Find research datasets worth reusing

Fig. 11 in The Hirnantian (Late Ordovician) brachiopod fauna of the East Baltic: Taxonomy of the key species

Fig. 11. Dalmanellid brachiopods from the Kuldiga Formation of the Porkuni Regional Stage, Hirnantian (Upper Ordovician), East Baltic, western Latvia A–D, F–I) and southwestern Estonia (E). A, B, D, H, I. Onniella sp. A. Dorsal valve, GIT 542-66, Aispute-41, depth 1001.15 m, exterior view. B. Ventral valve, LDM 382-50, Dižrungi-17, 896.0 m, ventral view. D. Shell, GIT 542-471, Riekstini-15, 860.85, dorsal (D 1), ventral (D 2), and lateral (D 3) views. H. Dorsal valve, GIT 542-480, Krjukai, 968.6 m, dorsal exterior view. I. Shell, GIT 542-472, Kandava-26, 964.5 m, ventral (I 1) and dorsal (I 2) views. C, E, F. Draborthis cf. caelebs Marek and Havliček, 1967. C. Dorsal valve, GIT 542-392, Riekstini-15, 857.5, interior view. E. Dorsal valve, GIT 542- 67, Ruhnu-500, 914.0 m, exterior view. F. Dorsal valve, GIT 542-4393, Mežmali-16, 913.2 m, interior view. G. Drabovia sp., dorsal valve, GIT 542-473, Mežmali-16, 910.1 m, interior view. Scale bars 2 mm.

Fig. 5 in The Hirnantian (Late Ordovician) brachiopod fauna of the East Baltic: Taxonomy of the key species

Fig. 5. Leptostrophiid brachiopod Eostropheodonta hirnantensis (M`Coy, 1851) from the Kuldiga Formation of the Porkuni Regional Stage, Hirnantian (Upper Ordovician), East Baltic, western Latvia. A. Ventral valve, GIT 542-316, Riekstini-15, depth 850.3 m, ventral exterior view. B. Ventral valve, GIT 542-333, Riekstini-15, 854.0 m, fragment of valve with ornament (B 1) and exterior view (B 2). C. Juvenile specimen, GIT 542-319, Mežmali-16, 906.56 m, ventral exterior view. D. Ventral valve, GIT 542-385, Aispute-41, 1000.5 m, interior view. E. Bedding plane with numerous casts of valves, GIT 542- 360, Vilcini-19, 906.5 m.

Fig. 4 in The Hirnantian (Late Ordovician) brachiopod fauna of the East Baltic: Taxonomy of the key species

Fig. 4. Strophomenoid brachiopods from the Kuldiga Formation of the Porkuni Regional Stage, Hirnantian (Upper Ordovician), East Baltic, western Latvia (A–F, H) and southwestern Estonia (G). A, B, F–H. Paromalomena polonica (Temple, 1965). A. Dorsal valve, GIT 542-299, Mežmali-16, depth 911.8 m, exterior view. B. Dorsal valve, GIT 542-352-1, Adze-6, 844.5 m, split into two parts: exterior view (B1) and impression (B2). F. Dorsal valve, GIT 542-377, Aispute-41, 884.4 m, exterior view. G. Dorsal valve, GIT 542-361, Ikla, 535.3 m, exterior view. H. Dorsal valve, GIT 542-355, Mežmali-16, 912.2 m, exterior view (H 1) and view of the chilidium (H2). C. Eostropheodonta cf. parvicostellata Rong, 1984. Dorsal valve, GIT 542-365, Aispute-41, depth 988.7 m, exterior view. D–E. Proboscisambon? sp. D. Mould of dorsal valve, GIT 542-53, Stirnas-18, depth 908.2 m, exterior view. E. Dorsal valve, GIT 542-322-1, exterior view; Riekstini-15, 858.6 m. Scale bars 2 mm.

Fig. 2. A in The Hirnantian (Late Ordovician) brachiopod fauna of the East Baltic: Taxonomy of the key species

Fig. 2. A. The facies belts in the Baltic Basin and the study area. B. The location of drill core sections. C. Enlarged Jurkalne area. Black dots mark the locality of the drill core with brachiopods of the Hirnantia Fauna; empty dots indicate occurrences of the Hirnantia Fauna (from Paškevičius 1997, 2000). Drill cores: 1, Stirnas-18; 2, Pliekalni-14: 3, Dizrungi-17, 4, Vilcini-19; 5, Adze-6; 6, Dreimaņi-11; 7, Riekstini-15; 8, Mežmaļi-16; 9, Mežvagari-13, 10, Ēdole-60; 11, Anši. Distribution of the Hirnantian rocks: a, outer limit the the Porkuni Stage, including of the Saldus Formation on the NE areas; b, outer limit of the Saldus Formation in northern part of region; c, outer limits of the distribution area of the Kuldiga Formation.

Fig. 3 in The Hirnantian (Late Ordovician) brachiopod fauna of the East Baltic: Taxonomy of the key species

Fig. 3. Leptaenin brachiopods from the Kuldiga Formation of the Porkuni Regional Stage, Hirnantian (Upper Ordovician), East Baltic, western Latvia A–D, F–G), southwestern Estonia (E). A, B, D, F, G. Leptaena (L.) rugosa (Dalman, 1828). A. Shell, LDM G 273-1, Ēdole-60 drill core, depth 840.7 m, ventral (A1) and ventro-lateral (A2) views. B. Shell, GIT G 542-2, Vilcini-15, 910.35 m (figured in Kaljo et al. 2008), ventral (B1) and posterior (B2) views. D. Shell, GIT 542-17, Stirnas-18, 908.6 m, dorsal exterior view. F. Shell, GIT 542-18, Stirnas-18, 909.4 m, ventral view. G. Dorsal valve, GIT 542-197, Sturi-8, 941.8 m, view of interior (G1) and cruralium (G2). C, E. Leptaena sp. C. Dorsal valve, GIT 542-189, Vilcini-15, 909.3 m, exterior view. E. Incomplete ventral valve, GIT 542-192, Ikla, 536.5 m, exterior view. Scale bars 10 mm.

Fig. 9 in The prevalence of Corynosoma parasite worms in the great cormorants and the Baltic herring in the northern Baltic Sea, Finland

Fig. 9. Size differences between infected and non-infected cormorants. The black line represents the median length (a and b) and median weight (c). The grey box represents the middle 50% of the data (n = 65).

Fig. 7 in The prevalence of Corynosoma parasite worms in the great cormorants and the Baltic herring in the northern Baltic Sea, Finland

Fig. 7. Size differences of cormorants between Kustavi and Airisto in terms of body length and body weight (n = 65). The black line represents the median length and weight. The grey box represents the middle 50% of the data (n = 65).

Fig. 6 in The prevalence of Corynosoma parasite worms in the great cormorants and the Baltic herring in the northern Baltic Sea, Finland

Fig. 6. Left: Body length of herring in the Archipelago Sea (n = 1167) and the Bothnian Sea (n = 1528) in 2018 and in the infected and non-infected herring (n = 7002). The black line represents the median length, and the grey box is the middle 50% of the data.

Fig. 2 in The prevalence of Corynosoma parasite worms in the great cormorants and the Baltic herring in the northern Baltic Sea, Finland

Fig. 2. Mean annual salinity (PSU) and temperature (T, ◦C) of the winter months (January–April) in the Bothnian Sea at 0–50 m depth during 1980–2021. Data from ICES Oceanographic dataset, 2021. ICES, Copenhagen.

Fig. 8 in The prevalence of Corynosoma parasite worms in the great cormorants and the Baltic herring in the northern Baltic Sea, Finland

Fig. 8. Size differences of cormorants between sexes (a, b, and c) and adults and juveniles (d, e, and f). The black line represents the median length (a, b, d, and e) and median weight (c and f). The grey box represents the middle 50% of the data (n = 65).

Fig. 3 in The prevalence of Corynosoma parasite worms in the great cormorants and the Baltic herring in the northern Baltic Sea, Finland

Fig. 3. Acanthocephala parasites in the body cavity of a herring (left; the red circle indicates the position of worms) and on the inner surface of the intestine of a cormorant (right). The upper photo indicates the size of parasites compared to a match (photos: J. Sahlst´en). (For interpretation of the references to colour in this figure legend, the reader is referred to the Web version of this article.)

Fig. 1 in The prevalence of Corynosoma parasite worms in the great cormorants and the Baltic herring in the northern Baltic Sea, Finland

Fig. 1. Map showing the sampling sites in the northern Baltic Sea: A = Archipelago Sea, B = Uusikaupunki, C = Merikarvia. The sampling locations in region A: 1 = Taivassalo, 2 = Velkua trawl area, 3 = western Rym¨attyl¨a, 4 = northern Airisto Inlet, 5 = Peimari.

Fig. 5 in The prevalence of Corynosoma parasite worms in the great cormorants and the Baltic herring in the northern Baltic Sea, Finland

Fig. 5. Prevalence (%) of the corynosoma infection in the Baltic herring in the Bothnian Sea (n = 1528) and the Archipelago Sea in 2018 (n = 1167). The black solid line expresses a linear trend: y = 7.55x + 6.33, r = 1.00.

Fig. 6 in New brachiopods from the Lower-Middle Ordovician (Billingen-Volkhov stages) of the East Baltic

Fig. 6. Bivariate plots of 51 measured specimens of Leoniorthis robusta. Solid rhombi represent specimens from Putilovo mud mound, open squares represent specimens from Popovka River, triangles represent specimens from Suhkrumägi road cut.

Fig. 5 in New brachiopods from the Lower-Middle Ordovician (Billingen-Volkhov stages) of the East Baltic

Fig. 5. Leoniorthis robusta gen. et. sp. nov. A–F. Specimens from Putilovo mud mound. G–J. Specimens from Popovka River. A. Holotype, PMU In 110, dorsal exterior (A1) and interior (A2). B. PMU In 111, ventral exterior. C. PMU In 145, ventral interior. D. PMU In 144, ventral interior. E. PMU In 120, dorsal interior (E1); enlargement of cardinal region (E2). F. PMU In 153, oblique view of hingeline and dorsal valve of conjoined specimen. G. PMU In 121, dorsal exterior. H. PMU In 122, dorsal interior. I. PMU In 125, ventral exterior. J. PMU In 123, ventral interior. Scale bars 1 mm.

Fig. 2 in New brachiopods from the Lower-Middle Ordovician (Billingen-Volkhov stages) of the East Baltic

Fig. 2. The standard section in Putilovo Quarry compared with the mud mound section (after Tolmacheva, Fedorov, and Egerquist in press). Levels with occurrences of Neumania paucicostata are marked with squares; levels with Leoniorthis robusta are marked with circles.

Fig. 4 in New brachiopods from the Lower-Middle Ordovician (Billingen-Volkhov stages) of the East Baltic

Fig. 4. Neumania paucicostata sp. nov. Specimens from Putilovo Quarry. A. Holotype PMU In 108; ventral valve interior (A1), enlargement of the spondylium showing the muscle attachment area (A2). B. PMU In 113, oblique internal view of ventral valve showing the U−shaped spondylium. Note that this specimen does not possess rounded muscle scars as in the holotype. C. PMU In 112, enlargement of spondylium on broken ventral valve, slightly oblique view showing theroughmuscleattachmentarea. D.PMUIn109,ventralviewofconjoinedspecimen. E.ExteriorofspecimenPMUIn228indifferentviews. F.PMUIn107, dorsal interior and exterior. G. PMU In 224; oblique posterior view of cardinalia (G1), dorsal valve interior (G2). Scale bars 1 mm.

Fig. 3. Neumania paucicostata. A. Dorsal valve interior showing the anteriorlylobedmusclescars,drawnfromspecimenPMUIn107. B in New brachiopods from the Lower-Middle Ordovician (Billingen-Volkhov stages) of the East Baltic

Fig. 3. Neumania paucicostata. A. Dorsal valve interior showing the anteriorlylobedmusclescars,drawnfromspecimenPMUIn107. B.Lateralview of ventral valve drawn from specimen PMU In 108 (holotype).

opencc-by-4.0Dec 2017View details →

FIGURE 1. 1-2 in Who's that girl? A singular Tropiduchidae planthopper from the Eocene Baltic amber (Hemiptera: Fulgoromorpha)

FIGURE 1. 1-2, FT-IR spectra of the amber specimen MAI UG 508762: FT-IR spectrum (1) and ATR corrected FT-IR spectrum with baseline corrected (2). 3-4, Piece of amber MAI UG 508762 with inclusion of Gedanotropis sontagae gen. et sp. nov., lower (3) and upper (4) sides.