Lovén's Law

Lovén (Reference Lovén1874) first noticed that in irregular echinoids the first basicoronal plates differed in size in the two ambulacral columns of the corona and furthermore that the larger plate occurred alternately on different sides of the ambulacrum. He instituted a system of denoting the ambulacra by Roman numerals in a clockwise direction as seen in oral view, starting with the ambulacrum immediately clockwise of the periproct (Fig. 1). He further identified the two ambulacral columns as a and b, so a shorthand statement of the position of the larger plates in Lovén's Law (as it has become known) is:

Figure 1. Lovén's Law as originally proposed by Lovén (Reference Lovén1874) and seen in the irregular echinoid Echinocyamus bisexus Kier, Reference Kier1968. Ambulacra are indicated by Roman numerals. Individual columns within ambulacra indicated by the letters A and B. Lovén's Law states that starting with ambulacrum I and proceeding clockwise in oral view, the larger basicoronal plates occur in columns IA, IIA, IIIB, IVA, VB. An = anus; H = hydropore (on the opposite surface of the echinoid); M = mouth (redrawn from Hotchkiss, Reference Hotchkiss1978, fig. 1).

Lovén further designated interambulacra by Arabic numerals clockwise in oral view, starting with the interambulacrum between his ambulacra I and II. Under this designation, the echinoid hydropore (madreporite) lies in interambulacrum 2 (H, Fig. 1). The only truly interambulacral structure in echinoid coronae is the interradial suture. Four columns of plates are added at the edge of the ocular plates, according to the so-called ocular plate rule (e.g., David et al., Reference David, Mooi, Telford, Emson, Smith and Campbell1995): the central pair of pore-bearing, ambulacral plates, and a single column of non-pore-bearing, adambulacral plates, one on either side (Mooi and David, Reference Mooi, David, Waters and Maples1997). All four columns are part of the axial skeleton, so in echinoids it is appropriate to restrict the term interambulacral to a position between ambulacra.

In any column of alternating pairs of plates truncated at a smooth surface, such as the edge of the mouth of an echinoid, it is inevitable that one plate will be smaller than the other. Equally, in any system of five ambulacra with a motif that alternates from one ambulacrum to the next, it is inevitable that one motif will occur three times and the other only twice. Furthermore, a unique pair of ambulacra occurs, which are both adjacent and identical.

What justifies the term ‘Lovén's Law’ is the fact that of the 32 possible arrangements of alternating ambulacral plates (10 Lovén-like and 22 non-Lovénian) only the one first described by Lovén is known to occur in echinoids. Furthermore, it is also present in all regular echinoids that can be scored, not just irregulars. The uniqueness of this pattern can be tested using reliable independent landmarks. In echinoids, the hydropore is always in Lovén's interambulacrum 2, in echinoid larval development the closure of the ring canal is in interambulacrum 4 in all examples studied so far (Saucède et al., Reference Saucède, Mooi and David2003, Reference Saucède, Mooi and David2007; Tsuchimoto et al., Reference Tsuchimoto, Yamada and Yamaguchi2011), and in irregular echinoids the periproct is always in interambulacrum 5. Finally, the unique pair of ambulacra are I and II. Thus, use of the term ‘Lovén's Law’ in echinoids seems justified.

In a collateral study of Paleozoic lysophiurine ophiuroids, 107 rays out of 113 scorable rays, when aligned using the madreporite, conformed with expression of Lovén's Law. On a per-ray basis, the fidelity was 0.947. Fidelity calculated for five rays is (0.947)⁵ = 0.762 (Hotchkiss, Reference Hotchkiss1995, p. 424, 432–435). At that time, Lovén's Law was not explicit in any ‘cystoid’ despite purposeful searching (Jackson, Reference Jackson1929, p. 495; Mortensen, Reference Mortensen1930, p. 343; Hotchkiss, Reference Hotchkiss1995, p. 418; Smith, Reference Smith1997).

Modification

David et al. (Reference David, Mooi, Telford, Emson, Smith and Campbell1995) showed that ‘Lovén's Law’ is more than an interesting pattern found in echinoids, but results from the mode of growth of the ambulacra and the sequence of formation of the ambulacral plates. In particular, they showed that the smaller basicoronal plate was always the first plate to develop in each ambulacrum. David et al. (Reference David, Mooi, Telford, Emson, Smith and Campbell1995, p. 160, fig. 3) determined this by locating the edge-defining transverse sutures in the ambulacral columns. Thus, it seems to us to make sense to identify the first ambulacral plate when trying to recognize ‘Lovén's Law’ in other classes of echinoderms. By chance, Lovén chose the second plate in each ambulacrum by describing the positions of the larger basicoronal plate in each ambulacrum of echinoids. Furthermore, we believe that consideration of the details of ambulacral growth is the key to understanding ambulacral homologies and recognizing Lovén's Law in other classes of echinoderms.

Secondly, Lovén identified his ambulacral columns by the letters a and b. Hotchkiss (Reference Hotchkiss1978, p. 538), in the first attempt to find ‘Lovén's Law’ in another echinoderm class (the ophiuroids), described the offset of ambulacral plates as ‘in Advance of’ (A) or ‘Behind’ (B) plates of the opposite column. We think these two meanings may lead to confusion since the first plate is always behind the second, but may occur in ambulacral column a. So, we recommend using the terms left (L) and right (R), as seen in oral view when looking down the ambulacrum in the direction of growth. Clockwise (C) and anticlockwise (A) are possible alternatives, but A and C might lead to confusion with the ambulacra using Carpenter's (Reference Carpenter1884, Reference Carpenter1891) system of ambulacral notation (see below).

Finally, the identity of the ambulacra in echinoderms is subject to three different notations (Fig. 2). Lovén's (Reference Lovén1874) has precedence and no doubt echinoid workers will continue to use it. Carpenter (Reference Carpenter1884) introduced an alternative system for the crinoids. He also designated ambulacra clockwise in oral view, but used letters of the alphabet (A–E) and started with the ambulacrum opposite the periproct. Carpenter designated interambulacra by means of the adjacent ambulacra. Thus, the interambulacrum containing the periproct, hydropore, and gonopore in most blastozoans is the CD interambulacrum (Fig. 2). Carpenter (Reference Carpenter1891) extended this system to blastoids and ‘cystoids.’ Then Jaekel (Reference Jaekel1899), thinking he was following Lovén's system, used Roman numerals clockwise from the ambulacrum immediately clockwise of the periproct for edrioasteroids (his Thecoidea) and ‘cystoids.’ Unfortunately, the periproct is not in homologous interambulacra in irregular echinoids versus other Paleozoic echinoderms, as determined from simultaneous expression of Lovén's Law and 2-1-2 symmetry in the edrioasteroids, Astrocystites Whiteaves, Reference Whiteaves1897, and Walcottidiscus Bassler, Reference Bassler1935 (= Stromatocystites of Hotchkiss, Reference Hotchkiss1995, figs. 3, 4). Carpenter letters are arranged in 2-1-2 symmetry as DE-A-BC, and Lovén's numerals are arranged in 2-1-2 symmetry as V,I - II - III,IV. Jaekel's influence on blastozoan studies is about as profound as Lovén's on echinoid research. Given the confusion that arises from using the same notation to identify different ambulacra using Lovén's and Jaekel's systems, we think a more unambiguous statement of Lovén's Law can be derived using left (L) and right (R), plus Carpenter's ambulacra (Fig. 3). So, identifying the first ambulacral plate or lateral branch of the radial water vessel and starting with Carpenter's ambulacrum A, we get a pattern in echinoids and in other classes of echinoderms of (Fig. 3):

Figure 2. Comparison of systems of ambulacral designation as seen in oral view. (1) Carpenter's rays (A–E) compared with Jaekel's ambulacra (I–V) in edrioasteroids. (2) Carpenter's rays (A–E) compared with Lovén's (I–V) in irregular echinoids. Note that although Jaekel (Reference Jaekel1899) thought he was copying Lovén (Reference Lovén1874) by designating the ambulacrum immediately clockwise to the periproct (Pe) by Roman numeral I, the ambulacra do not coincide because the periproct is in different interambulacra in edrioasteroids and irregular echinoids. Carpenter's (Reference Carpenter1884, Reference Carpenter1891) system using letters A–E is unambiguous. H = hydropore; M = mouth; Pe = periproct (surrounding the anus). Note that the hydropore is on the opposite surface in (2). Modified from Paul and Smith (Reference Paul and Smith1984, fig. 17, p. 472).

Figure 3. Modified version of Lovén's Law using Left (L) and Right (R) terminology and Carpenter's rays (A–E). Note that starting with Carpenter's ray A and identifying the first basicoronal plate in each ambulacrum, Lovén's Law becomes AR, BL, CR, DL, ER and the unique pair of identical adjacent ambulacra are E and A. An = anus; H = hydropore (on the opposite surface of the echinoid); M = mouth (modified from Hotchkiss, Reference Hotchkiss1978, fig. 1).

This gives three Right and two Left and the unique pair of identical adjacent ambulacra is EA (Fig. 3). Herein, we assume that a ‘Lovén-like’ pattern with cyclic RLRLR corresponds exactly to ‘Lovén's Law.’ This becomes our working hypothesis, and implies that Carpenter's ambulacra in echinoids are as indicated in Figure 3.

For further context, there are 2⁵ = 32 differing pentaradiate cyclic arrangements of biserial alternating ambulacral plates that could surround the peristome. The 32 are made up from just eight distinct cyclic patterns: RRRRR, RRRRL, RRRLL, RRLRL, LLLLL, LLLLR, LLLRR, and LLRLR. The patterns RRRRR and LLLLL can occur in only one arrangement, whereas five cyclic permutations apply to the six other patterns; hence [2 + (5 × 6) = 32]. The five cyclic versions of RRLRL are all Lovén-like, but only one expresses Lovén's law in any instance. In addition, we recognize the five cyclic versions of LLRLR as Lovén-like and of interest. From prior work, we are aware that probability of phenotypes is not uniformly distributed over the 32 slots of this outcome space (Hotchkiss, Reference Hotchkiss1978, Reference Hotchkiss1995). The probability is concentrated in the slot where Lovén's law is expressed, enabling a Bayesian heuristic for the working hypothesis (Jefferys and Berger, Reference Jefferys and Berger1992).

Testing homologies and additional assumptions

To test the working hypothesis above requires a reliable independent landmark. The gonopore cannot be used because echinoids typically have five. The periproct is known to migrate even within blastozoan superfamilies, both from just above the basal circlet to the oral surface (in hemicosmitoid rhombiferans) and, more importantly, from the CD interambulacrum to the BC interambulacrum (in glyptocystitoid rhombiferans). Furthermore, irregular echinoids only arose in the Early Jurassic (e.g., Saucède et al., Reference Saucède, Mooi and David2007). If the migration of the periproct outside the apical disc were a random process, there would be a 1 in 5 chance that irregular echinoids developed an eccentric periproct between exactly the same two ambulacra as early Paleozoic edrioasteroids and blastozoans. Saucède et al. (Reference Saucède, Mooi and David2003) have shown that posterior migration of the periproct in echinoids occurred eight separate times, but only once did the periproct succeed in moving outside the apical disc, leading to the monophyletic Irregularia. Nevertheless, all attempts involved the same anterior-posterior axis, so it would seem the process was not random as far as echinoids were concerned.

Paul and Smith (Reference Paul and Smith1984, fig. 16, p. 471) regarded the hydropore as a reliable landmark to determine ambulacral homologies. Although not explicitly stated, Paul and Smith (Reference Paul and Smith1984, p. 472, fig. 17; Fig. 2) illustrated Jaekel's numbering of ambulacra on the left and Lovén's on the right. Furthermore, the hydropore is always in the CD interambulacrum of edrioasteroids and blastozoans, which implies that Carpenter's ambulacrum A is equivalent to Lovén's ambulacrum V. However, using Lovén's Law to determine ambulacral homology implies that Carpenter's ambulacrum A is equivalent to Lovén's ambulacrum II. So, if one accepts the hydropore as a reliable landmark, then Lovén's Law cannot be applied to other classes of echinoderms. Alternatively, if Lovén's Law does determine ambulacral homologies, then the hydropore is an unreliable landmark. The latter seems distinctly possible given that hydropores occur in all five interambulacra in some ophiuroids (Hyman, Reference Hyman1955, p. 613) and some crinoids (Breimer, Reference Breimer, Moore and Teichert1978, p. T15, T46, fig. 30).

Body plan comparisons at lower taxonomic levels can employ homology markers that are not valid between classes. The madreporite in Paleozoic lysophiurine ophiuroids appears to have had consistent placement in relation to Lovén's Law (Hotchkiss, Reference Hotchkiss1995, p. 434). In 12 of 12 five-rayed specimens that score perfectly for Lovén's Law, the madreporite occupies Lovénian interradius III-IV (below shown to be homologous with Carpenter's interradius BC). The probability of observing the madreporite in the same interradius (not specifically the III-IV interradius, but any interradius) by chance in all twelve specimens is (0.2)¹¹ = 0.00000002.

The universal application of Lovén's Law could still be falsified if we could detect a ‘Lovén-like’ pattern that involved three lefts and two rights, which is commonly the case with edrioasteroid ambulacral cover plates (see below). This raises another important point. In attempting to find a Lovén-like pattern in other classes of echinoderms, we must be sure we are comparing homologous plates. Lovén described his pattern in the first pair of basicoronal plates of sea urchins. The mouth angle plates (MAPP) of asteroids and ophiuroids are directly opposite each other, symmetric, and first in the series of ambulacral plates. There is no possibility that symmetric MAPP could exhibit a Lovén-like pattern, but subsequent pairs of ambulacral plates in some Paleozoic ophiuroids do alternate across the ambulacral midline and are scorable. Although the sense of offset of alternate ambulacral plates does not change along the ambulacrum, we must track back to the MAPP to score the L or R offset. Comparing the first and second plates in one class with the second and third plates in another class will inevitably lead to false conclusions.

Finally, an unspoken assumption in virtually all papers dealing with Lovén's Law is that once laid down the plates maintain their relative positions, although Mooi and David (Reference Mooi, David, Waters and Maples1997, fig. 1) make this explicit. So, if the first basicoronal plate is on the left (or behind, i.e., adoral to the right plate), during later growth it cannot shift its position and become in advance of the right plate. This means that we can number ambulacral plates or blastozoan brachioles along the ambulacra in the order they occur in adults and be sure the numbers refer to homologous plates or brachioles as well as reflecting the order in which they developed during ontogeny.

Origin of Lovén's Law and the 2-1-2 ambulacral pattern

Sprinkle (Reference Sprinkle1973) drew attention to the fact that in many blastozoans (and other echinoderms) the ambulacra are arranged in a 2-1-2 pattern (Fig. 4). This pattern can be interpreted in terms of homologies of ambulacra because the unbranched ambulacrum is always central (Carpenter's A), and the branched ambulacra are always lateral. In addition, the gonopore and hydropore are always in the CD interambulacrum and the anus very commonly so as well. This has led some echinoderm workers (e.g., Bather, Reference Bather and Lankester1900, fig. 9, p. 11; Fell, Reference Fell1966, p. 239; Fell and Pawson, Reference Fell, Pawson and Boolootian1966, p. 9; Sprinkle, Reference Sprinkle1973, p. 43; Paul and Smith, Reference Paul and Smith1984, p. 470; Sumrall, Reference Sumrall2005, Reference Sumrall, Ausich and Webster2008, fig. 11.2, p. 233; Sumrall and Wray, Reference Sumrall and Wray2007, fig. 1, p. 150) to argue that three primary ambulacra leave the mouth: the A, BC combined, and DE combined. Later in ontogeny, the B and C plus the D and E ambulacra bifurcate.

Figure 4. 2-1-2 ambulacral pattern and interpretation of the first 10 ambulacral plates in terms of Lovén's Law in Walcottidiscus. Primary ambulacral plates are assigned the postscript 1 or 2, depending on the inferred order in which they developed, on the assumption that the plate nearest the center of the mouth (M) was developed first. A, BC, and DE are plates of the three primary ambulacra in an assumed triradiate growth stage. Note that when the paired ambulacra bifurcate, there is no alternative position for the new ambulacral plates (B2 and C2 or D2 and E2) other than in the acute angle between the dividing paired ambulacra. This inevitably produces a B left, C right, D left, E right pattern for the first ambulacral plates in ambulacra B–E, irrespective of the position of the original first plate in the paired ambulacra (i.e., BC1 and DE1). The only possible variation is in ambulacrum A, where the first plate might have been on the left or right. In Walcottidiscus, it is on the right, giving the basic Lovén's Law pattern of AR, BL, CR, DL, ER, with E and A the unique pair of identical adjacent ambulacra. (Reversed, cropped, and relabeled from Paul and Smith, Reference Paul and Smith1984, fig. 7A, p. 454; based on USNM 376690).

Smith's diagram of the oral plating in the Cambrian edrioasteroid Walcottidiscus (= Stromatocystites in Paul and Smith, Reference Paul and Smith1984, fig. 7, p. 454; reversed as Figure 4 herein to show symmetry as seen externally) enables us to suggest how Lovén's Law might have come into being from a triradiate precursor (see Smith and Zamora, Reference Smith and Zamora2013, fig. 4). Imagining the 1-1-1 arrangement of the three primary ambulacra radiating from the mouth, we can identify the relevant primary ambulacral plates carried into Walcottidiscus and determine which formed first. In ambulacrum A, the first plate (A1, Fig. 4) is on the right. In the combined BC ambulacrum, the first plate (BC1) is on the left, as it is in the combined DE ambulacrum (DE1). When the combined ambulacra bifurcated, it was inevitable that the new ambulacral plates would develop in the acute angles between the separating ambulacral branches. Thus, irrespective of the relative positions of the first two plates in the combined BC ambulacrum, ambulacrum B would have its first plate on the left and ambulacrum C on the right (compare the positions of BC1 and B2, plus BC2 and C2 in Fig. 4). The same argument applies to the bifurcation of ambulacra D and E. Thus, Walcottidiscus comes out with a Lovén-like pattern (our Fig. 4 herein), which is, starting at Carpenter's ambulacrum A:

The pattern is cyclic RLRLR. There are three rights and two lefts, and the unique identical adjacent ambulacra are E and A. This gives a plausible hypothesis of how Lovén's Law might have originated as an inevitable result of the combination of biserial ambulacral columns with alternating plates, plus the division of the 1-1-1 pattern of primary ambulacra into five separate ambulacra (D, E separate)-1-(B, C separate) with inevitably reversed motifs. Furthermore, if the bifurcation of the paired ambulacra inevitably results in a pattern of BL, CR, DL, ER, the only possible variation would be the L/R scores of ambulacrum A. In Walcottidiscus, the first plate in ambulacrum A is Right; in many edrioasteroids the first primary ambulacral cover plate is Left. Thus, both possible Lovén-like patterns that could be derived from the transition from a 1-1-1 to a 2-1-2 pattern are known.

Origin of Lovén's Law and the ‘BD different pattern’ of glyptocystitoid blastozoans

Paul (Reference Paul1972) recognized that glyptocystitoid rhombiferans (glyptoids for brevity) with five ambulacra always had an unusual arrangement of first brachiole facets. In ambulacra B and D, the first two brachioles were on the left side (as viewed from the mouth in the direction of growth) and thereafter brachiole facets alternated. In ambulacra A, C, and E, only the first facet was on the left and thereafter they alternated regularly. Later (Paul and Donovan, Reference Paul and Donovan2011, p. 436; Paul, Reference Paul2015a, p. 189), this pattern was christened the ‘BD different pattern’ (Fig. 5). It appears to be plesiomorphic for glyptoids and may have appeared as early as Macrocystella Callaway, Reference Callaway1877 in the Tremadoc (Paul, Reference Paul1968).

Figure 5. Coronocystis angulatus (Wood, Reference Wood1909) USNM 113309. (1) Stereophotos of the oral area to show the ‘BD different’ pattern of primary brachioles. Ambulacra B (mid right) and D (lower left) have the first two brachiole facets to the left and then alternate regularly. The other ambulacra have the first facet left and then alternate regularly. (2) Oblique view of ambulacrum D to show first two facets on left (top right of photograph). D = ambulacrum D; m = position of mouth; arrows indicate first seven brachiole facets in ambulacrum D. Note that because the ambulacrum grew down the photograph, anatomical left of the ambulacrum is on the right in (2). Scale bars = 2 mm.

Sumrall (Reference Sumrall2005, Reference Sumrall, Ausich and Webster2008, Reference Sumrall, Harris, Böttger, Walker and Lesser2010; Sumrall and Wray, Reference Sumrall and Wray2007; Sumrall and Waters, Reference Sumrall and Waters2012) first suggested that Lovén's Law could be recognized in the blastozoan Lepadocystis Carpenter, Reference Carpenter1891 (Fig. 6.1, herein). Sumrall (Reference Sumrall2005, Reference Sumrall, Ausich and Webster2008) used a very loose definition of Lovén's Law, namely that the two ambulacra that differed from the three in Lovén's original pattern were ambulacra B and D of Carpenter. Since Sumrall noted the unusual ambulacral pattern found in all pentaradiate glyptoids described above, he concluded this was evidence for Lovén's Law in blastozoans. Sumrall (Reference Sumrall, Ausich and Webster2008) explained the ‘BD different pattern’ as arising because the first left facet in the B and D ambulacra represented the first facet of the combined B + C and D + E ambulacra, whereas the second left facet represented the first facet of the separate B and D ambulacra. Paul (Reference Paul2015b, p. 626–627) criticized this interpretation on two grounds. First, that the two different ambulacra under Lovén's Law were the A and D ambulacra of Carpenter. This criticism arose from the assumption that the hydropore was a reliable landmark for interpreting ambulacral homologies (see Paul and Smith, Reference Paul and Smith1984, fig. 16, p. 471), and is abandoned here. Secondly, the topology of the branches is wrong. Under the assumption that the radial water vessels branched terminally, the first brachiole in ambulacra B and D should branch before the bifurcation of the B and C, or D and E ambulacra. Indeed, Sumrall (Reference Sumrall, Ausich and Webster2008, fig. 11.2 3) shows this order of branching, but by the next ontogenetic stage (fig. 11.2 4) the branches to the first brachioles and the division of the ambulacra are at the same place. In practice, the ambulacra divide before (i.e., closer to the mouth) both lateral branches to left brachiole facets in ambulacra B and D. This appeared to be an insuperable difficulty, both with Sumrall's primary brachioles explanation and Paul's first idea that the entire ambulacrum C was homologous with the ‘missing’ brachiole B² and ambulacrum E homologous with the missing brachiole D² (see Fig. 6.1).

Figure 6. (1) The ‘BD different pattern’ of primary brachioles in Lepadocystis moorei (Meek) (UC 57349). A–E = Carpenter ambulacra; A¹, A², etc. = primary brachioles of ambulacrum A; G = gonopore; H = hydropore; L = “first left ambulacral floor plates” of Sumrall and Waters (Reference Sumrall and Waters2012); PO1–PO7 = perioral plates; 1–6 = primary ambulacral cover plates. Note that in ambulacra B and D, the first two brachioles, B¹, B³ and D¹, D³, arise on the left (modified from Paul, Reference Paul2017, fig. 3, p. 585). (2) Cartoon of Lovén's law as developed in the second brachioles (black circles) of L. moorei, which show the pattern AR, BL, CR, DL, ER, where A–E are Carpenter's ambulacra and L = left, R = right, denoting the side of the main ambulacral groove on which the second brachiole lies. F = facet; m mouth; 1–7 perioral plates 1–7. Dashed line separates the orals and first brachioles of the summit from the second brachioles located below the summit. The first brachioles all diverge to the left, whereas the second brachioles diverge in keeping with Lovén's Law.

In fact, blastozoan ambulacra branch subterminally, leading to erect brachioles (Fig. 7). It is inevitable that the next lateral branch of the radial water vessel (RWV) to a new brachiole must separate from the main RWV proximal to (i.e., adoral to) the last brachiole facet (arrow, Fig. 7). This is very similar to what happens in echinoids, for example, where the tip of the radial water vessel emerges from the ocular pore. Lateral branches to new tube-feet occur adoral to the ocular plate (i.e., not strictly terminal, but subterminal; Mooi et al., Reference Mooi, David and Wray2005, fig. 2, p. 545). The principal difference is that each terminal blastozoan brachiole acted just once in a manner similar to the permanent behavior of the ocular plate of echinoids.

Figure 7. Camera lucida drawing of terminal ambulacrum of right branch of ambulacrum D in the holotype of Callocystites fresti Paul (SM A85652) to show point of subterminal branching (arrow). Because the last two flooring plates bear a brachiole facet, we assume a brachiole was originally present. The termination of the radial water vessel would be at the tip of that brachiole. Thus, branching in this and all other callocystitids was subterminal.

Sumrall and Sprinkle (Reference Sumrall, Sprinkle, Carnevalli and Bonasoro1999) described the early ontogeny of Lepadocystis moorei (Meek, Reference Meek1871). The smallest example they found had only three ambulacra, which they interpreted as the A, BC combined, and DE combined. In a tri-radiate Lepadocystis, the first growth stage of the ambulacra would be just three primary brachioles (A¹, BC¹, and DE¹, Fig. 8.1). Applying the idea that branching of the ambulacra was subterminal, if the next stage was the separation of the B from the C ambulacrum and the D from the E ambulacrum, then the points of separation are shown by the arrows in Figure 8.1. Figure 8.2 then shows the stage with five ambulacra, each with a single brachiole facet, and the black arrows indicate the branching points for the next stage when each ambulacrum had two brachiole facets (Fig. 8.3). Note that this has resulted in the observed pattern where the main ambulacra B and C separate before (i.e., adoral to) both the left facets in the B ambulacrum. The same pattern occurs with the D and E ambulacra. Thus, Sumrall (Reference Sumrall2005, Reference Sumrall, Ausich and Webster2008) was correct in his interpretation of a three-ambulacrum stage with the first primary brachioles representing A¹, BC¹, and DE¹. Furthermore, it becomes clear that the brachioles labeled C¹ and E¹ (Fig. 8.2, 8.3) are homologous with the ‘missing’ brachioles B² and D². Thus, the entire ambulacra C and E are indeed homologous with the brachioles B² and D². The fact that ambulacral branching in blastozoans must have been subterminal actually predicts the pattern we observe in the ‘BD different pattern’ of pentaradiate glyptoids. This interpretation assumes three stages between the triradiate first stage and the appearance of the ‘BD different pattern.’ An alternative possibility, kindly pointed out by Elise Nardin (personal communication to CRCP, 2019) is that when the paired ambulacra were bifurcating to form the first brachiole in ambulacra C and E, ambulacrum A also added a second brachiole on the right. We think this is less likely because branching of the paired ambulacra was primarily to achieve a total of five ambulacra. Reaching a stage with three facets in ambulacrum A by the time ambulacra B and D had reached facet 3 does not affect this argument about how the ‘BD different pattern’ arose.

Figure 8. Development of the ‘BD different pattern’ of primary brachioles in Lepadocystis moorei (Meek). (1) Three-ambulacra stage with a single brachiole (A¹, BC¹, and DE¹) in each ambulacrum. Arrows point to the positions where the branching to form separate ambulacra C and E must have taken place. (2) Five-ambulacra stage with a single brachiole in each ambulacrum. Arrows indicate the branching points necessary to produce a second brachiole in each ambulacrum. (3) Stage with two brachioles in each ambulacrum. Note that this has produced the ‘BD different pattern’ with the first two facets on the left in ambulacra B and D. Note also, the pattern of the second brachioles in each ambulacrum, which is A right, B left, C right, D left, E right, with A and E the unique pair of identical adjacent ambulacra (i.e., Lovén's Law). A–E = Carpenter's ambulacra; F = brachiole facet; M = mouth; O1–O7 = oral (perioral) plates. Solid lines = plate sutures, dashed lines = outline of peristome and facets.

Terminal ambulacral branching occurs in crinoids, where every lateral branch, whether of the main arm trunk or just to form a pinnule, involves an axillary plate. Indeed, we think that this difference in the mode of growth of the ambulacra in blastozoans and crinoids is possibly the most fundament difference between the two major taxa and considerably more important than the fact that blastozoan ambulacral structures are typically biserial, whereas crinoids have uniserial structures. Exceptions to both generalizations occur.

As far as Lovén's Law is concerned, we explicitly recognize Lovén's Law in the second brachioles of Lepadocystis moorei (Meek, Reference Meek1871), and explicitly the pattern LLLLL in the first brachioles. The second brachiole facets (Figs. 6.2, 8.3) show a perfect pattern of AR, BL, CR, DL, ER (i.e., three rights and two lefts), with E and A the unique pair of identical adjacent ambulacra as predicted above in considering the 2-1-2 ambulacral pattern and shown to be an inevitable consequence of the way the BC paired and DE paired ambulacra bifurcate.

A final point concerns the difficulty that this Lovén's Law pattern occurs in the first pairs of plates of the ambulacra in Walcottidiscus, but in the second set of brachioles in Lepadocystis and other pentaradiate glyptoids. Equally, Lovén's Law was first recognized in the first pair of basicoronal plates of echinoids, but also occurs in the second pair of ambulacral plates in ophiuroids; the first pair being the mouth angle plates, which are opposite and symmetric. So, are we comparing like with like in recognizing these Lovén-like patterns?

We would suggest that the answer is ‘yes’, because wherever along an ambulacrum Lovén's Law first manifests itself, the pattern will continue thereafter. It is simply necessary to trace the pattern back towards the mouth to see where it first appeared in order to make sure we are comparing like with like. So, if mouth angle plates do not show Lovén's Law, but the second pair of ambulacral plates does, we are comparing equivalent plates in all ambulacra. There is a potentially more serious difficulty with glyptoid ambulacra. The ambulacra of Walcottidiscus are biserial, so we are comparing the relative positions of pairs of plates. In glyptoids, the pattern is detected in the second branch of each ambulacrum leading to a brachiole.

Nevertheless, the first brachiole facet is supported by two plates, an oral and an L plate (Fig. 6.1). In ambulacrum A, for example, the plates are PO3 and an L plate. These two plates are on either side of the ambulacrum, and thus constitute the first pair of ambulacral plates. The same is true in all five ambulacra. So, we conclude that the second facets in Lepadocystis and other pentaradiate glyptoids involve the second pair of ambulacral flooring plates and are, therefore, homologous with the plates displaying Lovén's Law in Walcottidiscus and ophiuroids. Thus, we think the basic Lovénian pattern was established in the first pairs of ambulacral plates in Walcottidiscus. Subsequently, in lineages leading to ophiuroids, the first pair of ambulacral plates became modified as equal and opposite mouth angle plates before the first offset plates, which reflect Lovén's Law. In echinoids, the equivalents of the first pair of plates in Walcottidiscus appear to have been lost. In glyptoids, the first pair of plates supporting the first brachiole became modified to obscure the basic Lovénian pattern.

To summarize. The way in which five biserial alternating ambulacra arose from the primary 1-1-1 pattern inevitably results in a Lovénian pattern in the first pairs of ambulacral plates, that is AR, BL, CR, DL. ER, with EA being the unique pair of identical adjacent ambulacra. This pattern can also be derived from the ‘BD different pattern’ of primary brachiole facets in glyptocystitoid rhombiferans. Thus, a Lovénian pattern can be derived from the mode of development of the ambulacra of pentaradiate echinoderms with a 2-1-2 ambulacral pattern derived from a primary 1-1-1 pattern. This is present in the Cambrian Walcottidiscus and in glyptoids from the Tremadoc to at least the Wenlock. It now remains to see how this relates to Lovén's original observation in post-Paleozoic echinoids. Parsimony suggests that if we have two equally consistent patterns in Paleozoic echinoderms with a 2-1-2 ambulacral pattern and in post-Paleozoic echinoids, it is simpler to assume that they are the same. This assumption can potentially be falsified by the discovery of an alternative Lovén-like pattern, either with a different pair of identical adjacent ambulacra, or with three Left and two Right. The former requires a reliable independent landmark, which the closure of the ring canal might provide for living echinoderm classes. The latter is independent of any landmark.

Additional Paleozoic echinoderms that illustrate Lovén's Law

Edrioasteroidea

Edrioasteroids are Paleozoic eleutherozoan echinoderms typically with pentaradiate ambulacra in a 2-1-2 pattern. Bell (Reference Bell1976) subdivided them into two major groups, the Isorophida, which have uniserial ambulacral flooring plates, and the Edrioasterida, which have biserial alternating ambulacral flooring plates. Bell (Reference Bell1976, fig. 2, p. 25) showed that edrioasterid flooring plates are exposed on either side of the ambulacra and align perfectly with the ambulacral cover plates. Edrioasterids also have ambulacral pits, usually interpreted as positions of tube feet, which bear a 1:1 relationship to the flooring and cover plates. In Edriophus levis (Bather, Reference Bather1914), two lines of evidence (flooring plates and cover plates) produce a Lovén like pattern of AR, BL, CR, DL, ER; three R, two L, and EA the unique identical adjacent radii. This is identical to the pattern of first basicoronal plates seen in echinoids.

Isorophid edrioasteroids have biserial ambulacral cover plates, accompanied by pores for presumed tube feet in the suborder Lebetodiscina. Cover plates may be added in up to seven generations, making identification of first ambulacral cover plates difficult. Nevertheless, Lovén-like patterns can be coded in nearly 30 species on cover plates, pores, or both (Table 1). In isorophids, virtually without exception, the inevitable BL, CR, DL, ER pattern of mirror image motifs is present. The hydropore sometimes makes the coding of ambulacrum C particularly difficult. Both possibilities for ambulacrum A occur and AL more frequently than AR (26L, 14R, 5 uncertain; Table 1). In three species, Hemicystites parasiticus Hall, Reference Hall1852, Krama devonicum (Bassler, Reference Bassler1936), and Hadrochthus commensalis Bell, Reference Bell1976, different examples have ambulacrum A code in opposite ways. In Foerstediscus grandis Bassler, Reference Bassler1935, pores code right in ambulacrum A, but cover plates code left. Finally, in two different species of Isorophus, ambulacrum A codes in opposite ways. Even if one ignores the cover plates, the pores of edrioasteroids code left more frequently than right in ambulacrum A (Table 1). It is difficult not to conclude that the motif in ambulacrum A was not fixed in edrioasteroids. In addition, some authorities (e.g., Mooi et al., Reference Mooi, David and Wray2005) argue that cover plates are not rigidly subject to the ocular plates rule of terminal addition and so should not be used in attempting to recognize Lovén's Law.

Table 1. Occurrence of Lovén-like ambulacral patterns in Edrioasteroidea described by Bell, Reference Bell1976. Under evidence, Floor = flooring plates and Cover = cover plates. ‘None’ listed under pores for Isorophus austini (Foerste) indicates that no edrioasteroids listed below this level possess ambulacral pores.

Diploporita

Estonocystis Jaekel, Reference Jaekel1918 (Fig. 9) is a diploporite that shows another type of BD different pattern of primary brachioles to that seen in glyptocystitoid Rhombifera. It differs from Lepadocystis in having only one oral in each ambulacrum, which does not contribute to a brachiole facet, and no L plate. Thereafter, brachiole facets arise from single plates, not pairs of flooring plates as in glyptoids. It is unique among diploporites with a regular ambulacral structure in having up to three facets per ambulacral plate on either side of the ambulacra. All other such diploporites have one facet per ambulacral flooring plate. Its ‘BD different pattern’ arises because the first ambulacral plate in ambulacra B and D has one more facet than the first ambulacral plate in ambulacra A, C, and E, typically three in B and D, but only two in A, C, and E (Fig. 9.3).

Figure 9. Estonocystis Jaekel, Reference Jaekel1918. (1) Photo of TUG 1727-1, (2) photo plus plate outlines, (3) plate and ambulacral outlines with third brachiole facet in each ambulacrum shaded gray and labeled left (L) or right (R). Note third facets code A right, B left, C right, D left, E right, as in Lovén's Law. A–E = Carpenter's ambulacra; F = ambulacral facets BC¹ and DE¹; G = gonopore; H = hydropore; M = mouth; 1–6 = perioral plates. Solid lines = plate sutures, broken lines = outline of ambulacra and peristome. Scale bar = 5 mm. Photo from Geoscience Collections of Estonia.

Mature specimens do not show a Lovén-like pattern of ambulacral facets because the first two or three facets are on the first ambulacral plates, which lie on the left in all five ambulacra. The second pairs of facets are on the second ambulacral plates, which lie to the right in all ambulacra. Nevertheless, the simplest explanation of the extra facet in the first plate of ambulacra B and D is that they represent the BC¹ combined and DE¹ combined facets. If this is so, early in the development of the ambulacra when there were only ten facets, it is conceivable that both first facets in ambulacra B and D lay on the left within the first ambulacral plates, whereas in ambulacra A, C, and E, the first facet was on the left and the second on the right within the second ambulacral plate. This would have temporarily given a Lovén-like pattern of AR, BL, CR, DL, ER. Even so, the third brachiole facets in each ambulacrum of the specimen illustrated in Figure 9.3 code as AR, BL, CR, DL, ER: EA the unique pair of identical adjacent ambulacra.

The only other example from diploporite blastozoans is more convincing, but almost equally distinctive. Sphaeronitid diploporites entirely lack a regular ambulacral structure. The food grooves lack flooring and cover plates, but may extend over the theca and branch repeatedly. Sphaeronitids are united, among other things, by these food grooves plus a mouth frame composed of five radially positioned ‘oral’ plates, with a sixth in the CD inter-radius. The mouth is covered by six immovable, primary cover plates. Food entered the corners of the peristome through small ambulacral orifices, one per ambulacrum, and all branching of the food grooves occurs outside the limits of the peristome. Batalleria Chauvel and Meléndez, Reference Chauvel and Meléndez1978 (Fig. 10) is related to sphaeronitids in having a similar mouth frame, but unique in having ambulacral branching within the peristome. The pattern of sutures between the oral cover plates shows the classic 2-1-2 branching (Fig. 10). In addition, the food grooves branch with the first lateral branch on the right in ambulacrum A, left in ambulacrum B, etc. in a classic Lovénian pattern (Fig. 10). Each food groove then leaves the mouth at a separate ambulacral orifice opposite a brachiole (?) facet, so that although no ambulacral plates are involved, clearly the soft-tissue structures, such as the radial water vessels, were branched.

Figure 10. Camera lucida drawing from a latex cast of Batalleria? sp. to show 2-1-2 pattern of ambulacra (A–E) with first lateral branches to ambulacral facets (F) that fit Lovén's Law; A right, B left, C right, D left, E right; H = hydropore.

Interpretation

To restate Lovén's Law in terms of the positions of first basicoronal ambulacral plates, using Lovén's ambulacral designations and Left and Right notation gives the following pattern:

The transition from a triradiate 1-1-1 ambulacral pattern to a pentaradiate 2-1-2 pattern using Carpenter's ambulacral designations gives:

Parsimony then suggests that Lovén's interradius I-II is homologous with Carpenter's EA, so we can derive the following ambulacral homologies:

This is our fundamental hypothesis. Unfortunately, to be able to falsify this hypothesis requires a reliable independent landmark that can be recognized in all the classes of echinoderms that display Lovén-like ambulacral patterns. Currently, no such universal landmark can be recognized (see Testing homologies section above). Nevertheless, parsimony implies other important hypotheses. For example, our assumption of the homologies of Lovén's and Carpenter's radii is the simplest assumption only if Lovén's Law arose just once in the evolutionary history of the echinoderms. Secondly, if Lovén's Law is a consequence of the development of five ambulacra (as we argue above), it must have arisen early in the history of the echinoderms, and it should be widespread within the phylum. Finally, a plausible mechanism to explain how Lovén's Law arose is required to account for its fundamental nature. These are testable hypotheses and by making the first assumption we can investigate them.

A final point concerns the mechanism by which Lovén's Law can be recognized, especially in fossils. This includes the assumption that the order of ambulacral plates or lateral branches does not change during ontogeny. As originally stated, (Lovén, Reference Lovén1874) Lovén's Law was recognized using basicoronal ambulacral plates, which bear pores for the tube-feet/ampullae. Thus, both ambulacral plates and lateral branches of the radial water vessel (RWV) were involved. In other groups, we have used ambulacral flooring and cover plates (skeletal elements) as well as brachioles and ambulacral pores (lateral branches of the RWV). Strictly speaking, we need to know the homologies between echinoid ambulacral plates and fossil ambulacral plates. Here we argue that ambulacral flooring plates of blastozoan fossil echinoderms are homologous with echinoid ambulacral plates. Use of cover plates, in turn, requires knowledge of the relationship between cover plates and flooring plates. Ideally the two plate types should be in a 1:1 ratio or at least a known ratio and a fixed relationship, in order for cover plates to reveal Lovén's Law.