A review and revision of the Jurassic-Early Cretaceous Globigerinina, with especial reference to the Aptian assemblages of Speeton (North Yorkshire, England)

Banner, F. T.; Desai, Damini

doi:10.1144/jm.7.2.143

Cited by 72 publications

(31 citation statements)

References 32 publications

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“…However, Loeblich and Tappan (1987) did not consider wall microstructure as an important distinguishing feature for the hedbergellids and, as a result, they synonymized Praehedbergella under Hedbergella. Banner and Desai (1988) resurrected Praehedbergella by implicitly limiting its definition to include only FIGURE 7. Biostratigraphic ranges, percent planktic foraminifera, and mean, maximum and minimum test diameter for planktic species across the Aptian/Albian boundary interval in ODP Hole 1049C.…”

Section: Taxonomic Notes and Phylogenetic Classification Of The Aptiamentioning

confidence: 99%

Planktic Foraminiferal Species Turnover Across Deep-Sea Aptian/ Albian Boundary Sections

Huber

Leckie

2010

The Journal of Foraminiferal Research

141

137

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A major planktic foraminiferal species turnover accompanied by a dramatic reduction in shell size, a fundamental change in shell architecture, and a precipitous drop in the abundance of planktic relative to benthic species occurs across the Aptian/Albian boundary interval (AABI) at globally distributed deep-sea sections. Extinction of the large and distinctive planktic foraminifer Paraticinella eubejaouaensis, used to denote a level at or near the Aptian/ Albian boundary, coincides with the extinctions of relatively long-ranging

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Section: Taxonomic Notes and Phylogenetic Classification Of The Aptiamentioning

confidence: 99%

Planktic Foraminiferal Species Turnover Across Deep-Sea Aptian/ Albian Boundary Sections

Huber

Leckie

2010

The Journal of Foraminiferal Research

141

137

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“…In particular, (1) Hedbergella excelsa and the possible H. aptiana, from the lowermost assemblage, do not range above the lower Aptian (Longoria, 1974;Banner and Desai, 1988). The mean sizes of all the individuals, not exceeding 250 µm, also are characteristic of lower Aptian assemblages (see Tornaghi et al, 1989).…”

Section: Planktonic Foraminifersmentioning

confidence: 99%

Cretaceous Calcareous Plankton Biostratigraphy of Sites 872 through 879

Erba

Silvá

Watkins³

1995

Proceedings of the Ocean Drilling Program, 144 Scientific Results

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This paper documents the distribution of calcareous nannofossils and planktonic foraminifers in Cretaceous sequences recovered at Sites 872 through 879 drilled on guyots in the central and western Pacific Ocean during Leg 144. Calcareous plankton biostratigraphy allows us to obtain important biostratigraphic age constraints for the onset, development, and demise of shallow-water sedimentation on these guyots.Site 872 on Lo-En Guyot is the only site at which shallow-water limestones were not recovered during Leg 144. Here, the oldest sediment consists of pelagic limestone infilling fractures within the volcanic substrate. Calcareous plankton biostratigraphy constrains the age of these sediments to Coniacian to earliest Santonian (Dicarinella concavata planktonic foraminifer zone; CC14-CC15 nannofossil zones).On Wodejebato Guyot (Sites 873 through 877), initiation of carbonate platform sedimentation occurred in the late Campanian (CC22 nannofossil Zone), continued during the late Campanian and Maastrichtian, and ended during the late, possibly latest, Maastrichtian. On MIT Guyot (Site 878), calcareous plankton biostratigraphy indicates that the initiation of carbonate platform sedimentation occurred in the earliest Aptian (lower part of the Chiastozygus litterarius nannofossil zone before the "nannoconid crisis"). After a phreato-magmatic eruption that deposited a polymictic breccia, carbonate sedimentation resumed in the middle late Aptian (Nannoconus truittii Acme, Globigerinelloides algerianus to Hedbergella trocoidea planktonic foraminifer zones). Shallow-water deposition ended during the late Albian after the Biticinella breggiensis Zone. Carbonate platform sedimentation at Site 879 on Takuyo-Daisan Guyot began during the middle late Aptian (N. truittii Acme, G. algerianus to H. trocoidea planktonic foraminifer zones) and ended by late Albian time (Rotalipora ticinensis planktonic foraminifer zone). Shallow-water limestone at Site 879 correlates with the upper carbonate platform sequence recovered at Site 878, but its thickness is only half that of the coeval sequence deposited on MIT Guyot, suggesting the presence of hiatuses.

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“…Banner and Desai, 1988 Family Conoglobigerinidae Simmons, BouDagherFadel, Genus Globuligerina Bignot &Guyader, 1971, emend. Simmons, BouDagher-Fadel, Banner and Globuligerina bathoniana (PAZDROWA, 1969) Figure 4.…”

Section: Protoglobigerinids In Isolated Formsmentioning

confidence: 99%

Kimmeridgian protoglobigerinids (Foraminifera) from Crussol (SE France)

Görög

Wernli

2010

Swiss J Geosci

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A detailed investigation of the protoglobigerinids from the Kimmeridgian section of the Montagne de Crussol, SE France is presented. This monotonous succession of predominantly carbonate beds represents periplatform hemipelagic deposits, well dated by ammonites. Three species were determined in thin sections and in isolated forms after extraction by acetolysis. Favusella? parva (KUZNETSOVA) is the most common species occurring in almost the entire succession from the Orthosphinctes to the Beckeri zones. Favusella hoterivica (SUBBOTINA) has been retrieved less frequently from the Platynota to the Beckeri zones, and it is its oldest occurrence. The rare Globuligerina bathoniana (PAZDROWA) occurs only in the Late Kimmeridgian. Based on our study and the review of the literature a palaeogeographical map was plotted, showing that most of the protoglobigerinid occurrences are in deep water facies of the northern margin and central part of the Tethys. These records demonstrate the presence of Globuligerina bathoniana, G. oxfordiana (GRIGELIS), Favusella hoterivica, F.? parva and Compactogerina stellapolaris (GRIGELIS) in the Kimmeridgian.

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A review and revision of the Jurassic-Early Cretaceous Globigerinina, with especial reference to the Aptian assemblages of Speeton (North Yorkshire, England)

Cited by 72 publications

References 32 publications

Planktic Foraminiferal Species Turnover Across Deep-Sea Aptian/ Albian Boundary Sections

Planktic Foraminiferal Species Turnover Across Deep-Sea Aptian/ Albian Boundary Sections

Cretaceous Calcareous Plankton Biostratigraphy of Sites 872 through 879

Kimmeridgian protoglobigerinids (Foraminifera) from Crussol (SE France)

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