Tissue & Cell 36 (2004) 263–273 Ultrastructure of Early Jurassic fossil plant cuticles: Pachypteris gradinarui Popa G. Guignard a,∗ , M.E. Popa b,1 , G. Barale a,2 a Paléobotanique, Université Claude-Bernard Lyon 1 and UMR 5125 CNRS, Bâtiment Darwin A, 7 Rue Dubois, 69622 Villeurbanne Cedex, France b Laboratory of Palaeontology, Faculty of Geology and Geophysics, University of Bucharest, 1, N. Balcescu Ave., 70111 Bucharest, Romania Received 19 December 2003; received in revised form 13 March 2004; accepted 1 April 2004 Abstract Exceptional preservation of extinct Pachypteris extra-epidermal cuticle enabled the first detailed statistical measurements of its ultrastructure using transmission electron microscopy. Pachypteris is a leaf genus of the Mesozoic belonging to seed fern foliage of the order Corystospermales. The species studied in this paper is Pachypteris gradinarui Popa [Rev. Palaeobot. Palynol. 111 (2000) 31], based on fossils which are Early Jurassic in age (Hettangian-Sinemurian, approximately 205–190 million years old). Both the upper and the lower cuticles were thoroughly examined, including the detail of the stomatal complexes and epidermal cells. The data obtained from our TEM analysis, together with the confidence intervals, were very useful to give precise description of the cuticles as they distinguished between upper and lower epidermal and stomatal cell types. Moreover a combination of characters was used to develop the first dichotomous key based on ultrastructural characters, i.e. not only the total thickness of the cuticle but also details and proportions of A cuticle proper and B cuticular layer. Comparisons with ultrastructures known from other Pachypteris species show that the influence of space and time, diagenetic processes, and/or processes related to technical procedures, seem to be minimal within this genus. Detailed studies of this type may be very useful for further comparisons among other species and at higher taxonomical ranks. © 2004 Elsevier Ltd. All rights reserved. Keywords: Ultrastructure; Fossil leaf cuticles; Pachypteris gradinarui; Pteridospermopsida; Early Jurassic; South Carpathians 1. Introduction Cuticle is a very thin film covering the epidermis of the aerial parts of many tracheophytes. It is a very precise and even perfect external moulding of epidermal cells, and as it is often the only organic remains of fossil plants in various types of sediments their detailed study is very useful in Palaeobotany. Cuticles have been studied for decades (Harris, 1956; Archangelsky, 1991) and high variation has long been observed with light (LM) and scanning electron (SEM) microscopes. Ultrastructural studies using a transmission electron microscope (TEM) are still not in common practice, although they have been used for extant plant cuticles for approximately 40 years (Holloway, 1982). Thanks ∗ Corresponding author. Tel.: +33-4-7244-8203; fax: +33-04-7244-8203. E-mail addresses: guignard@univ-lyon1.fr (G. Guignard), mihai@mepopa.com (M.E. Popa), barale@univ-lyon1.fr (G. Barale). 1 Tel.: +40-72-273-4070; fax: +40-21-211-3120. 2 Tel.: +33-4-7244-8203; fax: +33-4-7244-8203. 0040-8166/$ – see front matter © 2004 Elsevier Ltd. All rights reserved. doi:10.1016/j.tice.2004.04.002 to very fine details observed within ultrathin sections of cuticles using TEM and found as very useful compared with LM or SEM approaches, the ultrastructural studies on fossil cuticles began in 1986 with the works of Archangelsky and Taylor, and Archangelsky et al. The Mesozoic seed fern group Corystospermales, belonging to class Pteridospermopsida (Taylor and Taylor, 1993; Stewart and Rothwell, 1993), represents a very interesting plant group when analysing the mixture of both primitive (e.g. compound leaves similar to fern fronds) and evolved characters (e.g. complex reproductive structures such as Umkomasia), along with the palaeogeographic significance (Vakhrameev, 1991) and the phytogeographic importance of many of their representatives. Among seed fern ultrastructural studies that have been reported (Archangelsky et al., 1986; Taylor et al., 1989; Maheshwari and Bajpai, 1996a,b; Bajpai, 1997), some studies have focused on the Corystospermales genus Pachypteris (Labe and Barale, 1996; Baldoni and Barale, 1996; Bajpai and Maheshwari, 2000). However, their results were mostly qualitative, i.e. description of the structures, and dealt only with epidermal 264 G. Guignard et al. / Tissue & Cell 36 (2004) 263–273 cell outlines not including stomatal apparatus, using lower magnifications with mainly short descriptions and measurements, and represent the current state of our knowledge of cuticular ultrastructure in Pachypteris. The genus Pachypteris Brongniart emend. Harris (Brongniart, 1828; Harris, 1964) is a common form genus of pteridosperm (seed fern) foliage for Triassic-Jurassic deposits of the Northern Hemisphere. Lower Jurassic (Hettangian-Sinemurian, approximately 205–190 million years old) continental deposits of the South Carpathians, central Romania, yield a rich and well preserved compression flora, including an abundant pteridosperm assemblage of which Pachypteris is represented by several species. Pachypteris gradinarui Popa (Popa, 2000), a new established taxon was collected from Cristian, an important fossil plant locality in Romania due to its excellently preserved fossil plants. Using results from these prior LM and SEM studies (Popa, 2000), and taking advantage of the high preservation quality allowing detailed observations of not only cuticle located above ordinary epidermal cells, but also above guard and subsidiary cells of the stomatal apparatus, we examined Pachypteris cuticle at the ultrastructural level using TEM for this study. 2. Material and methods The leaf fragments (Fig. 1) occur on sandstone hand specimens collected from Cristian (Brasov County, South Carpathians, Romania) (Popa, 2000). The sandstone is a fine, lithic sandstone, Lower Jurassic, Hettangian-Sinemurian in age. The leaf compressions preserve the frond rachis and pinnules with their diagenetically altered mesophyll, cell wall residues, and very well preserved cuticle including the details of epidermal cells and stomatal complexes. The cuticles were obtained by treating leaf compressions with Schultze’s Reagent (HNO3 + KClO3 ). KClO3 crystals and concentrated HNO3 acid were added to glass tubes containing the pinnule fragments until the upper and lower cuticle separated. After 4 weeks in paraformaldehyde solution, cuticles were prepared for the TEM study. This method is described in the papers of Lugardon (1971) and Guignard et al. (2001), including embedding and staining the material. Cuticles were pre-stained with osmium-tetroxide, embedded in blocks of Epon resin, cut with a diamond knife (Reichert Ultracut S) and finally stained with uranyl acetate and lead citrate. Two resin blocks, one containing the lower cuticle Figs. 1–31. Different views of the cuticle of Pachypteris gradinarui. Except Figs. 1 (camera microphotograph) and 18–20 (light microscope microphotographs), all other figures are transmission electron microscope microphotographs. OP: outer part of the cuticle; IP: inner part of the cuticle; EC: location of an ordinary epidermal cell; AW: anticlinal wall between two cells cuticle; CW: cell wall residues; SP: stomatal pit of the stomatal apparatus; SC: subsidiary cell location; GC: guard cell location. Some lettering indicate the different parts of the cuticles: cuticle proper A (= A1 (upper A1U + lower A1L for upper ordinary epidermal cell cuticle only) + A2) + cuticular layer B. B layer is making a reticulum with very various schemes observed in each type of cell; thus, in order to give the most complete view of all schemes observed, different examples are given for each type of cell. For the same reasons, the cuticles of all types of cells consisting of layers similar in ultrastructure, in order to give a better overview of each layer detailed figures at different magnifications (up to 125,000×) are provided. Fig. 1. General view of a leaf, No. G44. Figs. 2–10. Ordinary epidermal cell upper cuticle. Fig. 2. General view. The outer part is delimited with a hardly visible layer (arrows) at this low magnification (compare with Fig. 11). Numbers correspond to figures detailing parts of the cuticle in this page, parallel section, No. GGE978, 1800×. Fig. 3. Outermost part, made up with thin upper A1U and thicker lower A1L zones, parallel section, No. GGE981, 14,500×. Fig. 4. The above part of the anticlinal wall is made up with very contrasted B layer fibrils making a pillar-shape structure, parallel section, No. GGE973, 60,000×. Fig. 5. Outermost A1 layer, composed of sparsely lamellate A1U zone covering dispersed material, perpendicular section, No. GM0174, 35,000×. Fig. 6. A2 granular layer, perpendicular section, No. GM0169, 125,000×. Fig. 7. B fibrilous layer arranged in a reticulum, parallel section, No GGE970, 28,000×. Fig. 8. Cell wall residues with very parallel lines (see Figs. 17, 27, and 31 for comparison), parallel section, No. GGE965, 100,000×. Fig. 9. Fibrils of B layer are arranged as herring bones (arrows), parallel section, No. GGE974, 17,000×. Fig. 10. Fibrils of B layer are arranged in a reticulum with very condensed and very clear spaces, perpendicular section, No. GMD199, 45,000×. Figs. 11–17. Ordinary epidermal cell lower cuticle. Fig. 11. General view of the cuticle. In this case, the outermost part is clearly delimited (compare with Fig. 2). Numbers correspond to figures detailing parts of the cuticle in this page, parallel section, No. GGE983, 1400×. Fig. 12. Outer part of the cuticle, with the cuticle proper (A1 + A2) and the reticulum of the cuticular layer B, parallel section, No. GGE990, 28,000×. Fig. 13. Outermost continuous A1 polylamellate layer, covering the A2 granular layer, perpendicular section, No. GM0468, 60,000×. Fig. 14. Outermost part with an interrupted A1 polylamellate layer on the right side, parallel section, No. GGE993, 125,000×. Fig. 15. Reticulum of B layer leaving empty spaces different in size, parallel section, No. GGE994, 28,000×. Fig. 16. The fibrils of the B layer show a very condensed structure, perpendicular section, No. GM0331, 28,000×. Fig. 17. Parallel and numerous lines inside the cell wall running around the cell location (compare with Figs. 8, 27, and 31), perpendicular section, No. GM0339, 45,000×. Figs. 18–20. Stomatal apparati cells cuticle, general views. The sections show different aspects according to their location, one or two guard cells cuticles being visible depending on the orientation of the sections, the stomatal pit being more or less opened. Numbers correspond to the figures detailing this part of the cuticle, perpendicular sections, light microscope, No. P1-P2-P3, 1000×. Figs. 21–27. Subsidiary cell cuticle. Fig. 21. Outer part of the cuticle, showing the cuticle proper (A1 + A2) and the fibrils of the cuticular layer B, short and various in diameter. Numbers correspond to figures detailing parts of the cuticle in this page, perpendicular section, No. GM0450, 60,000×. Figs. 22 and 23. Outermost part with a faintly stained polylamellate A1 layer, covering the A2 granular layer, perpendicular sections, No. GM0470 and No. GM0471, 60,000×. Fig. 24. A2 granular layer, perpendicular section, No. GM0474, 35,000×. Fig. 25. Rather sparse fibrils are parallel and waving, perpendicular section, No. GM0453, 75,000×. Fig. 26. Detail of Fig. 25 showing the reticulum of fibrils at a higher magnification, perpendicular section, No. GM0454, 125,000×. Fig. 27. Innermost part along the cell location where the cell wall shows condensed lines (compare with Figs. 8, 17, and 31), perpendicular section, No. GM0450, 60,000×. Figs. 28–31. Guard cell cuticle. Fig. 28. Boundary between a guard and a subsidiary cell cuticle, with fibrils parallel just in the centre and making on both sides a reticulum orientated differently, perpendicular section, No. GM0456, 60,000×. Fig. 29. A1 polylamellate layer is not continuous in this outermost part, perpendicular section, No. GM0461, 125,000×. Fig. 30. B layer fibrils are running in all directions, perpendicular section, No. GM0458, 60,000×. Fig. 31. Innermost part around the cell location with cell wall residues made with parallel lines (compare with Figs. 8, 17, and 27), perpendicular section, No. GM0457, 60,000×. G. Guignard et al. / Tissue & Cell 36 (2004) 263–273 265 266 G. Guignard et al. / Tissue & Cell 36 (2004) 263–273 and the second the upper cuticle, were prepared and cut to 70 nm thick ultra-sections. All types of cell cuticles were cut transversal and parallel to the length of the cells. The ultra-sections were mounted on 300-Mesh uncoated grids and studied with TEM. The total number of studied grids, each containing one or several ultra-sections, depending on their size, was 65 (perpendicular to the leaf length: 10 for the upper cuticle and 35 for the lower cuticle; parallel to the leaf length: 20 in total, 10 for each upper and lower cuticles). The resin blocks and negatives (called GGE or GM in the figure captions for transmission electron microscopy, P for light microscopy, G for camera) are stored in the Guignard Collection in Lyon and in the Gradinaru collection in Bucharest. Cuticle preparations were illustrated using Corel Draw ver. 7 for vectorial drawings and Corel Photopaint ver. 7 for bitmap images. The TEM used is a Philips model CM120 at Centre technologique des microstructures (CT), Université Claude-Bernard, Lyon 1, in Villeurbanne, France. apparatus cuticle located above guard and subsidiary cells), and statistical values are provided (Tables 1 and 2). In most cases, the cell wall is made up of very concentrated parallel lines (Figs. 8, 17, 27, and 31), and were not included in the measurements and in the ultrastructure description. Upper cuticle: ordinary epidermal cell cuticle (Figs. 2–10; Tables 1 and 2). The cuticular membrane (CM) (13.7 m in mean thickness) consists of a thin cuticle proper (CP) (= A, 30.5% of the whole cuticle) and the cuticular layer (CL) (= B, 69.5%). The A1 layer, very rarely absent, is composed of a thin, faintly stained, sparsely lamellate upper zone A1U and a thicker mainly amorphous lower zone A1L , which more or less contains the same material as the A1U zone (Figs. 3 and 5). The A1U zone covers the A2 granular layer (Fig. 6). Below A2 is the B layer, which is made up of a reticulum of fibrils arranged in very diversed schemes (Figs. 7 and 9–10, see also the other detailed B layer figures among all other types of cells as only the whole set gives a complete idea of B layer in each type of cell: Figs. 15–16, 25–26, and 30). Among these schemes, fibrils have in different areas a “herring bone” appearance (termed used as in Holloway, 1982). Lower cuticle: ordinary epidermal cell (Figs. 11–17) and stomatal apparatus (Figs. 18–20) (subsidiary (Figs. 21–27) and guard cell (Figs. 28–31)) cuticles (see also Tables 1 and 2). 3. Results The terminology used is that of Archangelsky et al. (1986) and commonly used for fossil plants cuticles. Sections observed allowed 30 measurements for each type of cell (called ordinary epidermal cells and used for cuticle located above normal epidermal cells, to be distinguished with stomatal Table 1 Statistical values, made with 30 measurements for each type of cell cuticles Ordinary epidermal cells Upper cuticle CM CP (A) A1 A1U A1L A2 CL (B) OL (nm) TL (nm) Lower cuticle Mean Min.–max. Percent S.D. Var Mean Min.–max. Percent S.D. Var 13.68 4.17 1.64 0.10 1.54 2.53 9.51 7.71–23.63 2.25–6.19 0.63–3.31 0.05–0.25 0.50–3.16 1.50–4.40 3.90–19.50 100 30.48 11.99 0.73 11.26 18.49 69.52 5.03 1 0.67 0.045 0.65 0.58 4.57 25.28 0.99 0.45 0.002 0.42 0.34 20.92 12.26 0.20 0.05 6.97–23.27 0.09–0.47 0.02–0.08 100 1.63 0.41 4.89 0.09 0.02 23.91 0.08 0.003 0.15 12.06 5.80 7.59 0.06–0.40 6.80–23.00 3.90–8.40 3.90–16.70 1.22 98.37 0.08 4.83 1.92 3.52 0.07 23.29 0.004 0.01 Var Stomatal apparatus Subsidiary cell cuticle CM CP (A) A1 A2 CL (B) OL (nm) TL (nm) Guard cell cuticle Mean Min.–max. Percent S.D. 5.30 0.23 0.05 0.18 5.07 8.75 7.09 3.60–9.90 0.15–0.31 0.02–0.08 0.09–0.28 3.35–9.68 7.40–15.40 3.90–8.30 100 4.34 0.94 3.40 95.66 1.45 0.032 0.015 0.04 1.45 2.67 1.49 Var 2.10 0.001 0.0002 0.002 2.10 0.001 0.002 Mean Min.–max. Percent S.D. 3.99 0.28 0.08 0.20 3.71 11.80 7.45 0.99–8.25 0.19–1.07 0.04–0.14 0.12–0.98 0.72–8.02 3.90–23.0 3.90–7.70 100 7.02 2.01 5.01 92.98 2.31 0.15 0.03 0.15 2.35 6.66 0.96 5.35 0.023 0.001 0.023 5.50 0.04 0.001 Min.–max.: minimum and maximum values observed; percent: percentage of each detailed part of the cuticle; var: variance. The cuticular membrane CM is made up with cuticle proper CP (= A1 layer + A2 layer) and cuticular layer CL (= B layer). In the upper ordinary epidermal cell cuticle, the A1 layer is composed of an upper A1U and a lower A1L parts. All other A1 layer cuticles are composed of lamellae, opaque OL, and translucent TL. Except for very thin OL and TL measured in nm, all other measurements are in m. G. Guignard et al. / Tissue & Cell 36 (2004) 263–273 267 Table 2 √ Confidence interval (= x̄ ± (var/n) × 1.96, giving 95% ␣ risk) of the different types of cell cuticles, calculated among the different layers, zones and types of lamellae Continuous line shows affinities between different cells types, // shows weak affinities, disruption along a line shows disaffinities. The cuticles located just above the three types of cells are similar in ultrastructure (12.3, 5.3, and 4 m in mean thickness, respectively), and are composed of the CP (= A = polylamellate A1 + granular A2; 1.6, 7, and 4.3% of the whole cuticle, respectively) and the CL (= B; 98.4, 93, and 95.7% of the whole cuticle, respectively). The A1 layer (Figs. 13–14, 22–23 and 29), absent in some places (Figs. 14, 23 and 29), consists of about 5–8 opaque (5.8, 15.7, and 11.8 nm in mean thickness, respectively) and translucent (7.6, 7.1, and 7.5 nm of thickness in mean, respectively) thin lamellae. The A2 layer is granular and homogeneous (Figs. 12–13, 22–24, and 29). The B layer is composed of a reticulum of fibrils also arranged in very diversed schemes (Figs. 15–16, 25–26, and 30). 4. Discussion 4.1. General considerations, quantitative new data and their importance Following LM and SEM study of this taxon (Popa, 2000), TEM results support the exceptional quality of the fossil material, as many ultrastructural details could be observed. Despite the age of the compressions, the cell wall residues are usually in the lowermost part of the cuticle, and the quasi-omnipresent outermost A1 polylamellate layer of the cuticle is observed. Thickness measurements and other comparisons among the types of cuticles covering different types of cells were possible. Although fragility of the cuticles among several pteridosperm taxa has been already noted and discussed (Kerp and Barthel, 1993; Krings and Kerp, 1997), stomatal apparati were easily observed and measured in P. gradinarui. Stomatal complex detail is usually difficult to obtain with TEM and is often rarely observed in fossil plant cuticles. They are not provided in the papers of the other authors discussed below, certainly due to both rarity in the cuticles compared to ordinary epidermal cells and technical fragility of the sections on the copper grids. Transversal and parallel (to the length of cells) sections, permitting the same TEM details, showed the homogeneity of the layers, especially the homogeneous density and orientation of the B layer fibrils and of the polylamellae of A1 layer, enabling a three-dimensional reconstruction (Fig. 32). A combination of percentages and absolute values of the different layers (Fig. 33; Tables 1 and 2) were found to identify the four types of cells (upper and lower ordinary epidermal cell cuticles, subsidiary and guard cell cuticles belonging to stomatal apparatus). These detailed characters provide new criteria that can be used for identification. Considering only the percentages of thicknesses of each layer, the upper cuticle represented by one type (30.5% of A, 69.5% of B layer) is different from the lower one represented by three types (thinner A layer between 1.6 and 7%, thicker B layer between 93 and 98.4%). Details of the A layer (considered as 100%) enable the same kinds of distinction: the upper cuticle has a 39% A1 layer and a 61% A2 layer, while the three lower cuticles have a thinner A1 (between 21 and 28%) and a thicker A2 layer (between 72 and 79%). Popa (2000) noted that one of the reasons for taxonomic problems in pteridosperms is the great macromorphological variability. In P. gradinarui, the minimum and maximum values of absolute ultrastructural thicknesses are usually relatively large leading to a high variance (Table 1, called var) and standard deviation (Table 1, called S.D.). However, measuring the variability of each layer in each cuticle type is valuable and illustrates the necessity of a sufficient number of measurements. In addition, Popa (2000) also noted the “unclear setting of character assessments” for this taxon. 268 G. Guignard et al. / Tissue & Cell 36 (2004) 263–273 Fig. 32. Three-dimensional reconstruction of the cuticle. OEC: ordinary epidermal cell; SC: subsidiary cell cuticle; GC: guard cell cuticle; AW: anticlinal wall between two cells cuticle; CW: cell wall residues. √ With the confidence interval value (= x̄ ± (var/n) × 1.96, giving 95% ␣ risk) calculated with 30 measurements among seven characters, a combination of affinities and disaffinities distinguishes among the four types of cuticles (Fig. 33; Table 2) making a positive answer to Popa’s taxonomic remark, and these ultrastructural measurements could be applied to try to resolve taxonomic problems. Using only these discriminative values of the confidence interval, a dichotomous key using the seven ultrastructural measured characters is proposed enabling identification of each type of cell (Table 3). As eventual compression of the total cuticle can- not be neglected during these millions of years in the sediment but seems to be impossible to check with only extinct plants (Guignard and Zhou, in press; concerning a study on extinct and living gingkos), the percentages of thickness of the layers are also indicated for each type of cuticle. Ordinary epidermal cell cuticles (12.3–13.7 m in mean) have the same range of measurements, and they are separated from stomatal apparatus cuticles (4–5.3 m in mean) in total thickness and in the thickness of the B cuticular layer (9.5–12.1 m in mean versus 3.7–5.1 m in mean). The tendency for stomatal apparatus cuticle to be different in thick- Table 3 Dichotomous key enabling the identification of each of the four types of cuticles observed in P. gradinarui, using only the distinctions with the confidence √ interval (= x̄ ± (var/n) × 1.96, giving 95% ␣ risk) among seven ultrastructural characters noted with their mean values Thick total thickness 12.3–13.7 m, B cuticular layer 9.5–12.1 m Thin total thickness 4–5.30 m, B cuticular layer 3.7–5.1 m → → Ordinary epidermal cell cuticle Stomatal apparatus cell cuticle Absence of polylamellae in the A1 layer. Cuticle proper A 4.2 m, composed of A1 layer 1.7 m and A2 layer 2.5 m Presence of polylamellae in the A1 layer. Cuticle proper A 0.2 m, composed of A1 layer 0.05 m and A2 layer 0.15 m Presence of polylamellae in the A1 layer (0.05 m) Presence of polylamellae in the A1 layer (0.08 m) → Upper cuticle: 30.5% A; 69.5% B → Lower cuticle: 4.3% A; 95.7% B → Subsidiary cell lower cuticle: 1.6% A; 98.4% B Guard cell lower cuticle: 7% A; 93% B → G. Guignard et al. / Tissue & Cell 36 (2004) 263–273 269 √ Fig. 33. Mean and confidence interval CI (= x̄ ± (var/n) × 1.96, giving 95% ␣ risk) for each of the four types of cell cuticles. Values represent the mean ± CI. As cuticle proper A, divided in A1 polylamellate and A2 granulous layers, shows differences hardly discernable between the three lower cell cuticles compared with the upper ordinary epidermal cell cuticle, it is presented with two graphs: one on the left side with the four types of cell cuticles, including upper and lower cuticles, and one with only three lower types of cell cuticles. 270 G. Guignard et al. / Tissue & Cell 36 (2004) 263–273 ness and in qualitative aspect from normal epidermal cell cuticles has been observed before (or at least it can be seen in the figures provided by the different following authors) in fossil plants from various groups (belonging to Cheirolepidiaceae in Guignard et al., 1998; belonging to Conifers and possibly related to the Cheirolepidiaceae in Archangelsky and Taylor, 1986; belonging to Cycads or Pteridosperms in Archangelsky et al., 1986; belonging to Bennettitales in Villar de Seoane, 2001; belonging to Gingkoales in Villar de Seoane, 1997). Although these differences cannot be related with the functions of stomatal apparatus as they are fossil plants and though experiment is impossible, it can be noted that the same kinds of differences are common in living plants where stomata are known to be submitted to variations in volume, opening, and closuring processes being due to water and other molecules exchanges (Larcher, 1995; Willmer and Fricker, 1996). In the case of P. gradinarui, details of cuticle proper A provide even more precise distinctions between the four types: the upper cuticle is the most distinct with three characters/5 left, i.e. thickness of A cuticle proper, A1–A2 layers. Moreover as the two last characters (opaque and translucent lamellae) are missing in this type of cuticle because of the special A1 layer (Fig. 3), it is distinguished from the lower ordinary epidermal cell cuticle in the dichotomous key. In the set of the three lower cuticles remaining, subsidiary and guard cell cuticles have one distinct character (thickness of A1 layer) but it is interesting to note that three less distinctive characters are also present yet not taken into account in the dichotomous key (thicknesses of: A cuticle proper, opaque lamellae in A1 layer, B cuticular layer; all indicated with // in Table 2; see also diagrams in Fig. 33 showing a weak attachment between subsidiary and guard cell cuticles). 4.2. Taxonomic considerations 4.2.1. Comparisons with previous studies in P. indica, P. papillosa, P. desmomera, P. bagualensis. Time and space considerations, technical procedures, and diagenetic processes Previously studied taxa show ultrastructure similar to the present material. This is surprising since they were collected from various regions from all over the world distribution of this genus (Baldoni and Barale, 1996), with different types of sediments and diagenetic histories, and represent various time intervals. Concerning qualitative description of the cuticles, Pachypteris indica Oldham and Morris emend. Bose and Roy (1968) (Plate I, 1 and 2 in Bajpai and Maheshwari, 2000) was collected from the Early Cretaceous, Sivaganaga Formation, Naicoloma India, in arenaceous sediments. It has a thick B layer, which is their “inner electron-lucent zone, irregularly reticulate to fibrillate . . . .” It resembles P. gradinarui (collected from Lower Jurassic at Cristian, Brasov County, Romania, in fine sandstones) with fibrils showing very diverse schemes. Even herring bone fibrils are observed in their photo 2 on the right bottom side. There are a few differences in the cuticle proper A; they seem to describe only an A2 layer (their “outer electron dense zone with homogeneous matrix”), indicating that it could be an upper cuticle. But the provided magnification is not great enough to determine the presence or absence of the lightly stained A1 layer (see the present Fig. 2 with P. gradinarui where it is hardly visible at 1800× magnification, yet visible at 14,500× magnification in Fig. 3). However there is another possibility for its absence in their study, the A1 layer was not present in a few sections observed in P. gradinarui, as already noted in results. Labe and Barale (1996) observed P. papillosa (Thomas and Bose) Harris (Middle Jurassic—Bajocian-Bathonian, Hasty Bank—England, collected in fluvio-deltaic sediments) and P. desmomera (De Saporta) Barale (from Upper Jurassic—Kimmeridgian, Creys Jura—France, in lithographic limestone), and similar features exist when compared to P. gradinarui. The upper and lower cuticles descriptions clearly show differences between upper and lower cuticles, as P. gradinarui. They have an A1 polylamellate layer clearly observed for P. papillosa only in the lower cuticle as our material, however, existing for P. desmomera in the upper cuticle, but their photo pl. II 2 resembles P. gradinarui with the special A1 layer observed in the upper cuticle. They have also an A2 amorphous layer, and a B fibrilous layer that is variable in ultrastructure and described as reticulate and alveolate by the authors and with herring bone fibrils in the case of P. desmomera (Plate III 5). Baldoni and Barale (1996) observed P. bagualensis (Menéndez) Baldoni and Barale (Middle Jurassic, Neuquén Province, Argentina, collected in black clays), ultrastructure of the cuticle layers is more difficult to interpret since the authors describe it as in poor preservation (“degradacion parcial” in their text; their Plate II 7, 8 and 9). Their term “amorphous” could correspond to a certain level of degradation but it is not very clear, the cuticle has an outer dark zone without polylamellae, a middle bright zone and an inner darker zone. In addition it can be noted that despite three different procedures (maceration and preparation of resin blocks) used in the three Pachypteris papers, the images reveal the same kinds of details. Nevertheless the use of uranyl acetate-lead citrate (the present study) versus potassium permanganate in the staining (Bajpai and Maheshwari, 2000) appears to produce clearer images. As detailed above, precise quantitative measurements provide useful characters for identification of P. gradinarui. Compared with shorter measurements of previous studies, the total cuticular thickenesses of these Pachypteris species are within the range of variation found in P. gradinarui. The epidermal cell cuticle in P. indica (Bajpai and Maheshwari, 2000) is 10–17 m thick. P. papillosa (Labe and Barale, 1996) is 22 m thick for the upper epidermal cell cuticle, and 19 m for the lower one. P. desmomera (Labe and Barale, 1996) is 27 m in thickness for the upper epidermal cell cuticle, and 19 m for the lower one. P. bagualensis (Baldoni and Barale, 1996) has the most detailed measurements: for a total of 1.7–2.35 m the upper cuticle is 0.05–0.2 m thick G. Guignard et al. / Tissue & Cell 36 (2004) 263–273 for their outer dark zone (2.9–8.5% of the total that could correspond to A1 layer with degraded absent polylamellae), 0.5–0.95 m for the middle bright zone (29.4–40.4% of the total that could be the A2 granular), and 1.15–1.2 m for the inner darker zone (51.1–67.7% of the total that could be the B layer). The lower cuticle has only one measurement reported for the inner darker zone, which is 0.4–1 m thick. Labe and Barale (1996) indicated a thicker upper cuticle and a thinner lower one for P. papillosa. Other pteridosperm studies indicate this variability (Archangelsky et al., 1986; with Ticoa harrisii, noting that “the layering of the cuticle membrane is not uniform in the fossils and differs on the upper and lower epidermis”). However, future studies should provide confidence intervals with their measurements of different types of cells, as they may show difference as in the present study (Fig. 33; Table 2). In any case, they would enable comparisons with the present P. gradinarui study and precise attribution of ultrastructural characters to a rank of taxonomy, i.e. for instance if one character is in common within two species its significance moves up automatically at a higher taxonomical level (genus or family). The relationship between fossil and living plant cuticles is observed in rare cases of taxa containing both extinct and extant plants (e.g. in gingkos; Guignard and Zhou, in press) and both qualitative (description of the layers) and quantitative (measurements) data are provided. Nevertheless, the six types of cuticles defined by Holloway (1982) are used for fossil plant cuticles. For living plants this number is evidently very small compared with the few tens of very different genera and species of angiosperms and gymnosperms Holloway (1982) compared. Moreover, concluded that “each species must be considered individually and it should not be assumed that any structural features which may be observed are of universal occurrence” (Holloway, 1982, p. 28). This is also true for fossil plants, although the six types of cuticles are usually found, more precise distinctions have to be made. Even if they are successfully attributed to one of Holloway’s six types, the features may not in fact be equivalent. For instance, in Pachypteris taxa previously studied, the terms “close to” (“se rapprocherait de” in Labe and Barale, 1996), “approximately” (“aproxima” in Baldoni and Barale, 1996) and “close resemblance” (Bajpai and Maheshwari, 2000) are used. This is in accordance with Holloway’s observations on living plants. P. papillosa (Labe and Barale, 1996) was attributed to Holloway’s type 2 (“polylamellate outer region sharply delineated against inner, mainly reticulate region”) and P. desmomera (Labe and Barale, 1996) to type 1 (“outer region faintly lamellate, gradually merging with inner mainly reticulate region”). If the P. gradinarui results have only partial affinities with Holloway’s types, the situation becomes even more complicated as there are two types of affinities for this single taxon (mainly type 1 for lower cuticle, mainly type 2 for upper cuticle). For reasons discussed above, the attribution of P. bagualensis (Baldoni and Barale, 1996) to type 6 (“mainly amorphous”), possibly due to partial degradation, and of P. indica (Bajpai and 271 Maheshwari, 2000) to type 3 (“outer region amorphous, inner region mainly reticulate”), due to the possible absence of outermost polylamellae, may not provide useful criteria. 4.2.2. Position within Corystospermales According to Popa (2000), pteridosperm taxa represent a morphologically diverse and still not well understood group, especially when examining leaf form genera without attached reproductive structures. In the Corystospermales, the Northern Hemisphere, European genera, such as Pachypteris (including here the junior synonym Thinnfeldia), Cycadopteris, Komlopteris, and Rhaphidopteris, have some differences with other corystosperm form genera, such as the Southern Hemisphere Dicroidium. Only Dicroidium and Pachypteris are known as true corystosperms by their reproductive organs. The other genera, as Komlopteris, Rhaphidopteris and Cycadopteris, are reported to corystosperms by their vegetative affinities. For this reason, they may be not true corystosperms, and it can explain their ultrastructural differences. Corystosperms may not represent a natural taxon. 4.2.2.1. P. gradinarui and the genus Cycadopteris. Cycadopteris brauniana Zigno emend. Barale (Labe and Barale, 1996), the only species where ultrastructure has been examined within this genus, has two different types of cuticles (upper and lower, but less distinct than for Pachypteris species reported in the same article) as most Pachypteris species described above. However, other similarities seem to be absent. The upper cuticle is striate and rarely lamellate (Fig. 1A and B, Labe and Barale, 1996), above an amorphous and inner electron lucent zone. The lower cuticle is sparsely lamellate, followed by an amorphous zone and an innermost alveolate layer. The lower cuticle (7 m) is included in our measurements, the thickness of the upper cuticle (40 m) is not observed in P. gradinarui (maximum of 23.63 m). When compared to C. brauniana, P. gradinarui has more ultrastructural similarities with other Pachypteris than with Cycadopteris. Popa (2000) recognized macromorphological affinities between the two genera Pachypteris and Cycadopteris, and suggested that P. gradinarui may be a transitional taxon between these two genera. However, the ultrastructure of the cuticle does not support this interpretation. Based on these ultrastructural features, Pachypteris and Cycadopteris may not be that related. It was also proposed with the macromorphological study of Barale (1982). As with Pachypteris, more detailed ultrastructural study may be useful for taxonomic resolution within Cycadopteris too. 4.2.2.2. P. gradinarui and the genus Komlopteris. Cuticular ultrastructure of Komlopteris is very different from Pachypteris and Cycadopteris. Moreover, within Komlopteris many features are in closely related taxa, and thus perhaps these characters can be used at a higher taxonomic level than species. Maheshwari and Bajpai (1996a), 272 G. Guignard et al. / Tissue & Cell 36 (2004) 263–273 Bajpai (1997) and Bajpai and Maheshwari (2000) described the cuticle of Thinnfeldia indica Feistmantel (Komlopteris indica (Feistmantel) Barbacka; Barbacka, 1994). Bajpai and Maheshwari (2000) discussed the differences between Komlopteris indica and Pachypteris indica. Despite fungi and technical problems (electron dense spots), the ultrastructural similarities between Komlopteris indica and K. nordenskioeldii (Nathorst) Barbacka (studied in Guignard et al., 2001; see also Barbacka, 1994; Barbacka and van Konijnenburg-van Cittert, 1998) are striking. These cuticles are amorphous, and consist of zones with variable granule densities (Figs. 6 and 7, Bajpai, 1997; Figs. 1–3, Maheswari and Bajpai, 1996a; Plate I 3, Bajpai and Maheshwari, 2000; see also the reconstruction of the cuticle Fig. 1, Guignard et al., 2001). The cuticle is constituted of only cuticle proper A (only A2, with an absence of A1 outermost layer), and thus is very different from the Pachypteris gradinarui cuticle, except for the pillar shape structure above the anticlinal walls (Guignard et al., 2001, compare Fig. 4 and their Plate V 2 in shade cuticles). measurements of the features distinguish upper and lower epidermal and stomatal cell types. (2) Three-dimensional reconstruction and a dichotomous key (Table 3) using a combination of ultrastructural characters illustrate a difference between the four types of cell cuticles: ordinary epidermal cell cuticles of both upper and lower cuticles, and subsidiary and guard cell cuticles belonging to stomatal apparatus. (3) Comparisons with other ultrastructural studies of Pachypteris species seem to show that diagenetic processes, time and space, and/or processes related to technical procedures, are minimal within this genus. (4) This study provides a new approach that may be useful for the comparison of the cuticular ultrastructure among fossil plants. Further comparisons with other species of the same genus could enable to state about the importance of characters as criteria at species or at different taxonomic ranks. These characters are: total thickness of the cuticle, A cuticle proper and B cuticular layer thickness; A1 and A2 layers thickness; presence or absence of polylamellae in the A1 layer and their thickness. 4.3. P. gradinarui and the genera Rhaphidopteris—Dicroidium Acknowledgements The cuticular ultrastructure of Pachypteris gradinarui varies from these two other taxa, supporting the macromorphological differences noted by Popa (2000). Resemblances also exist between Rhaphidopteris and Dicroidium but are less similar than Komlopteris comparisons. Rhaphidopteris fragilis Barale (Barale, 1972) has a complex B layer composed of different zones (see Fig. 4A in Labe and Barale, 1996). The polylamellate layer has regularly arranged lamellae in the upper part and sparse, irregularly arranged, translucent lamellae in the lower part (see their Plate IV 6–9). In this respect the cuticle has ultrastructural affinities with Gingkoales cuticles (Guignard and Zhou, in press). Moreover, recent studies have shown that Rhaphidopteris is heterogeneous (Zhou and Zhang, 2000; Zhou et al., 2001), and some of the species are closely comparable with ginkgoalean fossils in gross morphology and cuticular structure. Even the lysigenous resin bodies characteristic of ginkgos have been found in the leaves of one species, R. cornuta Zhang and Zhou (1996). Maheshwari and Bajpai (1996b) have studied Dicroidium gouldii Retallack (Retallack, 1977), and show some affinities with Rhaphidopteris. For example D. gouldii also has a complex B layer (see their general views at low magnification in Plate 12 and Plate 21 for both cuticles of pinnules). Maheshwari and Bajpai (1996b) also described a Dicroidium sp., but however they were uncertain about placing it in this genus. 5. Conclusions (1) Quantitative descriptions of the cuticular ultrastructure of P. gradinarui were developed and statistical This research was partly supported by Université Claude-Bernard Lyon 1, with the Professorship offered to Dr. Mihai E. Popa during the summer of 2002. The cuticle material was kindly provided by Dr Eugen Gradinaru. We wish to thank M. Nicolas Labert for the technical assistance and members of the Centre technologique des microstructures CTM, Université Claude-Bernard 1, France. Many thanks are due to Dr. Lisa Boucher and Dr Jennifer McElwain for their English linguistic corrections. References Archangelsky, S., 1991. Ultrastructural studies in fossil plant cuticles. Curr. Sci. 61, 676–677. Archangelsky, S., Taylor, T.N., 1986. Ultrastructural studies of fossil plant cuticles. II. Tarphyderma gen. n., a Cretaceous conifer from Argentina. Am. J. Bot. 73, 1577–1587. Archangelsky, S., Taylor, T.N., Taylor, F.L.S., Kurmann, M.H., 1986. Ultrastructural studies of fossil plants cuticles: Ticoa harrisii from the early Cretaceous of Argentina. Bot. J. Linn. Soc. 92, 101–116. Bajpai, U., 1997. Taphonomic constraints on preservation of cuticles in compression fossils: fungi induced ultrastructural changes in cuticular membranes. Palaeobotanist 46, 31–34. Bajpai, U., Maheshwari, H.K., 2000. Ultrastructure of the leaf cuticle of Pachypteris indica and its comparison with Komlopteris indica. Acta Palaeobot. 40, 131–137. Baldoni, A., Barale, G., 1996. El genero Pachypteris Bronghiart emend. Harris en el jurasico medio de Argentina. Consideracion sobre la distribution estratigraphica y geographica. Rev. Esp. Paleontol. 11, 134–142. Barale, G., 1972. Sur la présence du genre Rhaphidopteris Barale dans le Jurassique supérieur de France. C.R. Acad. Sci. Paris 275, 2467–2470. G. Guignard et al. / Tissue & Cell 36 (2004) 263–273 Barale, G., 1982. Le genre Cycadopteris Zigno dans l’Ouest européen. Palaeontogr. B 183, 8–56. Barbacka, M., 1994. Komlopteris Barbacka gen. nov., a segregate from Pachypteris Brongniart. Rev. Palaeobot. Palynol. 83, 339–349. Barbacka, M., van Konijnenburg-van Cittert, J.H.A., 1998. Sun and shade leaves in two Jurassic species of Pteridosperms. Rev. Palaeobot. Palynol. 103, 209–221. Bose, M.N., Roy, S.K., 1968. On the occurrence of Pachypteris in the Jabalpur Series of India. Palaeobotanist 16, 1–9. Brongniart, A., 1828. Prodrome d’une histoire des végétaux fossiles. Levrault ed., pp. 49–50. Guignard, G., Thévenard, F., van Konijnenburg-van Cittert, J.H.A., 1998. Ultrastructure of Hirmeriella muensteri. Rev. Palaeobot. Palynol. 104, 115–141. Guignard, G., Boka, K., Barbacka, M., 2001. Sun and shade leaves? Cuticle ultrastructure of Jurassic Komlopteris nordenskioeldii (Nathorst) Barbacka. Rev. Palaeobot. Palynol. 114, 191–208. Guignard, G., Zhou, Z., Comparative studies of leaf cuticle ultrastructure between the living and oldest known ginkgos in China. Int. J. Plant Sci., in press. Harris, T.M., 1956. La cuticule des plantes fossiles. Endeavour 60, 210– 214. Harris, T.M., 1964. The Yorkshire Jurassic flora. Part 2. Caytoniales, Cycadales and Pteridosperms. Brit. Mus. (Nat. Hist.) 2, 1– 191. Holloway, P.J., 1982. Structure and histochemistry of plant cuticular membranes: an overview. In: Cutler, D.F., Alvin, K.L., Price, C.E. (Eds.), The Plant Cuticle. Linn. Soc., London, pp. 1–32. Kerp, H., Barthel, M., 1993. Problems of cuticular analysis of pteridosperms. Rev. Palaeobot. Palynol. 78, 1–18. Krings, M., Kerp, H., 1997. An improved method for obtaining large pteridosperm cuticles. Rev. Palaeobot. Palynol. 96, 453–456. Labe, M., Barale, G., 1996. Etudes ultrastructurales de la cuticule de préspermatophytes fossiles du Jurassique. Rev. Paléobiol. 15, 87– 103. Larcher, W., 1995. Physiological Plant Ecology. Springer ed., 506 pp. Lugardon, B., 1971. Contribution à la connaissance de la morphogénèse et de la structure des parois sporales chez les Filicinées isosporées. Unpublished Thesis No. 458, Toulouse University, France. 273 Maheshwari, H.K., Bajpai, U., 1996a. Biochemical degradation of the cuticular membrane in an early Cretaceous frond: a TEM study. Curr. Sci. 70, 933–935. Maheshwari, H.K., Bajpai, U., 1996b. Ultrastructure of the cuticular membrane in two Late Triassic corystospermaceous taxa from India. Palaeobotanist 45, 41–49. Popa, M.E., 2000. Aspects of Romanian Early Jurassic palaeobotany and palynology. Part II. A new species of Pachypteris from Cristian. Rev. Palaeobot. Palynol. 111, 31–47. Retallack, G.J., 1977. Triassic vegetation: microfiche supplement to a paper by Greg Retallack, 1977, reconstructing Triassic vegetation of eastern Australasia: a new approach for the biostratigraphy of Gondwanaland. Alcheringa 1, 253–283. Stewart, W.N., Rothwell, G.W., 1993. Paleobotany and the evolution of plants. Cambridge University Press ed., pp. 295–337. Taylor, W.A., Taylor, T.N., Archangelsky, S., 1989. Comparative ultrastructure of fossil and living gymnosperm cuticles. Rev. Palaeobot. Palynol. 59, 145–151. Taylor, T.N., Taylor, E.L., 1993. The Biology and Evolution of Fossil Plants. Prentice Hall ed., pp. 575–588. Vakhrameev, V., 1991. Jurassic and Cretaceous floras and climates of the Earth. Cambridge University Press ed., p. 244. Villar de Seoane, L., 1997. Comparative study between Ginkgoites tigrensis Archangelsky and Gingko biloba Linn. Leaves. Palaeobotanist 46, 1–12. Villar de Seoane, L., 2001. Cuticular study of Bennettitales from the Springhill formation, Lower Cretaceous of Patagonia, Argentina. Cretac. Res. 22, 461–479. Willmer, C., Fricker, M., 1996. Stomata. Chapman and Hall ed., 375 pp. Zhang, B., Zhou, Z., 1996. A new species of Rhaphidopteris Barale (Gymnospermae) and its taxonomic position. Acta Palaeontol. Sin. 35, 528–543 (in Chinese with English summary). Zhou, Z., Zhang, B., 2000. On the heterogeneity of the genus Rhaphidopteris Barale (Gymnospermae) with descriptions of two new species from the Jurassic Yima Formation of Henan, Central China. Acta Palaeontol. Sin. 39, 14–25. Zhou, Z., Zhang, B., Wu, X., 2001. Tharrisia, a new fossil leafy organ genus, with description of three Jurassic species from China. Palaeontogr. B 256, 95–109.