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Uvigerina celtica

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Figures 1–3. Uvigerina celtica n. sp. Surface sample PO201/10-701 off Galicia (43.700 ° N, 8.617 ° W, 188 m water depth), size fraction > 250 μm. Figure 1: paratype (no. 3722 ), note the multiple lines of small pustules between the costae. Figure 2: paratype (no. 3720 ). Figure 3: holotype (no. 3719).
 Figure 4. Uvigerina celtica n. sp. Surface sample R19 from the Oslofjord (59.299 ° N, 10.544 ° E, 87 m water depth), size fraction > 125 μm, specimen no. U86 (photo by M Schweizer, Utrecht, 2005).
 Figure 5. Uvigerina celtica n. sp. Surface sample M39009-1 from the Gulf of Cadiz (36.350 ° N, 7.142 ° W, 681 m water depth), size fraction > 250 μm.
 Figure 6. Uvigerina pigmead’Orbigny 1826. Quasitopotypic specimen, Lugagnano clay pit near Castell’Arquato, Italy, Lower Pliocene.
 Figure 7. Uvigerina pigmead’Orbigny 1826. Surface sample 16766-1 off Sierra Leone (8.292 ° N, 14.540 ° W, 2383 m water depth), size fraction 63–250 μm (photo by S. Timm, Kiel, 1992).
 Figures 8–11. Uvigerina pigmead’Orbigny 1826. All specimens from IMAGES core MD95-2039 off northern Portugal at 3381 m water depth, sample 330 cm, last Glacial, 18.7 ka (Schönfeld and others, 2003), size fraction 250–500 μm. Figure 8: apertural view (different specimen than figure 9), note the thin and low costae. Figure 9: quasi-juvenile specimen. Figures 10, 11: adult specimens, note that though specimen 11 is quite hispid, the costae are still much more delicate in comparison to Uvigerina peregrina (figure 14).
 Figures 12, 13. Uvigerina peregrina parvaLutze 1986. Surface sample PO200/10-4-1 off Cape Sines, southern Portugal (37.330 ° N, 9.510 ° W, 1265 m water depth), size fraction > 250 μm. Note the distinctively higher and more serrate costae compared to specimens 4 and 5.
 Figures 14–18. Uvigerina peregrinaCushman 1923. Figure 14: surface sample SO83 4GK, Setubal Canyon off southern Portugal (38.1828 ° N, 9.5873 ° W, 2310 m water depth), size fraction > 250 μm. Figures 15, 16: IMAGES core MD95-2040 off northern Portugal at 2465 m water depth, sample 2–3 cm, size fraction > 250 μm, late Holocene. Note the much more robust costae in figure 16 in comparison to figure 8. Figure 17: surface sample SO16416-1 southern Florida Straits (24.198 ° N, 80.716 ° W, 826 m water depth), size fraction > 250 μm. Figure 18: surface sample PO201/10-749 off Brittany (47.609 ° N, 7.915 ° W, 2011 m water depth), size fraction > 250 μm.

Figures 1–3. Uvigerina celtica n. sp. Surface sample PO201/10-701 off Gal... Available to Purchase

Published: 01 October 2006
PLATE 1 Figures 1–3. Uvigerina celtica n. sp. Surface sample PO201/10-701 off Galicia (43.700 ° N, 8.617 ° W, 188 m water depth), size fraction > 250 μm. Figure 1: paratype (no. 3722 ), note the multiple lines of small pustules between the costae. Figure 2: paratype (no. 3720 ). Figure 3
Journal Article

TAXONOMY AND DISTRIBUTION OF THE UVIGERINA PEREGRINA PLEXUS IN THE TROPICAL TO NORTHEASTERN ATLANTIC Available to Purchase

Joachim Schönfeld
Published: 01 October 2006
Journal of Foraminiferal Research (2006) 36 (4): 355–367.
DOI: https://doi.org/10.2113/gsjfr.36.4.355
...PLATE 1 Figures 1–3. Uvigerina celtica n. sp. Surface sample PO201/10-701 off Galicia (43.700 ° N, 8.617 ° W, 188 m water depth), size fraction > 250 μm. Figure 1: paratype (no. 3722 ), note the multiple lines of small pustules between the costae. Figure 2: paratype (no. 3720 ). Figure 3...
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View PDF for article title, TAXONOMY AND DISTRIBUTION OF THE <span class="search-highlight">UVIGERINA</span> PEREGRINA PLEXUS IN THE TROPICAL TO NORTHEASTERN ATLANTIC
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Maximum transversal diameter (MTD) versus the maximal length (maxL) of Uvigerina peregrina (all three populations of Figure 3) in comparison to a) Uvigerina peregrina parva, b) Uvigerina celtica n. sp., and c) Uvigerina pigmea. The curves display logarithmical regression lines (Uvigerina peregrina: MTD =− 729.3 + 402.72 * log (maxL), R: 0.89. Uvigerina peregrina parva: MTD = −670.8 + 361.75 * log (maxL), R: 0.91. Uvigerina celtica n. sp.: MTD = −484.5 + 284.09 * log (maxL), R: 0.81. Uvigerina pigmea: MTD = −526.8 + 300.33 * log (maxL), R: 0.89). d) Frequency distribution box plots of the maxL/MTD ratios of the species. Bars: 10th and 90th percentile, boxes: lower quartile, median and upper quartile, asterisk: mean value, cirles: outliers. The number of observations is given on top or bottom of the diagrams.

Maximum transversal diameter (MTD) versus the maximal length (maxL) of Uvi... Available to Purchase

Published: 01 October 2006
F igure 4. Maximum transversal diameter (MTD) versus the maximal length (maxL) of Uvigerina peregrina (all three populations of Figure 3 ) in comparison to a) Uvigerina peregrina parva , b) Uvigerina celtica n. sp., and c) Uvigerina pigmea . The curves display logarithmical regression
Journal Article

Foraminifera on the Demerara Rise offshore Surinam: crustal subsidence or shallowing of an oxygen minimum zone? Available to Purchase

BRENT WILSON, LEE-ANN C. HAYEK
Published: 12 December 2014
Geological Magazine (2015) 152 (5): 788–801.
DOI: https://doi.org/10.1017/S0016756814000673
... Uvigerina celtica – – – – – 0.03 – – – Uvigerina peregrina 0.12 0.13 0.08 0.05 0.05 0.10 0.31 0.29 0.15 Mean CoBI p for species with CoBIp >0.02 0.15 0.05 0.07 0.09 0.08 0.06 0.13 0.09 0.09 Twenty-four species had a partial...
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View PDF for article title, Foraminifera on the Demerara Rise offshore Surinam: crustal subsidence or shallowing of an oxygen minimum zone?
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Journal Article

LIVE BENTHIC FORAMINIFERAL FAUNAS ALONG A BATHYMETRICAL TRANSECT (282–4987 M) ON THE PORTUGUESE MARGIN (NE ATLANTIC) Available to Purchase

Mark Phipps, Frans Jorissen, Antonio Pusceddu, Silvia Bianchelli, Henko De Stigter
Published: 01 January 2012
Journal of Foraminiferal Research (2012) 42 (1): 66–81.
DOI: https://doi.org/10.2113/gsjfr.42.1.66
... are distinguished: (1) eutrophic upper-slope stations (282–1002 m) with faunas dominated by Uvigerina mediterranea, U. elongatastriata, Melonis barleeanus, Bigenerina nodosaria, Trifarina bradyi, Epistominella vitrea, Cribrostomoides bradyi , and Bolivina robusta, (2) mesotrophic middle- to lower-slope stations...
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View PDF for article title, LIVE BENTHIC FORAMINIFERAL FAUNAS ALONG A BATHYMETRICAL TRANSECT (282–4987 M) ON THE PORTUGUESE MARGIN (NE ATLANTIC)
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Journal Article

DISTRIBUTION OF BENTHIC FORAMINIFERA IN COARSE SEDIMENTS, RÍA DE VIGO, NW IBERIAN MARGIN Available to Purchase

Paula Diz, Guillermo Francés, Susana Costas, Carlos Souto, Irene Alejo
Published: 01 October 2004
Journal of Foraminiferal Research (2004) 34 (4): 258–275.
DOI: https://doi.org/10.2113/34.4.258
... belong to the Trochamminacea ( Lepidodeuterammina ochracea, Remaneica helgolandica, R. plicata, R. anglica, Deuterammina rotaliniformis, D. eddystonensis, D. celtica, Portatrochammina murrayi, Rotaliammina mayori ). Calcareous foraminifera are mainly rotaliids and spirillinids; miliolids are very scarce...
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View PDF for article title, DISTRIBUTION OF BENTHIC FORAMINIFERA IN COARSE SEDIMENTS, RÍA DE VIGO, NW IBERIAN MARGIN
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