The Early Evolutionary History of Planktonic Foraminifera 1997
DOI: 10.1007/978-94-011-5836-7_2
|View full text |Cite
|
Sign up to set email alerts
|
Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

1
36
0

Year Published

2003
2003
2018
2018

Publication Types

Select...
3
2
1

Relationship

0
6

Authors

Journals

citations
Cited by 22 publications
(37 citation statements)
references
References 0 publications
1
36
0
Order By: Relevance
“…8, 10). Disregarding the height of the trochospire G. bathoniana is strongly related to G. oxfordiana as illustrated by of Pazdrowa (1969), Stam (1986) or Simmons et al (1997).…”
Section: Protoglobigerinids In Isolated Formsmentioning
confidence: 99%
See 1 more Smart Citation
“…8, 10). Disregarding the height of the trochospire G. bathoniana is strongly related to G. oxfordiana as illustrated by of Pazdrowa (1969), Stam (1986) or Simmons et al (1997).…”
Section: Protoglobigerinids In Isolated Formsmentioning
confidence: 99%
“…The diameter is 250-260 lm and the wall surface shows pseudomuricae in discontinuous ridges. Simmons et al (1997) have chosen G. stellapolaris as type species of their new monotypic (Gradstein, 1983, p. 552, pl. 2, figs.…”
Section: Records In Rock Thin Sections In the Literaturementioning
confidence: 99%
“…Planktic foraminifers are morphotaxonomically divided into two groups, Globigerinina and Heterhelicina (Boudagher-Fadel 2013 ), although their taxonomic rank differs in the literature (Order level in Boudagher-Fadel 2013 , Suborders in Simmons et al 1997 , lower than Order in Pawlowski et al 2013 ). The oldest records of planktic Globigerinina are Conoglobigerina avariformis , C. balakhmatovae , C. dagestanica and possibly C. avarcia (Superfamily Favusellaceoidea, Family Conoglobigerinidae) from the upper Bajocian (169-168 Ma: Middle Jurassic) (Simmons et al 1997 ;Boudagher-Fadel 2013 ).…”
Section: Foraminifersmentioning
confidence: 99%
“…The oldest records of planktic Globigerinina are Conoglobigerina avariformis , C. balakhmatovae , C. dagestanica and possibly C. avarcia (Superfamily Favusellaceoidea, Family Conoglobigerinidae) from the upper Bajocian (169-168 Ma: Middle Jurassic) (Simmons et al 1997 ;Boudagher-Fadel 2013 ). Although their most probable ancestors are considered as benthic foraminiferal genera Praegubkinella or Oberhauserella (e.g., Clémence and Hart 2013 ), a missing link in the fossil records is present between the last occurrence of these two benthic foraminifers in the Toarcian (182-174 Ma) and the fi rst occurrence of planktic Conoglobigerina in the upper Bajocian (169-168 Ma) (Simmons et al 1997 ). Hart et al ( 2003 ) suggest that planktic foraminifers evolved from a partially planktic (meroplanktic) form around the Toarcian Anoxic Events (182-174 Ma).…”
Section: Foraminifersmentioning
confidence: 99%
“…Using associated algae, Banner and Simmons (1994) noted that Palorbitolina lenticularis was most common in sediments thought to be deposited at depths of between 10 and 50m. Simmons et al (1997) noted that muddy, orbitolinid-rich beds, with large, flat, orbitolinids seem to be characteristic of transgressive deposits, while more conical forms thrive in the shallowest water. The relationship between orbitolinid shape and palaeobathymetry seems to mimic that observed for Holocene larger foraminifera (e.g.…”
Section: Palaeoecology Of the Cretaceous Larger Foraminiferamentioning
confidence: 99%