291:
118:
636:
263:
during fossilization. Classification is based on the distinctive two-layer walls and verticils (blind pores) branching outward from the cylindrical body. The organism likely was surrounded by a mucilaginous coating, preserved in fossils as transparent calcite cement. As of 1998, no reproductive
258:
Members of the family took the form of calcareous cylindrical tubes 100 to 400 micrometers (0.0039 to 0.0157 in) in diameter and up to 5 millimeters (0.20 in) in length. The tubes are single or (rarely) paired with an axial canal that is often replaced with clear
480:
Corrochano, Diego; Barba, Pedro; Colmenero, Juan R. (March 2012). "Glacioeustatic cyclicity of a
Pennsylvanian carbonate platform in a foreland basin setting: An example from the Bachende Formation of the Cantabrian Zone (NW Spain)".
512:
Bahamonde, Juan R.; Della Porta, Giovanna; Merino-TomΓ©, Oscar A. (April 2017). "Lateral variability of shallow-water facies and high-frequency cycles in foreland basin carbonate platforms (Pennsylvanian, NW Spain)".
267:
Beresellids became important marine carbonate sediment producers in the middle
Carboniferous, in association with various phylloid algae. They are thought to have favored shallow, sheltered
319:
Choh, Suk-Joo; Kirkland, Brenda L. (1 September 2008). "Sedimentologic role ofin situ
Beresellid algal colonies, Holder Formation (Upper Pennsylvanian), New Mexico, U.S.A.".
677:
582:
414:
433:
Kenrick, Paul; Li, Cheng-Sen (April 1998). "An early, non-calcified, dasycladalean alga from the Lower
Devonian of Yunnan Province, China".
670:
706:
354:
Brenckle, Paul L. (1985). "Cribrokamaena and
Crassikamaena, New Genera of Late Paleozoic Algae from the United States".
117:
711:
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244:
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271:. Local accumulations were sometimes extensive enough to be distinguished as beresellid
635:
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28:
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Elliott, G. F. (1991). "Dasycladalean Algae of the
Palaeozoic and Mesozoic".
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of organisms of uncertain affinity, sometimes placed within the
548:
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and their fossils are found in strata ranging in age from the
235:(multicellular animals), but tentatively assigned to the
651:
264:
structures have been found for members of this group.
557:
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308:
428:
426:
279:, making this a rock-forming family of algae.
671:
8:
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20:
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435:Review of Palaeobotany and Palynology
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650:. You can help Knowledge (XXG) by
399:Calcareous Algae and Stromatolites
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455:10.1016/S0034-6667(97)00050-X
499:10.1016/j.sedgeo.2011.12.009
407:10.1007/978-3-642-52335-9_7
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527:10.1007/s10347-016-0487-3
321:Carbonates and Evaporites
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113:Scientific classification
111:
23:
16:Extinct family of algae
646:-related article is a
609:Paleobiology Database
468:Kenrick & Li 1998
707:Green algae families
491:2012SedG..245...76C
483:Sedimentary Geology
447:1998RPaPa.100...73K
368:1985MiPal..31...55B
297:Paleontology portal
243:. Beresellids were
485:. 245β246: 76β93.
333:10.1007/BF03176154
712:Ulvophyceae stubs
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596:Open Tree of Life
551:Taxon identifiers
416:978-3-642-52337-3
356:Micropaleontology
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441:(1β2): 73β88.
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253:early Permian
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249:late Devonian
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39:428β295
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33:Early Permian
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29:Late Devonian
24:Beresellaceae
22:
19:
702:Dasycladales
652:expanding it
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362:(1): 55β67.
359:
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349:
327:(2): 79β88.
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245:cosmopolitan
241:Dasycladales
220:
219:
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209:Uraloporella
207:
201:
195:
194:
178:
163:Dasycladales
126:
18:
644:Ulvophyceae
401:: 125β130.
273:bafflestone
153:Ulvophyceae
143:Chlorophyta
691:Categories
283:References
237:green alga
139:Division:
574:Q33135305
535:131889753
341:128972150
277:packstone
197:Beresella
165: (?)
568:Wikidata
521:(2): 6.
203:Dvinella
172:Family:
601:4003121
588:4983546
487:Bibcode
443:Bibcode
384:1485580
364:Bibcode
269:lagoons
261:calcite
251:to the
233:Metazoa
226:extinct
189:Genera
159:Order:
149:Class:
614:111107
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515:Facies
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239:order
229:family
224:is an
642:This
531:S2CID
380:JSTOR
337:S2CID
127:Clade
648:stub
583:GBIF
411:ISBN
47:Preκ
523:doi
495:doi
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439:100
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329:doi
275:or
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307:^
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97:Pg
41:Ma
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211:?
176:β
102:N
92:K
87:J
82:T
77:P
72:C
67:D
62:S
57:O
52:κ
36:~
31:-
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