Taphocoenoses and diversification patterns of calcimicrobes and calcareous algae, Ordovician, Tarim Basin, China
Despite the crucial role of epibenthic primary producers (cyanobacteria, green and red algae), no diversity curves for calcimicrobes and calcareous algae are available to assess the pyramiding paleoecology characterizing the Ordovician biodiversification episode. A total of 24 taxa of calcimicrobes...
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Published in | Canadian journal of earth sciences Vol. 53; no. 7; pp. 702 - 711 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Ottawa
National Research Council of Canada
01.07.2016
NRC Research Press Canadian Science Publishing NRC Research Press |
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Abstract | Despite the crucial role of epibenthic primary producers (cyanobacteria, green and red algae), no diversity curves for calcimicrobes and calcareous algae are available to assess the pyramiding paleoecology characterizing the Ordovician biodiversification episode. A total of 24 taxa of calcimicrobes and calcareous algae are identified from a Dapingian to lower Katian succession of carbonate sedimentary rocks exposed at the Leyayilitag ridge, Bachu Uplift, Tarim Basin, northwest China. Calcimicrobes (14 taxa), Dasycladales (seven taxa), Bryopsidales (one taxon), and Cyclocrinales (two taxa) contribute to five distinct taphocoenoses characterizing a suite of carbonate mounds. In stratigraphic order, these are calathid sponge mounds, algal calcimicrobial mounds, algal mounds, algal reefs, and calcimicrobial mounds. Within the lower Katian Belodina confluens Zone, the diversity increases substantially from around 5 to more than 20 taxa per 2 Ma. This increase in diversity is based on new calcimicrobes (Bija, Ortonella, Garwoodia, Hedstroemia, Rothpletzella, Phacelophyton, Rauserina) and the diversification of Dasycladales and Cyclocrinales. By comparison, the global diversity of calcimicrobes and calcareous algae (derived from literature data) started to increase earlier, namely within the late Darriwilian Pygodus serra Zone (offset of about 4 Ma). This offset might be due to the peculiar lithology of the Sandbian Tumuxiuke Formation (condensed section of red nodular limestones bounded by disconformities). However, a similar temporal offset is recorded for calathid sponge mounds; therefore, the Tarim tectonic microplate (Tarim Block) might display an endemic-anachronistic character. The diversity curves of Ordovician benthic primary producers (calcimicrobes, calcareous algae) are similar to those recorded by some fossil groups, in particular eleutherozoan echinoderms. |
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AbstractList | Despite the crucial role of epibenthic primary producers (cyanobacteria, green and red algae), no diversity curves for calcimicrobes and calcareous algae are available to assess the pyramiding paleoecology characterizing the Ordovician biodiversification episode. A total of 24 taxa of calcimicrobes and calcareous algae are identified from a Dapingian to lower Katian succession of carbonate sedimentary rocks exposed at the Leyayilitag ridge, Bachu Uplift, Tarim Basin, northwest China. Calcimicrobes (14 taxa), Dasycladales (seven taxa), Bryopsidales (one taxon), and Cyclocrinales (two taxa) contribute to five distinct taphocoenoses characterizing a suite of carbonate mounds. In stratigraphic order, these are calathid sponge mounds, algal calcimicrobial mounds, algal mounds, algal reefs, and calcimicrobial mounds. Within the lower Katian Belodina confluens Zone, the diversity increases substantially from around 5 to more than 20 taxa per 2 Ma. This increase in diversity is based on new calcimicrobes (Bija, Ortonella, Garwoodia, Hedstroemia, Rothpletzella, Phacelophyton, Rauserina) and the diversification of Dasycladales and Cyclocrinales. By comparison, the global diversity of calcimicrobes and calcareous algae (derived from literature data) started to increase earlier, namely within the late Darriwilian Pygodus serra Zone (offset of about 4 Ma). This offset might be due to the peculiar lithology of the Sandbian Tumuxiuke Formation (condensed section of red nodular limestones bounded by disconformities). However, a similar temporal offset is recorded for calathid sponge mounds; therefore, the Tarim tectonic microplate (Tarim Block) might display an endemic-anachronistic character. The diversity curves of Ordovician benthic primary producers (calcimicrobes, calcareous algae) are similar to those recorded by some fossil groups, in particular eleutherozoan echinoderms.Original Abstract: Malgre le role cle des producteurs primaires epibenthiques (cyanobacteries, algues vertes et rouges), aucune courbe de diversite pour les calcimicrobes et les algues calcaires n'est disponible pour evaluer la paleoecologie pyramidale qui caracterise l'episode de biodiversification ordovicienne. Un total de 24 taxons de calcimicrobes et d'algues calcaires sont identifies dans une sequence allant du Dapingien au Katien inferieur de roches sedimentaires carbonatees exposee sur la crete de Leyayilitag, dans la zone de soulevement de Bachu du bassin du Tarim (nord-ouest de la Chine). Des calcimicrobes (14 taxons), dasycladales (sept taxons), bryopsidales (un taxon) et cyclocrinales (deux taxons) font partie de cinq thanatocoenoses distinctes qui caracterisent une suite de monticules carbonates. En ordre stratigraphique, il s'agit de monticules d'eponges calathides, de monticules algaires et calcimicrobiens, des monticules algaires, des recifs algaires et des monticules calcimicrobiens. Dans la zone a Belodina confluens du Katien inferieur, la diversite augmente considerablement d'environ 5 a plus de 20 taxons chaque 2 Ma. Cette augmentation de la diversite repose sur de nouveaux calcimicrobes (Bija, Ortonella, Garwoodia, Hedstroemia, Rothpletzella, Phacelophyton, Rauserina) et la diversification des dasycladales et cyclocrinales. En comparaison, la diversite planetaire des calcimicrobes et des algues calcaires (tiree de donnees publiees) a commence a augmenter plus tot, soit dans la zone a Pygodus serra du Darriwilien tardif (un decalage d'environ 4 Ma). Ce decalage pourrait etre le fait de la lithologie particuliere de la Formation sandbienne de Tumuxiuke (sequence condensee de calcaires nodulaires rouges limites par des discordances erosionnelles). Cependant, un decalage temporel semblable est observe pour des monticules d'eponges cathalides, de sorte que la microplaque tectonique du Tarim (bloc du Tarim) pourrait presenter un caractere endemique-anachronistique. Les courbes de diversite des producteurs primaires benthiques (calcimicrobes et algues calcaires) de l'Ordovicien sont semblables a celles enregistrees par certains groupes de fossiles, en particulier les echinodermes eleutherozoaires. [Traduit par la Redaction] Despite the crucial role of epibenthic primary producers (cyanobacteria, green and red algae), no diversity curves for calcimicrobes and calcareous algae are available to assess the pyramiding paleoecology characterizing the Ordovician biodiversification episode. A total of 24 taxa of calcimicrobes and calcareous algae are identified from a Dapingian to lower Katian succession of carbonate sedimentary rocks exposed at the Leyayilitag ridge, Bachu Uplift, Tarim Basin, northwest China. Calcimicrobes (14 taxa), Dasycladales (seven taxa), Bryopsidales (one taxon), and Cyclocrinales (two taxa) contribute to five distinct taphocoenoses characterizing a suite of carbonate mounds. In stratigraphic order, these are calathid sponge mounds, algal calcimicrobial mounds, algal mounds, algal reefs, and calcimicrobial mounds. Within the lower Katian Belodina confluens Zone, the diversity increases substantially from around 5 to more than 20 taxa per 2 Ma. This increase in diversity is based on new calcimicrobes (Bija, Ortonella, Garwoodia, Hedstroemia, Rothpletzella, Phacelophyton, Rauserina) and the diversification of Dasycladales and Cyclocrinales. By comparison, the global diversity of calcimicrobes and calcareous algae (derived from literature data) started to increase earlier, namely within the late Darriwilian Pygodus serra Zone (offset of about 4 Ma). This offset might be due to the peculiar lithology of the Sandbian Tumuxiuke Formation (condensed section of red nodular limestones bounded by disconformities). However, a similar temporal offset is recorded for calathid sponge mounds; therefore, the Tarim tectonic microplate (Tarim Block) might display an endemic-anachronistic character. The diversity curves of Ordovician benthic primary producers (calcimicrobes, calcareous algae) are similar to those recorded by some fossil groups, in particular eleutherozoan echinoderms. |
Audience | Academic |
Author | Neuweiler, Fritz Shen, Yuefeng |
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SubjectTerms | Algae algal mounds algal structures Analysis Asia Bachu Uplift Basins Biodiversity biogenic structures Bryopsidales Carbonates China Chlorophyceae Chlorophyta Cyanobacteria Cyclocrinales Dasycladaceae Dasycladales Far East floral studies Fossils Geological time Leyayilitag Ridge Lithology lithostratigraphy Maralbexi China Marine algae microfossils morphology Mounds Offsets Ordovician Paleobotany Paleoecology Paleozoic Plantae Rothpletzella Sedimentary geology Sedimentary rocks sedimentary structures Sponges Stratigraphy Tarim Basin Tumuxiuke Formation Xinjiang China |
Title | Taphocoenoses and diversification patterns of calcimicrobes and calcareous algae, Ordovician, Tarim Basin, China |
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