles on the posterior lobe (Figs. 1g, 2h). Now, the larvae are competent for metamorphosis and swim driven by the cilia that are around the anterior lobe. At this stage, the larvae have setae pouch muscles at the base of each bundle of setae. These setae pouch muscles are interconnected by medioventral longitudinal and transversal muscles (for a detailed description of myogenesis and larval myoanatomy of N. anomala see Altenburger and Wanninger 2010).
Metamorphosis
At a water temperature of 14 °C, metamorphosis takes place around 6–10 days after fertilization (dpf). During metamorphosis, the larva lies flat on the surface with the ventral side pointing toward the substrate. The anterior lobe and the posterior end of the posterior lobe are bent ventrally, thus exposing the dorsal posterior lobe to the environment (Fig. 4a–c). The larva attaches itself to the substrate with the posterior-most tip of the posterior lobe. The dorsal mantle develops from an oval-shaped area on the dorsal side of the posterior lobe and secretes the first-formed brachial valve (Figs. 3b, 4d–f). The larval lobes are retained during the first steps of metamorphosis and are subsequently remodeled to form the lophophore and other adult organs (Figs. 1h, 2i).
Prior to settlement, the larva swims along the bottom of the culture dish, probably in order to test whether the substrate is suitable for settlement. Larvae ready for metamorphosis appear to be slightly curled, as they turn the anterior lobe and the posterior tip of the posterior lobe ventrally. However, strongly curled larvae with maximally contracted musculature are arrested in their development and unable to metamorphose (Fig. 3a, d). The larval musculature of healthy, settling, and metamorphosing individuals remains elongated and relaxed (i.e., non-contracted) prior its resorption in the juvenile (Fig. 3e). There is no ventral mantle at this stage of development (Figs. 2i, 3c). Some days after settlement, the larval lobes give rise to the adult tissues including the lophophore (Fig. 3f).
Discussion
Development and regional specification during N. anomala embryogenesis were described previously, but interpreted differently (Nielsen 1991; Freeman 2000). According to all observations (published previously and presented herein), the cilia on the anterior lobe function as locomotory organ of the larva prior to metamorphosis. Once the larva has found a suitable place for settlement, it attaches itself to the substrate with the posterior-most tip of the posterior lobe, which is bent ventrally. A distinguishable domain of cells between the setal bundles on the dorsal side of the posterior lobe participates in the formation of the mantle that will secrete the dorsal valve during metamorphosis (Fig. 4d, e) (Nielsen 1991; Freeman 2000). Nielsen (1991, page 25) states moreover: “…the brachial (‘dorsal’) valve was secreted by the anterior part of the dorsal side of the larva while the pedicle (‘ventral’) valve was secreted by the posterior part of the dorsal side, i. e. both valves are actually dorsal!”.
We reject this interpretation for several reasons. First of all, the attachment area of the larvae is the posterior-most tip of the posterior lobe; thus, one cannot make a distinction between dorsal and ventral at this point. It is further not clear which epithelia form the ventral mantle that would be needed to secrete the ventral valve. It was assumed that the ventral valve is secreted by and spreads from the attachment area (Nielsen 1991). We agree with the assumption that cuticle spreads from the attachment area. However, we disagree that it is a valve, as the juveniles in our experiments did not develop a ventral mantle that could secrete the ventral valve within the first 17 days after metamorphosis. This is seen in the specimen shown in Fig. 4d–f, which has a mantle on the dorsal side of the larva, but not on the ventral side. The juvenile specimens in Figs. 2i and 3c, which are shown from the ventral side, likewise have a dorsal valve but neither a ventral valve nor a ventral mantle. Only the attachment area is visible at this stage of development, which makes it clear that the absence of a ventral mantle and a ventral valve is not due to experimental procedures.
The development of the ventral valve in postmetamorphic stages of N. anomala is delayed. A similar delay of ventral valve development is found in juvenile stages of the Ordovician craniid Orthisocrania and in some paleozoic rhynchonelliforms such as Antigonambonites (Popov et al. 2007, 2010). Later stages of N. anomala show a ventral valve consisting of a very thin periostracal layer with which the animals cement themselves to the substrate (Rowell 1960). According to these observations, the ventral mantle does not begin to secrete calcite until the animals are in the “12–14 pairs of cirri stage” and about 1 mm wide (Rowell 1960).
Generally, the ventral valve of adult N. anomala shows “a predominantly organic layer … survives within the central area of the pedicle valve of living Crania” (Williams and Wright 1970, page 48). In mature adults, over 10 mm in diameter, a calcitic thickening exceeding 0.5 mm is limited to an anterior arc which forms a dorsally convex submarginal rim so that a central area, between 3 and 5 mm across, remains only partially covered by the merest mineral film (Williams and Wright 1970).
It is well established that the Craniida occur in the fossil record not before the Lower Ordovician with the clade Pseudocrania (Bassett 2000). This is late compared to the Linguliformea and the Rhynchonelliformea, which are found much earlier in the fossil record, namely already in the Lower Cambrian (Williams et al. 2007). Many phylogenetic analyses hint toward the Craniiformea as being derived within Brachiopoda, based on both morphological and molecular data (Carlson 1995; Holmer et al. 1995; Cohen 2000; Cohen and Weydmann 2005). It thus makes no sense to hypothesize a potential body plan ground pattern based on the development of N. anomala, because of the risk to take an apomorphy of a subclade as a character for the whole taxon (Wägele 2005).
The attachment area of N. anomala is at the posterior-most tip of the posterior lobe (Nielsen 1991). Also, the lecithotrophic larvae of rhynchonelliform brachiopods attach themselves with the posterior-most tip of their pedicle lobe to the substrate at the onset of metamorphosis (Altenburger and Wanninger 2009). This pedicle lobe contains the primordium of the juvenile pedicle that forms after metamorphosis (Stricker and Reed 1985a). In the rhynchonelliform larva, the dorsal and ventral valves are secreted by mantle epithelium that is formed on the underside of the skirt-like mantle lobe, which is reverted over the apical lobe during metamorphosis (Stricker and Reed 1985b, c). In N. anomala, no inversion takes place. Here, the dorsal valve is secreted from the dorsal mantle after settlement, and there is no ventral valve at this stage. In our view, the cementing cuticle of N. anomala may represent the same material that is used to attach the pedicle to the substrate in rhynchonelliform brachiopods. Rhynchonelliform brachiopods glue themselves to the substrate by a sticky secretion for tentative attachment, followed by secretion of a layer of cuticle which is secreted between the glued pedicle and substrate for permanent attachment (Stricker and Reed 1985a; Chuang 1996). From this perspective, the lecithotrophic larvae of Rhynchonelliformea and Craniiformea are not that different. Because if one takes the skirt-like mantle that constitutes the mantle lobe of three-lobed rhynchonelliform larvae away and consequently the ability to invert the skirt-like lobe over the apical lobe during metamorphosis, the remaining larva is bilobed. The body plan of N. anomala could resemble an early stage rhynchonelliform larva before it separates the mantle from the pedicle lobe. In the rhynchonelliform Terebratalia transversa (Sowerby 1846), the mantle lobe forms during a second constriction as an outgrowth from the pedicle lobe from the dorsal side of the larva and slowly grows around both sides of the larva toward the ventral side (Stricker and Reed 1985b; Freeman 2003). Larva of N. anomala might keep the prospective mantle cells, which later also develop the setal sacs on their dorsal side, without developing a mantle lobe.
These considerations lead us to the conclusion that Craniiformea might be a derived group within Rhynchonelliformea that has lost the pedicle and the ventral valve in early postmetamorphic development. This view is supported by the following characters uniting the craniiforms and the rhynchonelliforms: 1. Lecithotrophic larvae with an attachment area at the posterior-most tip of the larva, 2. calcitic shells with punctae (Williams 1997), 3. the gonads are placed within the mantle canals (Popov et al. 1993), and 4. one pair of oblique muscles is present (Popov et al. 1993).
The following characters have previously been used to unite the Craniiformea with the Linguliformea (to form the clade Inarticulata), but these may more likely represent apomorphies of the Craniiformea within the Rhynchonelliformea: a secondary through-gut at the posterior body wall and loss of hinge articulation because of loss of the ventral valve in early postmetamorphic development. The craniiform body plan is thus derived from the rhynchonelliform body plan and the Craniiformea may represent a subclade of the Rhynchonelliformea. A naming of this clade has already been proposed as the Calciata (Popov et al. 1993).
Our observations contribute significantly to the understanding of brachiopod interrelationships which are still hotly debated, especially with regard to the position of Phoronida (Helmkampf et al. 2008; Sperling et al. 2011; Cohen 2013; Cohen and Bitner 2013). In relation to our findings, this is relevant because in a study based on nuclear housekeeping genes combined with three ribosomal genes, the craniids behave as a “rogue taxon” that is placed with little statistical resolution at the base of Brachiopoda (Sperling et al. 2011).
Coming back to the metamorphosis of N. anomala, we want to point out a further important difference to the previously described mechanisms. This concerns the ability of maximally contracted curled larvae to metamorphose. Although we observed curled larvae, these are arrested in development and do not metamorphose. While curled larvae have contracted muscles (Fig. 3d), all individuals that successfully completed metamorphosis in our study (N = 15) showed relaxed, that is, expanded medioventral longitudinal muscles after settlement and prior to resorption (Fig. 3e; see also Altenburger and Wanninger 2010 for a general description of the musculature in N. anomala). Also, the anterior–posterior alignment of the gut of the adults is incompatible with a “folding” event of the body axis during metamorphosis (Williams and Carlson 2007). Another argument is the presence of complete ventral and dorsal mesenteries in N. anomala (Chuang 1960). Phoronids, which are “folded” animals, have developed lateral mesenteries instead (Bailey-Brock and Emig 2000).
Especially, the hypothesis of a “brachiopod fold” put forward by Cohen et al. (2003) focuses on the “curling” event prior to metamorphosis. However, if one wants to make this comparison, the “fold” would be between the anterior and the posterior lobe of the larva. To arrive at a brachiopod body plan from this folding event, one valve had to be secreted from the dorsal anterior lobe and the other one from the dorsal posterior lobe. But this is not the case and it was never reported that way.
Accordingly, the larvae do neither fold before nor during metamorphosis; they only bend the anterior lobe and the posterior-most tip of the posterior lobe ventrally. Thus, hypotheses arguing for a “brachiopod fold event” during brachiopod evolution are not supported by larval development and metamorphosis of N. anomala and should therefore be rejected.
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Acknowledgments
We thank Andreas Schmidt-Rhaesa for helpful comments that significantly improved the manuscript. We are grateful to the staff at the Sven Lovén Centre for Marine Sciences in Kristineberg, Sweden, for providing laboratory space. Gary Wife (University of Uppsala) is thanked for assistance with the scanning electron microscope. Lars Holmer acknowledges support from the Swedish Research Council (VR 2009-4395, 2012-1658).
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Altenburger, A., Wanninger, A. & Holmer, L.E. Metamorphosis in Craniiformea revisited: Novocrania anomala shows delayed development of the ventral valve . Zoomorphology 132, 379–387 (2013). https://doi.org/10.1007/s00435-013-0194-3
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DOI: https://doi.org/10.1007/s00435-013-0194-3