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Figure 1 in New record of the rare flounder Parabothus budkeri (Chabanaud, 1943) (Teleostei: Bothidae) from the Gulf of Aqaba, northern Red Sea, with a key to the genus Parabothus

Figure 1. – Parabothus budkeri (Chabanaud, 1943), HUJ 1635, 1 male, 49.7 mm SL, Red Sea, Gulf of Aqaba, Israel, Eilat. Photograph by D. Golani. Ocular side.

Figure 2. – Significant French ichthyological records for 2017. A in French ichthyological records for 2017

Figure 2. – Significant French ichthyological records for 2017. A: Sphyrna zygaena, ~250 cm, 18 Sep. 2017, (photo by Rémy Descamps); B: Acipenser sturio, 922 mm TL, 22-23 Apr. 2017, MNHN-IC 2019-0092; C: Muraena helena, 1153 mm TL, 11 Feb. 2017, MNHN-IC 2019-0093; D: Nessorhamphus ingolfianus, 460 mm TL, 29 Oct. 2017, MNHN-IC 2019-0094; E: Evermannella balbo, 123 mm TL, 29 Oct. 2017, MNHN-IC 2019-0095; F: Raniceps raninus, 118 mm TL, 22 Nov. 2017, MNHN-IC 2019-0096; G: Cheilopogon heterurus, 370 mm TL, 23 June 2017, MNHN-IC 2019-0097; H: Scopelogadus beanii, 97 mm TL, 29 Oct. 2017, MNHN-IC 2019-0098; I: Zenopsis conchifer, 245 mm TL, 10 Oct. 2017; J: Eutelichthys leptochirus, 68 mm TL, 22 June 2017, MNHN-IC 2019-0099.

Figure 3. – Selected fishes from the White Nile. A in New and rare records of fishes from the White Nile in the Republic of the Sudan

Figure 3. – Selected fishes from the White Nile. A: Clarias werneri, 129 mm SL, Kosti; B-D: Haplochromis sp. "Kosti", 35 mm SL, Kosti; E: Sarotherodon galilaeus, 119 mm SL, Al Jabalayn; F: Sarotherodon sp."round head", 133 mm SL, Kosti.

Figure 2. – Selected fishes recorded from the White Nile. A-F and I-J in New and rare records of fishes from the White Nile in the Republic of the Sudan

Figure 2. – Selected fishes recorded from the White Nile. A-F and I-J from Al Jabalayn. A: Brevimyrus niger, male, 137 mm SL; B: Mormyrus hasselquistii, 282 mm SL; C: Petrocephalus keatingii, male, 145 mm SL; D: Pollimyrus petherici, 200 mm SL; E: Neolebias unifasciatus, female, 22mm SL; F: N. unifasciatus, male, 20 mm SL; G: N. unifasciatus, 18.2 mm SL, BMNH 1948.1.14.6-8; H: N. trewavasae, 19.7 mm SL, BMNH 1948.1.14.11; I. Paradistichodus dimidiatus, 42 mm SL; J: Enteromius macrops, 39 mm SL. (Photos G & H by The Trustees of the Natural History Museum, London).

Figure 1 in Redescription of the ocellus-bearing cuskeel Neobythites kenyaensis (Ophidiidae), with new Southeast African records and remarks on intraspecific morphological and colour variation

Figure 1. – Map with sampling localities for Neobythites kenyaensis. Number of specimens indicated for localities with multiple occurrences.

Figure 4 in Redescription of the ocellus-bearing cuskeel Neobythites kenyaensis (Ophidiidae), with new Southeast African records and remarks on intraspecific morphological and colour variation

Figure 4. – Radiograph of Neobythites kenyaensis, SAIAB 98890, 102 mm SL (M. Lisher). Inverted colour version on bottom.

FIGURE 8 in Termite nests in eolian backshore settings: An unusual record throughout the Quaternary in the Neotropical realm

FIGURE 8. Hypogean structures in nest D.4. Successive cuts evidencing a general funnel shape (a, b) and agglomer- ated passages (c, d) as a lateral projection.

FIGURE 7. Termite nests from site D in Termite nests in eolian backshore settings: An unusual record throughout the Quaternary in the Neotropical realm

FIGURE 7. Termite nests from site D. General view of nests close to the shoreline (a); grass around the mounds. Detail of big epigeal portion in D.6 (b). Details of the cast nest D.4 (c). Detail of passages of epigeal portion and the surrounding roots in the bottom portion (d). Schematic disposition of termite nests in cross-section (e) and plan view (f); the closest nest is ca. 58 m from shoreline.

FIGURE 4. Termite nests from site B in Termite nests in eolian backshore settings: An unusual record throughout the Quaternary in the Neotropical realm

FIGURE 4. Termite nests from site B. General view of nest B.1 (a) and proximity to the shoreline; sparse vegetation of grasses and ferns around the mound. Detailed view of B.1 nest cast (b) and lateral projections mostly inside roots. Detail of the passages inside roots (c), cast by resin. Schematic disposition of termite nests in cross-section (d) and in plan view (e); closest nest is nearly 50 m from shoreline, where the nests are concentrated in interdune settings in the frontal dune zone.

FIGURE 5. Termite nests from site C in Termite nests in eolian backshore settings: An unusual record throughout the Quaternary in the Neotropical realm

FIGURE 5. Termite nests from site C. General view of nest C.1, next to a stream (a); it is seem a diverse vegetation close to the permanent stream, but the termite nests are restrict to grass. Detail of nest C.1 surrounded by grass (b). Detail of the inner passages of nest C.2 surrounded by grass roots (c). Schematic disposition of the termite nests in cross-section (d) and plan view (e); closest nest is approximately 170 m from the shoreline, where the nests are concentrated in the wet interdune zone.

FIGURE 1 in Termite nests in eolian backshore settings: An unusual record throughout the Quaternary in the Neotropical realm

FIGURE 1. Schematic map of studied areas (red circles). In this study only coastal occurrences of termite nests were considered. Site A: 29°23'3.26"S, 49°45'29.94"W; Site B: 30° 5'21.61"S, 50°10'9.26"W; Site C: 31° 9'34.00"S, 50°49'0.12"W; Site D: 33°43'40.44"S, 53°21'3.80"W. Modified from Google Earth.

FIGURE 12 in Tracking biases in the regular echinoid fossil record: The case of Paracentrotus lividus in recent and fossil shallow-water, high-energy environments

FIGURE 12. Relative abundance of Paracentrotus lividus spine remains. A, Is Mesas (Pleistocene-Bulk sample). B, Sa Mesa Longa Beach (Recent-Surface collection). C, Sa Mesa Longa Beach (Bulk sample). N = number of counted specimens.

FIGURE 13 in Tracking biases in the regular echinoid fossil record: The case of Paracentrotus lividus in recent and fossil shallow-water, high-energy environments

FIGURE 13. Biostratinomic signatures (abrasion and encrustation) of spine remains. A, Is Mesas (Pleistocene-Bulk sample). B, Sa Mesa Longa Beach (RecentSurface collection). C, Sa Mesa Longa Beach (RecentBulk sample). N = number of counted specimens

FIGURE 11 in Tracking biases in the regular echinoid fossil record: The case of Paracentrotus lividus in recent and fossil shallow-water, high-energy environments

FIGURE 11. Distribution of ambulacral and interambulacral plates in the two sediment fractions (> 2 mm and 1-2 mm) investigated herein. N = number of counted specimens.

FIGURE 9 in Tracking biases in the regular echinoid fossil record: The case of Paracentrotus lividus in recent and fossil shallow-water, high-energy environments

FIGURE 9. Relative abundance of Paracentrotus lividus test remains. A, Is Mesas (Pleistocene-Bulk sample). B, Sa Mesa Longa Beach (Recent-Surface collection). C, Sa Mesa Longa Beach (Bulk sample). N = number of counted specimens.

FIGURE 10 in Tracking biases in the regular echinoid fossil record: The case of Paracentrotus lividus in recent and fossil shallow-water, high-energy environments

FIGURE 10. Biostratinomic signatures (fragmentation, abrasion and encrustation) of echinoid test remains. A, Is Mesas (Pleistocene-Bulk sample). B, Sa Mesa Longa Beach (Recent-Surface collection). C, Sa Mesa Longa Beach (Recent-Bulk sample). N = number of counted specimens. Numbers (1-11) are explained in Figure 9. Colors: dark grey, light grey and black represent fragmentation, abrasion and encrustation, respectively.

FIGURE 6. A in Tracking biases in the regular echinoid fossil record: The case of Paracentrotus lividus in recent and fossil shallow-water, high-energy environments

FIGURE 6. A, Panoramic view of Sa Mesa Longa Beach (Central-western Sardinia). B-H, Recent remains of Paracentrotus lividus from Sa Mesa Longa. B, Complete denuded test showing encrustation by serpulids. C, Test fragment made up of several ambulacral and interambulacral plates sutured together, showing inter- and intraplate fragmentation and encrustation by coralline algae and the polychaete Spirorbis. D, Internal view of a large test fragment affected by intraplate fragmentation and encrustation by serpulid worms. E, Two interambulacral plates showing abrasion and encrustation by Spirorbis. F, Single ambulacral plates showing fragmentation (white arrow). G, Epiphysis from the jaw apparatus showing fragmentation and abrasion. H, Madreporite from the apical system affected by fragmentation (white arrow). I, Test fragment of Arbacia lixula showing intraplate fracturing. J, Complete test of Echinocyamus pusillus. B, C, D, I, J Scale bar equals 1 cm. E–H scale bars equal 0.5 cm.

FIGURE 7 in Tracking biases in the regular echinoid fossil record: The case of Paracentrotus lividus in recent and fossil shallow-water, high-energy environments

FIGURE 7. Scanning electron micrographs of suture faces in recent Paracentrotus lividus. A, Interradial suture between interambulacral plates showing galleried stereom with galleries running in aboral-oral direction. A1, Detail of the galleried stereom and collagen fibers. B, Adradial suture of interambulacral plates showing galleried stereom. B1, Detail of the parallel galleries and collagen fibers. C, Adapical suture of an interambulacral plates showing knob-like trabecular protrusions and cavities. C1, The close-up shows numerous knob-like protrusions some of which are interconnected to one another in twos, threes or more. D, Adoral suture of ambulacral plates; 1) Radial ridge at the boundary between ambulacral plates (running across perradial sutures) and 2) galleried stereom. A, B, C Scale bars equal 100 µm; A1, B1, C1 Scale bars equal 20 µm. D Scale bar equals 1 mm.

FIGURE 8 in Tracking biases in the regular echinoid fossil record: The case of Paracentrotus lividus in recent and fossil shallow-water, high-energy environments

FIGURE 8. Size-frequency distribution of the rotulae of the Aristotle's lantern both in Pleistocene deposit and recent setting. Each box-plot represents 25 and 75 percent quartile of all values, Q1 and Q3 respectively. Black line inside the box represents the median. Whiskers are drawn from Q1 and Q3 to the largest values less than 1.5 times the Interquartile range (Q1-Q3). N = number of counted specimens.

FIGURE 4. Associated fauna from levels A and B in Tracking biases in the regular echinoid fossil record: The case of Paracentrotus lividus in recent and fossil shallow-water, high-energy environments

FIGURE 4. Associated fauna from levels A and B of the Is Mesas deposit (Late Pleistocene). A, Patella caerulea. B, Diodora gibberula. C, Cerithium vulgatum. D, Hexaplex trunculus. E, Melarhaphe neritoides. F, Acanthocardia tuberculata. G, Irus irus. H, Arca noae. I, Cardita calyculata. J, Cladocora caespitosa. Scale bars equal 1 cm.