Difference between revisions of "Alveole"

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[[File:Fig 09.jpg|thumb|<font size="2"> '''Fig. 1.''' Alveoles.
 
[[File:Fig 09.jpg|thumb|<font size="2"> '''Fig. 1.''' Alveoles.
  '''A-D''': model (schematic, not to scale) of the genus ''Malatyna'' SIREL, subaxial, subequatorial and tangential sections. Igualada, North-Eastern Spain. Uppermost Middle Eocene. '''E-F''': ''Globoreticulina iranica'' RAHAGHI, tangential and axial sections. Shiraz, Iran. Middle-Upper Eocene. '''G-H''': ''Bullalveolina bulloides'' REICHEL, axial and subequatorial sections. Peribetics, South-Eastern Spain. Lower Oligocene. '''I''': ''Austrotrillina striata'' ADAMS, sections perpendicular to apertural axis and tangential sections. Kirkuk, Iraq. Oligocene. '''J-K''': ''Everticyclammina virguliana'' (KOECHLIN), equatorial sections. Mechra Klila, North-Eastern Morocco, Uppermost Jurassic. All sections transmitted light micrographs.
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  '''A-D''': model (schematic, not to scale) of the genus ''Malatyna'' Sirel, subaxial, subequatorial and tangential sections. Igualada, North-Eastern Spain. Uppermost Middle Eocene. '''E-F''': ''Globoreticulina iranica'' Rahaghi, tangential and axial sections. Shiraz, Iran. Middle-Upper Eocene. '''G-H''': ''Bullalveolina bulloides'' Reichel, axial and subequatorial sections. Peribetics, South-Eastern Spain. Lower Oligocene. '''I''': ''Austrotrillina striata'' Adams, sections perpendicular to apertural axis and tangential sections. Kirkuk, Iraq. Oligocene. '''J-K''': ''Everticyclammina virguliana'' (Koechlin), equatorial sections. Mechra Klila, North-Eastern Morocco, Uppermost Jurassic. All sections transmitted light micrographs.
'''a''': (main) [[aperture]]; '''al''': alveole; '''bl''': basal layer; '''f''': (main) [[foramen]]; ''pr'': [[proloculus]]; '''prp''': [[preseptal passage]] (in these cases extending over most of the [[chamber lumen]]); '''s''': [[septum]]; '''sa''': [[supplementary aperture]]; '''sl''': septular ridges (incomplete septula).(Hottinger, 2006; fig. 9 [http://paleopolis.rediris.es/cg/CG2006_M02/index.html] with permission from the author).]]
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'''a''': (main) [[aperture]]; '''al''': alveole; '''bl''': basal layer; '''f''': (main) [[foramen]]; ''pr'': [[proloculus]]; '''prp''': [[preseptal passage]] (in these cases extending over most of the [[chamber lumen]]); '''s''': [[septum]]; '''sa''': [[supplementary aperture]]; '''sl''': septular ridges (incomplete septula); (Hottinger, 2006; fig. 9 [http://paleopolis.rediris.es/cg/CG2006_M02/index.html] '''CC'''/BY-NC-SA)]]
  
 
==Definition==
 
==Definition==
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''Remarks'': The term alveole is used here exclusively for exoskeletal structures, i.e. for subepidermal, tiny compartments of the chamber cavity coated by an organic lining. Alveoles are supposedly filled with chamber plasm. Alveoles must be distinguished from paraporous or parakeriothecal cavities that are an adjunct of wall texture. Like true [[pores]], these cavities are (by definititon) neither filled with living chamber plasm nor coated by the [[organic lining]]. The simultaneous presence of both alveolar structures and keriothecal wall texture in the fusulinid ''Verbeekina'' and its relatives, the combination of an alveolar exoskeleton with a paraporous external wall in ''Dicyclina'' or with a bilamellar perforate wall in ''Fabiania'' supports a consequent restriction of the term's use to exoskeletal structures, never to textures.  
 
''Remarks'': The term alveole is used here exclusively for exoskeletal structures, i.e. for subepidermal, tiny compartments of the chamber cavity coated by an organic lining. Alveoles are supposedly filled with chamber plasm. Alveoles must be distinguished from paraporous or parakeriothecal cavities that are an adjunct of wall texture. Like true [[pores]], these cavities are (by definititon) neither filled with living chamber plasm nor coated by the [[organic lining]]. The simultaneous presence of both alveolar structures and keriothecal wall texture in the fusulinid ''Verbeekina'' and its relatives, the combination of an alveolar exoskeleton with a paraporous external wall in ''Dicyclina'' or with a bilamellar perforate wall in ''Fabiania'' supports a consequent restriction of the term's use to exoskeletal structures, never to textures.  
Layers of alveoles coating the lateral chamber wall are present in various agglutinated groups of which ''Cyclammina'' is the most prominent while ''Everticyclammina'' is an early extinct representative of an exoskeletal layer of exclusively undivided, shallow alveoles. The Neogene group of ''Textulariella'' CUSHMAN (GRÖNHAGEN & LUTERBACHER, 1966) has branching alveoles. Among the porcelaneous foraminifera with alveoles, ''Austrotrillina'' is a prominent group. In this genus, species with deep and branching alveoles - ''A. howchini'' (SCHLUMBERGER) - are said to evolve from earlier forms with layers of shallow, undivided alveoles (ADAMS, 1968). The term alveole is also used for rows of blind recesses in postseptal position over supplementary apertures in the previous septal face as in ''Subalveolina'' or ''Bullalveolina''. We do not yet know, how to interpret (in terms of exo- or endoskeletal elements) these alveoles nor what might be their biological meaning.
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Layers of alveoles coating the lateral chamber wall are present in various agglutinated groups of which ''Cyclammina'' is the most prominent while ''Everticyclammina'' is an early extinct representative of an exoskeletal layer of exclusively undivided, shallow alveoles. The Neogene group of ''Textulariella'' Cushman (Grönhagen & Luterbacher, 1966) has branching alveoles. Among the porcelaneous foraminifera with alveoles, ''Austrotrillina'' is a prominent group. In this genus, species with deep and branching alveoles - ''A. howchini'' (Schlumberger) - are said to evolve from earlier forms with layers of shallow, undivided alveoles (Adams, 1968). The term alveole is also used for rows of blind recesses in postseptal position over supplementary apertures in the previous septal face as in ''Subalveolina'' or ''Bullalveolina''. We do not yet know, how to interpret (in terms of exo- or endoskeletal elements) these alveoles nor what might be their biological meaning.
  
  
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==References==
 
==References==
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Adams (1968), A revision of the foraminiferal genus Austrotrillina PARR.- Bulletin of the British Museum (Natural History), London, (Geology series), vol. 16, N° 2, p. 71-97.
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Grönhagen  & Luterbacher  (1966), Beobachtungen an den Foraminiferen-Gattungen Pseudotextulariella und Textulariella sowie verwandten Formen. Eclogae geologicae Helvetiae, Basel, vol. 59, N° 1, p. 235-246.
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Hottinger (2006), [http://paleopolis.rediris.es/cg/CG2006_M02/index.html Illustrated glossary of terms used in foraminiferal research]. [http://paleopolis.rediris.es/cg/uk-index.html Carnets de Géologie], [http://paleopolis.rediris.es/cg/CG2006_M02/index.html Memoir 2], ISSN 1634-0744                                       
 
Hottinger (2006), [http://paleopolis.rediris.es/cg/CG2006_M02/index.html Illustrated glossary of terms used in foraminiferal research]. [http://paleopolis.rediris.es/cg/uk-index.html Carnets de Géologie], [http://paleopolis.rediris.es/cg/CG2006_M02/index.html Memoir 2], ISSN 1634-0744                                       
 
                      
 
                      
 
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Latest revision as of 09:48, 1 April 2019