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Neoeponides duwi

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Journal Article
Published: 01 January 2003
Micropaleontology (2003) 49 (2): 146–150.
...Robert P. Speijer Abstract The holotype of Neoeponides duwi ( Nakkady 1950 ), originally described as a variety of Discorbis pseudoscopos Nakkady, is re-described and re-figured. This species appears to have no phylogenetic relationship with D. pseudoscopos. Neoeponides duwi is recorded...
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Studied localities (triangles) in Egypt where  <span class="search-highlight">Neoeponides</span> <span class="search-highlight">duwi</span>  is observe...
Published: 01 January 2003
TEXT-FIGURE 1 Studied localities (triangles) in Egypt where Neoeponides duwi is observed.
Image
Scale bars100μm
 1a–c Holotype of the species described as  Discorbis pseud...
Published: 01 January 2003
PLATE 1 Scale bars100μm
 1a–c Holotype of the species described as Discorbis pseudoscopos Nakkady (Natural History Museum, London No. P41731)
 2a–c Holotype of Neoeponides duwi (Nakkady) (Natural History Museum, London No. P41733). Note the poor visibility of the umbilical features, compared
Journal Article
Published: 20 April 2018
Journal of Foraminiferal Research (2018) 48 (2): 100–120.
... curve records the typical carbon isotope excursion (CIE) and shows four distinctive intervals (pre-CIE, CIE-“core”, CIE-“recovery”, post-CIE) over the entire PETM interval in both cores. In the pre-CIE interval, the more proximal site (OS–01) shows high abundances of Neoeponides duwi co-occurring...
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Journal Article
Published: 01 September 2011
Journal of Micropalaeontology (2011) 30 (2): 167–182.
..., but contains pyrite and fish remains, and is interpreted as an anoxic level formed during rapid relative sea-level rise. Incursion of a Neoeponides duwi (Nakkady, 1950) benthic assemblage in LDE bed II is interpreted as repopulation of the seafloor after anoxia. The sea-level cycle associated with the LDE...
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Benthic foraminifera of core OS–01. All scale-bars represent 100 μm.  1  Ne...
Published: 20 April 2018
Figure 4. Benthic foraminifera of core OS–01. All scale-bars represent 100 μm. 1 Neoeponides duwi (61.50 m; OS–01); 2 Anomalinoides zitteli (60.90 m; OS–01); 3 Oridorsalis plummerae (60.50 m; OS–01); 4 Anomalinoides affinis (60.70 m; OS-01); 5 Valvulineria scrobiculata (60.70 m; OS
Journal Article
Published: 01 October 2003
Journal of Foraminiferal Research (2003) 33 (4): 355.
...., Systematics and paleoecology of the foraminifer Neoe-ponides duwi (Nakkady) from the Paleocene of Egypt.—Micro-paleontology, v. 49, no. 2, 2003, p. 146–150, 1 figure, 1 plate.—“The holotype of Neoeponides duwi (Nakkady 1950), originally described as a variety of Discorbis pseudoscopos Nakkady, is re...
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Typical planktic and benthic foraminifera in the Qreiya 3 section.  figs 1–...
Published: 01 September 2011
. Benthic foraminifera from the LDE interval: 9, Siphogenerinoides esnehensis , sample Q3–35 (8.0 m); 10, Neoeponides duwi , spiral view, sample Q3–44 (8.40 m); figs 11–17 . Benthic foraminifera with an outer neritic and bathyal habitat: 11, Cibicidoides pseudoacutus , spiral view, sample Q3–1 (0.0 m
Journal Article
Published: 01 December 2009
Journal of the Geological Society (2009) 166 (6): 1135–1142.
... oxygenation have caused enhanced preservation of organic matter during both events; (2) both event deposits show a very high planktonic/benthic foraminiferal ratio, and the benthic foraminiferal assemblage is dominated by opportunistic taxa indicating shallow water ( Neoeponides duwi in the latest Danian...
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Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 15–40.
.... TEXT-FIGURE 3 Bio-and chemostratigraphy of the upper Paleocene-lower Eocene succession at G. Owaina (A), G. Duwi (B) and G. Abu Had (C) (from Von Salis et al. 1998 ). Recent integrated studies by members of the P/E Boundary Working Group in southern Egypt have enabled a higher resolution...
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