Ediakarano

Panahong Ediakarano
635–635 milyong taon ang nakalilipas

Mean na atmosperikong nilalamang O₂sa loob ng tagal ng panahon

ca. 8 Bolyum %^[1]
(40 % ng modernong lebel)

Mean na atmosperikong nilalamang CO₂ sa tagal ng panahon

ca. 4500 ppm^[2]
(16 mga beses sa lebel na pre industriyal)

−640 —

–

−630 —

–

−620 —

–

−610 —

–

−600 —

–

−590 —

–

−580 —

–

−570 —

–

−560 —

–

−550 —

–

−540 —

–

−530 —

–

−520 —

–

−510 —

–

−500 —

Cryogenian

Ediakarano

Cambrian

←

Huling mga pamayanang Ediakarano

←

Huling putatibong Ediakarano

←

mga embryo?

←

Huling ekstensibong pagyeyelo

←

Unang megafossil na Ediakarano

←

Pagyeyelong
Gaskiers

Mga diskong
Aspidella

Rangeomorphs

Neoproterosoiko

(huling era ng Prekambriyano)

Palæosoiko

(unang era ng Phanerozoic)

Iskalang aksis:Mga milyong taon ang nakalilipas.
References: Waggoner 1998,^[3] Hofmann 1990^[4]

Ang Ediakarano (Ingles: Ediacaran /ˌiːdiˈækərən/) na ipinangalan sa Bulunbundking Ediacara ng Timog Australia ang panahong heolohiko ng era na Neoproterosoiko at ng eon na Proterozoic na na nauna sa panahong Cambrian na unang panahon ng era na Paleozoic at eon na Phanerozoic. Ang katayuan nito bilang isang opisyal na panahong heolohiko ay pinagtibay noong 2004 ng International Union of Geological Sciences (IUGS) na gumagawa ritong unang bagong panahong heolohiko na idineklara sa 120 taon. ^[5]^[6]^[7]

Bagaman ang panahong ito ay hinango mula sa Bulubundking Ediacara kung saan ang unang mga natuklasang fossil ng eponimosong biotang Ediakara ay natuklasan noong 1946 ng heologong si Reg Sprigg, ang uring seksiyon ng stata ay matatagpuan sa kama ng Creek na Enorama ^[8] wsa loob ng Gorge na Brachina ^[9] in the Flinders Ranges of South Australia, at 31°19′53.8″S 138°38′0.1″E / 31.331611°S 138.633361°E / -31.331611; 138.633361.

Mga sanggunian

↑ Image:Sauerstoffgehalt-1000mj.svg
↑ Image:Phanerozoic Carbon Dioxide.png
↑ Waggoner, Ben (1998). "Interpreting the Earliest Metazoan Fossils: What Can We Learn?". Integrative and Comparative Biology. 38 (6): 975–982. doi:10.1093/icb/38.6.975. ISSN 1540-7063. Nakuha noong 2007-03-08.{{cite journal}}: CS1 maint: date auto-translated (link)
↑ Hofmann, H.J.; Narbonne, G.M.; Aitken, J.D. (1990). "Ediacaran remains from intertillite beds in northwestern Canada". Geology. 18 (12): 1199–1202. doi:10.1130/0091-7613(1990)018<1199:ERFIBI>2.3.CO;2.{{cite journal}}: CS1 maint: date auto-translated (link)
↑ A. Knoll, M. Walter, G. Narbonne, and N. Christie-Blick (2004) "The Ediacaran Period: A New Addition to the Geologic Time Scale." Submitted on Behalf of the Terminal Proterozoic Subcommission of the International Commission on Stratigraphy.
↑ Knoll, A. H.; Walter, MR; Narbonne, G. M; Christie-Blick, N (2004). "A new period for the geologic time scale" (PDF). Science. 305 (5684): 621–622. doi:10.1126/science.1098803. PMID 15286353.{{cite journal}}: CS1 maint: date auto-translated (link)
↑ Knoll, A. H.; Walter, M. R.; Narbonne, G. M.; Christie-Blick, N. (2006). "The Ediacaran Period: A new addition to the geologic time scale" (PDF). Lethaia. 39: 13–30. doi:10.1080/00241160500409223. Inarkibo mula sa orihinal (PDF) noong 2007-02-21. Nakuha noong 2012-09-23.{{cite journal}}: CS1 maint: date auto-translated (link)
↑ "Geological time gets a new period: Geologists have added a new period to their official calendar of Earth's history—the first in 120 years". London: BBC. 2004-05-17.{{cite news}}: CS1 maint: date auto-translated (link) Accessed 27 December 2010.
↑ South Australian Museum Newsletter April 2005 Naka-arkibo 2011-02-17 sa Wayback Machine. Accessed 9 August 2010.

[1] Image:Sauerstoffgehalt-1000mj.svg

[2] Image:Phanerozoic Carbon Dioxide.png

[Waggoner1998t-3] Waggoner, Ben (1998). "Interpreting the Earliest Metazoan Fossils: What Can We Learn?". Integrative and Comparative Biology. 38 (6): 975–982. doi:10.1093/icb/38.6.975. ISSN 1540-7063. Nakuha noong 2007-03-08.{{cite journal}}: CS1 maint: date auto-translated (link)

[4] Hofmann, H.J.; Narbonne, G.M.; Aitken, J.D. (1990). "Ediacaran remains from intertillite beds in northwestern Canada". Geology. 18 (12): 1199–1202. doi:10.1130/0091-7613(1990)018<1199:ERFIBI>2.3.CO;2.{{cite journal}}: CS1 maint: date auto-translated (link)

[Knoll2004a-5] A. Knoll, M. Walter, G. Narbonne, and N. Christie-Blick (2004) "The Ediacaran Period: A New Addition to the Geologic Time Scale." Submitted on Behalf of the Terminal Proterozoic Subcommission of the International Commission on Stratigraphy.

[Knoll2004-6] Knoll, A. H.; Walter, MR; Narbonne, G. M; Christie-Blick, N (2004). "A new period for the geologic time scale" (PDF). Science. 305 (5684): 621–622. doi:10.1126/science.1098803. PMID 15286353.{{cite journal}}: CS1 maint: date auto-translated (link)

[Knoll2006-7] Knoll, A. H.; Walter, M. R.; Narbonne, G. M.; Christie-Blick, N. (2006). "The Ediacaran Period: A new addition to the geologic time scale" (PDF). Lethaia. 39: 13–30. doi:10.1080/00241160500409223. Inarkibo mula sa orihinal (PDF) noong 2007-02-21. Nakuha noong 2012-09-23.{{cite journal}}: CS1 maint: date auto-translated (link)

[8] "Geological time gets a new period: Geologists have added a new period to their official calendar of Earth's history—the first in 120 years". London: BBC. 2004-05-17.{{cite news}}: CS1 maint: date auto-translated (link) Accessed 27 December 2010.

[9] South Australian Museum Newsletter April 2005 Naka-arkibo 2011-02-17 sa Wayback Machine. Accessed 9 August 2010.

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