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Silicified microfossils from the Ediacaran Doushantuo Formation along a shelf margin-slope-basin transect in Hunan Province, South China, with stratigraphical implications

Part of: Memoirs

Published online by Cambridge University Press:  24 February 2025

Qing Ouyang*
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China , , , , , State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (Wuhan), Wuhan 430074, China
Chuanming Zhou
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China , , , , , University of Chinese Academy of Sciences, Nanjing, Nanjing 211135, China
Shuhai Xiao
Affiliation:
Department of Geosciences, Virginia Tech, Blacksburg, VA 24061, USA
Chengxi Wu
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China , , , , , University of Chinese Academy of Sciences, Beijing 100049, China
Zhe Chen
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China , , , , ,
Xianguo Lang
Affiliation:
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, and Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
Hongyi Shi
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China , , , , , University of Chinese Academy of Sciences, Beijing 100049, China
Yunpeng Sun
Affiliation:
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China , , , , , University of Chinese Academy of Sciences, Beijing 100049, China
*
*Corresponding author

Abstract

Silicified microfossils are reported from nine stratigraphic sections of the Ediacaran Doushantuo Formation deposited in shelf margin, slope, and basin environments in Hunan Province of South China. These microfossils include sphaeromorphic and acanthomorphic acritarchs (15 genera and 29 species, including three new acanthomorph species, Bullatosphaera? colliformis n. sp., Eotylotopalla inflata n. sp., and Verrucosphaera? undulata n. sp.), multicellular algae, tubular microfossils, and other problematic forms, representing major fossil groups similar to those from the Doushantuo Formation in more proximal facies (e.g., inner shelf and shelf lagoon). A database of the abundance and occurrences of Doushantuo acanthomorphs is assembled and analyzed using quantitative and data-visualization methods (e.g., rarefaction analysis, non-parametric multidimensional scaling, and network analysis). The results show that, at the genus and species levels, taxonomic richness of Doushantuo acanthomorphs exhibits considerable variation among facies, but this variation is largely due to sampling and taphonomic biases. The results also show that numerous acanthomorph taxa have broad facies distribution, affirming their biostratigraphic value. The analysis confirms that acanthomorphs in the Weng'an biota of shelf margin facies are composed of a mixture of Member II and Member III assemblages of shelf-lagoon facies in the Yangtze Gorges area. The study shows the biostratigraphic potential of acanthomorphs in the establishment of regional biozones using the first appearance datum of widely distributed taxa, highlighting the importance of continuing exploration of under-sampled Doushantuo sections in slope and basinal facies.

UUID: http://zoobank.org/6fc92858-4054-4117-8043-1f06cfe77155

Information

Type
Memoir
Copyright
Copyright © The Author(s), 2025. Published by Cambridge University Press on behalf of Paleontological Society
Figure 0

Figure 1. Ediacaran paleogeography and Proterozoic outcrop distribution in Hunan Province of South China. (1) Paleogeographic map of the Yangtze block during deposition of the Doushantuo Formation (modified from Jiang et al., 2011). Rectangle frame marks the location of (2). (2) Simplified geological map (modified from Luo et al., 2002) showing the distribution of Proterozoic strata in northern Hunan Province where the studied sections are located. Section abbreviations: CJB, Caojunba; LJYZ, Lujiayuanzi; HP, Heping; TP, Tianping; CW, Caowan; SDP, Siduping; MJD, Majindong; LHK, Lianghekou; JSC, Jinshichong.

Figure 1

Figure 2. (1) Lithostratigraphic sequence of the Doushantuo Formation at studied localities, acanthomorph-bearing sampling horizons, and their correlations with those in the Yangtze Gorges area (represented by the Jiulongwan section). Lithostratigraphic column and C-isotopic profile of the Jiulongwan section modified from McFadden et al. (2008). (2) Generalized paleobathymetric profile showing location of Doushantuo Formation sections known to be fossiliferous. Horizontal distances and water depth are not to scale.

Figure 2

Figure 3. Outcrop photos of the Doushantuo Formation at the studied sections. (1) Olistostrome containing breccia (arrowheads) in shales of the lower Member II at Siduping section. (2) Chert nodules from the lower Member II at Siduping section (sample 19SDP-2). (3) Chert nodules (arrowheads) from the lower Doushantuo Formation at Tianping section (sample 19TP-1). (4) Olistostrome from the lower Doushantuo Formation at Tianping section. (5) Chert nodules (arrowheads) from shales of the lower Doushantuo Formation at Caowan section (sample 19CW-8). (6) A chert nodule (arrowheads) from the middle Doushantuo Formation at Lianghekou section (sample 21LHK-1). (7) Stratigraphic sequence of Nantuo Formation diamictite, basal Doushantuo Formation cap dolostone, and lower Doushantuo Formation calcareous shale and mudstone at Majindong section.

Figure 3

Table 1. Sample number, stratigraphic height, number for thin sections, and microfossil abundance data of the Doushantuo Formation from the nine studied sections in Hunan Province. Refer to Figure 2 for stratigraphic height measurements. Refer to Geological setting section for GPS coordinates of the sections. PN = present, not counted; \ = not observed.

Figure 4

Figure 4. Appendisphaera grandis Moczydłowska, Vidal, and Rudavskaya, 1993, emend. Moczydłowska, 2005. (1, 2) PB201998, thin section 18JSC-2-5, U40/4; circled 2 in (1) marks area magnified in (2). (3, 4) PB201999, thin section 19HP-1-33, N41/1; circled 4 in (3) marks area magnified in (4). (5, 6) PB202000, thin section 19TP-1-19, D49/4; circled 6 in (5) marks area magnified in (6). (7–9) PB202001, thin section 19SDP-2-d1, Y24/1; circled 8 and 9 in (7) mark areas magnified in (8) and (9), respectively. (10, 11) PB202002, thin section 21DC-5-4, V34/1; circled 11 in (10) marks area magnified in (11).

Figure 5

Figure 5. Appendisphaera magnifica (Zhang et al., 1998) Liu et al., 2014a. (1) PB202003, thin section 19SDP-7-1, N38/3. (2) PB202004, thin section 19SDP-7-3, E39/2. (3) PB202005, thin section 19SDP-7-3, E30/2. (4) PB202006, thin section 19SDP-7-3, K30/2. (5) PB202007, thin section 19SDP-7-24, H37. (6) PB202008, thin section 19SDP-7-24, H34.

Figure 6

Figure 6. Appendisphaera tenuis Moczydłowska, Vidal, and Rudavskaya, 1993, emend. Moczydłowska, 2005. (1, 2) PB202009, thin section 19TP-1-14, J27; circled 2 in (1) marks area magnified in (2). (3–5) PB202010, thin section 19TP-1-39, J47/1; circled 4 and 5 in (3) mark areas magnified in (4) and (5), respectively. (6–8) PB202011, thin section 19TP-1-40, F37; circled 7 and 8 in (6) mark areas magnified in (7) and (8), respectively.

Figure 7

Figure 7. Asterocapsoides wenganensis (Chen and Liu, 1986) Xiao et al., 2014. (1, 2) PB202012, thin section 21LHK-1-10, R34/4. (1) and (2) show the same area at different focal levels; red arrowheads denote large conical processes.

Figure 8

Figure 8. Bullatosphaera? colliformis new species. Red arrowheads denote basally constricted spherical or hemispherical ornamentations. (1–6) Holotype, PB202013, thin section 19CW-6-2, K30/3; circled 2, 3, and 6 in (1) mark areas magnified in (2, 3, 6), respectively; circled 4 in (1) marks areas in (4, 5), which show the same area at different focal levels. (7–10, 13) PB202014, thin section 19CW-6-12, L31/4. (7, 8) Show the same area at different focal levels; circled 9 in (7) marks area magnified in (9); circled 10 and 13 in (8) mark areas magnified in (10) and (13), respectively. (11, 12, 14) PB202015, thin section 19CW-9-7, O35/4; circled 12 and 14 in (11) mark areas magnified in (12) and (14), respectively. Scale bars in (3) and (6) also apply to (2, 4, 5); scale bars in (9) and (12) also apply to (10, 13, 14).

Figure 9

Figure 9. Sketch of Bullatosphaera? colliformis new species.

Figure 10

Figure 10. (1) Cavaspina acuminata (Kolosova, 1991) Moczydłowska, Vidal, and Rudavskaya, 1993, PB202016, thin section 21DC-3-1, Q30/4. (2) Cavaspina basiconica Moczydłowska, Vidal, and Rudavskaya, 1993, PB202017, thin section 21DC-5-4, M40/1. (3, 4) Cavaspina uria (Nagovitsin and Faizullin in Nagovitsin et al., 2004) Nagovitsin and Moczydłowska in Moczydłowska and Nagovitsin, 2012, thin section 21DC-5-4; red arrowheads in (1–4) denote conical processes; (3) PB202018, G41/1; (4) PB202019, E45/4. (5–7) Eotylotopalla sp. PB202025, thin section 19CW-6-15, O41/1, showing the same area at different focal levels. Scale bars in (5) and (7) also apply to (6).

Figure 11

Figure 11. (1–4, 7, 8) Eotylotopalla dactylos Zhang et al., 1998. (1) PB202020, thin section 19TP-1-13; (2) PB202021 (left) and PB202022 (right), thin section 21DC-2-38, Q48; (3, 4) PB202023, thin section 14HA-115-1, D47/3, showing the same area at different focal levels; (7, 8) PB202024, thin section 21DC-5-3, Q30/3, showing the same area at different focal levels. (5, 6, 9–12) Eotylotopalla cf. E. dactylos Zhang et al., 1998, PB202026, thin section 21DC-2-12, O21/4. (5, 6) The same area at different focal levels; (9–12) magnified views of the processes denoted by circled 9–12 in (6) under cross-polarized light; red arrowheads denote the angular transition from the side wall of the processes to the distal end.

Figure 12

Figure 12. Morphological comparisons between Eotylotopalla specimens described here, published Eotylotopalla dactylos, and specimens identified as Eotylotopalla sp. by Liu et al. (2014a) and by Ye et al. (2022) but reassigned to Eotylotopalla dactylos in this study. Symbols with black outline represent specimens described in this study. Note that two of the three specimens published as Eotylotopalla sp. (Liu et al., 2014a, fig. 31.10, 31.11, and Ye et al., 2022, fig. 23H–J) are very poorly preserved thus their process density (number of processes per 100 μm of vesicle periphery) is unmeasurable.

Figure 13

Figure 13. Eotylotopalla inflata new species. (1–4) Holotype, PB202027, thin section 19TP-1-38, N30/3, showing the same area at different focal levels.

Figure 14

Figure 14. Hocosphaeridium anozos (Willman in Willman and Moczydłowska, 2008) Xiao et al., 2014; red arrowheads denote hooked process terminations. (1–5) PB202028, thin section 21DC-2-20, R20/2; circled 2–5 in (1) mark areas magnified in (2–5), respectively; scale bars in (3) and (5) also apply to (2) and (4). (6–8) PB202029, thin section 21DC-2-20, P18/2; circled 7 and 8 in (6) mark areas magnified in (7) and (8), respectively; scale bar in (8) also applies to (7). (9–11) PB202030, thin section 21DC-2-20, R21; circled 10 and 11 in (9) mark areas magnified in (10) and (11), respectively. (12–14) PB202031, thin section 21DC-2-20, O18/3; circled 13 and 14 in (12) mark areas magnified in (13) and (14), respectively.

Figure 15

Figure 15. Hocosphaeridium scaberfacium Zang in Zang and Walter, 1992, emend. Liu et al., 2014a; red arrowheads denote hooked process terminations. (1–3) PB202032, thin section 19HP-1-28, Q33; circled 2 and 3 in (1) mark the same area magnified in (2) and (3), respectively, at different focal levels to show different processes. (4–6) PB202033, thin section 19TP-1-40, K44; circled 5 and 6 in (4) mark areas magnified in (5) and (6), respectively. (7, 8) PB202034, thin section 19CW-6-15, N40/4; circled 8 in (7) marks the area magnified in (8). (9) PB202035, thin section 19SDP-7-3, G41/1. (10–12) PB202036, thin section 21DC-2-20, P18; circled 11 and 12 in (10) mark areas magnified in (11) and (12), respectively.

Figure 16

Figure 16. Knollisphaeridium maximum (Yin, 1987) Willman and Moczydłowska, 2008, emend. Liu and Moczydłowska, 2019. (1–3) PB202037, thin section 14HA-140-1, S53/4; circled 2 and 3 in (1) mark areas magnified in (2) and (3), respectively. (4, 6) PB202038, thin section 14HA-140-3, E28/4; circled 6 in (4) marks the area magnified in (6). (5, 7, 8) PB202039, thin section 21DC-6-9, H34; circled 7 and 8 in (5) mark areas magnified in (7) and (8), respectively; scale bar in (7) also applies to (8); red and blue arrowheads in (7) denote undeformed and slightly deformed processes, respectively.

Figure 17

Figure 17. (1) Megasphaera inornata Chen and Liu, 1986, emend. Xiao et al., 2014; PB202040, thin section 19SDP-1-13, K42/2. (2) Megasphaera ornata Xiao and Knoll, 2000, emend. Xiao et al., 2014; PB202041, thin section 19SDP-1-22, P39/2; red arrowhead denotes the outer surface of the sculptured vesicle wall.

Figure 18

Figure 18. (1–3) Mengeosphaera bellula Liu et al., 2014a, PB202042, thin section 19CW-6-12, K33; circled 2 and 3 in (1) mark areas magnified in (2) and (3), respectively. (4–8) Mengeosphaera constricta Liu et al., 2014a, PB202043, thin section 14HA-115-2, W43/2; circled 5 in (4) marks the same area magnified in (5) and (6) at different focal levels; circled 7 and 8 in (4) mark areas magnified in (7) and (8), respectively. (9–14) Mengeosphaera gracilis Liu et al., 2014a. (9, 10, 12) PB202044, thin section 19TP-1-12, H43/1; circled 10 and 12 in (9) mark areas magnified in (10) and (12), respectively; (11, 13, 14) PB202045, thin section 19CW-6-15, G36; circled 13 and 14 in (11) mark areas magnified in (13) and (14), respectively. Scale bar in (8) represents 5 μm and applies to (5–7); scale bar in (14) applies to (13).

Figure 19

Figure 19. (1, 2) Mengeosphaera latibasis Liu et al., 2014a, emend. Liu and Moczydłowska, 2019, PB202046, thin section 14HA-115-1, T49/4; circled 2 in (1) marks the area magnified in (2). (3) Mengeosphaera minima Liu et al., 2014a, PB202047, thin section 21DC-5-4, T31/2. (4) Mengeosphaera minima? PB202048, thin section 21DC-3-1, G23/3. (5–11) Mengeosphaera mamma Ye et al., 2022. (5–7) PB202049, thin section 21LHK-1-10, L38/1; circled 6 and 7 in (5) mark areas magnified in (6) and (7), respectively; (8, 10) PB202050, thin section 21MJD-1-10, L45; circled 10 in (8) marks the area magnified in (10); (9, 11) PB202051, thin section 21MJD-1-11, L33; circled 11 in (9) marks the area magnified in (11). Red arrowheads in (2), (5–7), (10), and (11) denote reflection points of biform processes; red arrowheads in (4) denote the basally joined, strongly inflated processes.

Figure 20

Figure 20. (1, 2) Tanarium cf. T. capitatum Liu and Moczydłowska, 2019, PB202052, thin section 21DC-2-35, M32/1, showing the same area at different focal levels. (3, 5) Tanarium conoideum Kolosova, 1991, emend. Moczydłowska, Vidal, and Rudavskaya, 1993, PB202053, thin section 21DC-5-4, R43/3, showing the same area at different focal levels. (4, 6, 7) Tanarium paucispinosum Grey, 2005: (4) PB202054, thin section 19CW-6-9, N35/3; (6, 7) PB202055, thin section 19CW-5-29, H38, showing the same area at different focal levels.

Figure 21

Figure 21. Tanarium pilosiusculum Vorob'eva, Sergeev, and Knoll, 2009. (1–4) PB202056, thin section 19CW-6-15, O41; circled 2–4 in (1) mark areas magnified in (2–4), respectively; (5–7) PB202057, thin section 21LHK-1-10, M31/2; circled 6 and 7 in (5) mark areas magnified in (6) and (7), respectively.

Figure 22

Figure 22. (1–3) Tanarium triangulare (Liu et al., 2014a) Liu and Moczydłowska, 2019: (1, 2) PB202058, thin section 14HA-140-5, F24/1, same area at different focal levels; (3) PB202059, thin section 14HA-140-3, D31/1. (4) Tanarium tuberosum Moczydłowska, Vidal, and Rudavskaya, 1993, PB202060, thin section 21DC-4-11, U45. Red arrowheads in (1) and (2) denote typical conical basal part of some processes.

Figure 23

Figure 23. Tianzhushania spinosa Yin and Li, 1978, emend. Yin in Yin and Liu, 1988. (1–6) PB202061, thin section 21LHK-1-10, O41/4; circled 2 and 6 in (1) mark the areas magnified in (2) and (6), respectively; circled 3 in (2) marks the area magnified in (3); circled 4 in (2) marks the same area magnified in (4) and (5) at different focal levels. Red arrowheads denote hollow cylindrical processes embedded in multilaminate membrane; blue arrowheads denote poorly preserved multilaminate membrane.

Figure 24

Figure 24. Trachyhystrichosphaera? sp. (1–8) PB202062, thin section 19CW-6-16, M40/3; circled 2–5 and 8 in (1) mark areas magnified in (2–5) and (8), respectively; circled 6 in (1) marks the same area magnified in (6) and (7) at different focal levels to show different processes. Scale bar in (5) also applies to (2–4, 6–8). Red arrowheads denote cylindrical processes, yellow arrowheads denote conical processes, blue arrowheads denote outer membrane.

Figure 25

Figure 25. Urasphaera fungiformis Liu et al., 2014a. (1–3) PB202063, thin section 14HA-115-1, N50; circled 2 in (1) marks the same area magnified in (2) and (3) at different focal levels to show different processes.

Figure 26

Figure 26. Verrucosphaera? undulata new species. (1–5) Holotype, PB202064, thin section 21DC-6-1, H44; circled 2 in (1) marks the same area magnified in (2) and (3) at different focal levels to show different processes; circled 4 in (1) marks the same area magnified in (4) and (5) at different focal levels to show different processes; (6–8) PB202065, thin section 21DC-5-4, S47; circled 7 and 8 in (6) mark areas magnified in (7) and (8), respectively. Red arrowheads denote thin cylindrical processes on top of thick conical processes.

Figure 27

Figure 27. Verrucosphaera? undulata new species. (1–4) PB202066, thin section 21DC-5-4, P41/2; circled 2–4 in (1) mark areas magnified in (2–4), respectively; (5–7) PB202067, thin section 21DC-5-4, T32/4; circled 6 and 7 in (5) mark areas magnified in (6) and (7), respectively; (8–10) PB202068, thin section 21DC-5-4, L43/3; circled 9 and 10 in (8) mark areas magnified in (9) and (10), respectively. Red arrowheads denote thin cylindrical processes on top of thick conical processes.

Figure 28

Figure 28. Sketch of Verrucosphaera? undulata new species.

Figure 29

Figure 29. Weissiella cf. W. grandistella. (1–7) PB202069, thin section 21DC-2-30, T35; circled 2–4 in (1) mark areas magnified in (2–4), respectively; red arrowheads denote cross-walls in the processes; (5–7) cross-polarized light microscopic photographs of (1); circled 6 in (2) and circled 7 in (3) showing areas in (6) and (7), respectively; recrystallized micro-quartz indicated by yellow arrowheads; scale bar in (6) also applies to (7).

Figure 30

Figure 30. Recrystallized micro-quartz in chert nodules. (1, 3) A poorly preserved microfossil under plane- (1) and cross- (3) polarized light, showing recrystallized micro-quartz up to 7 μm in size (yellow arrowheads); thin section 19TP-1-39. (2) A well-preserved microfossil under cross-polarized light, showing recrystallized micro-quartz in various sizes (yellow arrowheads); thin section 21DC-5-3. (4) A poorly preserved microfossil under cross-polarized light, with the vesicle interior filled with sightly recrystallized chalcedony (red arrowhead), vesicle wall destroyed by three large calcite crystals, and extra-vesicle matrix filled with micro-quartz in various sizes (yellow arrowheads); thin section 19TP-1-25.

Figure 31

Table 2. Summary of acanthomorph occurrence and abundance data at the nine studied sections. Each occurrence is denoted by fossiliferous sample name and number of specimens. For example, “21DC-4, 1” means one acanthomorph specimen recovered from the sample 21DC-4. Notes for superscripts: (1) Identified as Cavaspina cf. C. basiconica by Shi et al. (2022). (2) Identified as ?Verrucosphaera sp. by Shi et al. (2022). (3) Identified as Appendisphaera fragilis by Ouyang et al. (2017). (4) Identified as ?Cavaspina basiconica by Ouyang et al. (2017). (5) Identified as indeterminate acanthomorph by Ouyang et al. (2017). (6) Identified as Mengeosphaera spicata by Ouyang et al. (2017). (7) Identified as Mengeosphaera latibasis? by Ouyang et al. (2017). (8) Identified as Mengeosphaera chadianensis, Mengeosphaera sp. indet., and M.? cuspidata by Ouyang et al. (2017).

Figure 32

Figure 31. Indeterminate acanthomorphs. (1) PB202070, thin section 19SDP-1-5, O23/4. (2) PB202071, thin section 19SDP-7-3, J28. (3) PB202072, thin section 19CW-5-21, K39. (4) PB202073, thin section 21LHK-1-2, P35. Red arrowheads denote processes.

Figure 33

Figure 32. Sphaeromorphic acritarchs. (1) PB202074, thin section 21LHK-1-6, E42. (2) PB202075, thin section 19HP-1-20, O33/3. (3) PB202076, thin section 19CW-5-30, Q36/3. (4) PB202077, thin section 19TP-1-26, B40.

Figure 34

Figure 33. Multicellular algae. (1, 2) Wengania minuta Xiao, 2004b, PB202078, thin section 19SDP-1-19, N41/4, showing the same area at different focal levels. (3–5, 7) Unnamed thalli with large cells; (3–5) PB202079, thin section 19SDP-1-19, M35; (7) PB202081, thin section 19SDP-1-25, K42/3. (6) Unnamed multicellular thallus, PB202080, thin section 19CW-6-15, M41.

Figure 35

Figure 34. Tubular microfossils. (1) Quadratitubus orbigoniatus Xue, Tang, and Yu, 1992, emend. Liu et al., 2008, PB202082, thin section 19CW-6-13, M44/3. (2) Possible Quadratitubus orbigoniatus, PB202083, thin section 21DC-2-36, L40/2. (3, 4) Sinocyclocyclicus guizhouensis Xue, Tang, and Yu, 1992, emend. Liu et al., 2008; (3) PB202084, thin section 19SDP-7-3, J37/2; (4) PB202085, thin section 21MJD-1-10, K36/3.

Figure 36

Figure 35. Microbial mats consist of filamentous microfossils. (1) A small fragment of Siphonophycus mat, PB202086, thin section 21MJD-1-3, K32/2. (2, 4) Mat with thin filaments interwoven into spherical structures, PB202087, thin section 19CW-6-9, L38; circled 4 in (2) marks the area magnified in (4). (3) Microbial mat consists of various filamentous microfossils including Siphonophycus Schopf, 1968, emend. Knoll et al., 1991, and Salome Knoll, 1982, PB202088, thin section 18JSC-2-3, H34/4. (5, 6) Microbial mat consisting of filamentous microfossils of various sizes; (5) PB202089, thin section 19CW-6-6; (6) PB202090, thin section 19SDP-7-19, Q36.

Figure 37

Figure 36. Filamentous and coccoidal microfossils. (1) Obruchevella minor Zhang, 1984a, PB202091, thin section 18JSC-2-4, T22/2. (2) Salome svalbardense Knoll, 1982, PB202092, thin section 21LHK-1-6, J38. (3, 4) Salome hubeiensis Zhang, 1986: (3) PB202093, thin section 19TP-1-40, J33/3, (4) PB202094, thin section 19CW-6-14, J36/2. (5) Bundled filaments resembling Polytrichoides Hermann, 1974, emend. Hermann in Timofeev et al., 1976, PB202095, thin section 19HP-2-6, M40. (6) Septate trichome with cells much wider than length resembling Oscillatoriopsis Schopf, 1968, emend. Butterfield et al., 1994, PB202096, thin section 19HP-2-3, Q38/3. (7, 8) Aggregated coccoids resembling Myxococcoides Schopf, 1968: (7) PB202097, thin section 21LHK-1-10, Q43/2; (8) PB202098, thin section 21LHK-1-10, N48/3.

Figure 38

Figure 37. Microbial mat preserved as reworked clasts. (1, 2) PB202099, thin section 21LHK-1-15, N42/2; circled 2 in (1) mark the area magnified in (2); (3) PB202100, thin section 19SDP-7-22, F38/2; (4) PB202101, thin section 21LHK-1-3, O44.

Figure 39

Figure 38. Problematic microfossils. (1–4) Microfossil with branching filaments, PB202102, thin section 19SDP-3-14, H34/3, same area at different focal levels to show different branches and bifurcations; red arrowheads denote bifurcations. (5, 6) Polybessurus sp. (5) PB202103, thin section 21MJD-1-13, P37/2; (6) PB202104, thin section 19TP-1-25, M39/4.

Figure 40

Table 3. Paleoenvironmental distribution of reported acanthomorphic acritarchs from the Doushantuo Formation in South China. Numbers in each cell refer to data sources, as detailed below. Hashtag sign (#) indicates that the reported specimen was mistakenly assigned to Briareus vasformis Liu and Moczydłowska, 2019, by Ouyang et al. (2021), and should be B. robustus Liu and Moczydłowska, 2019. Data sources shown in the table: (1) This study. (2) Yin and Li, 1978. (3) Awramik et al., 1985. (4) Chen and Liu, 1986. (5) Yin, 1987. (6) Yin and Liu, 1988. (7) Yin, 1990. (8) Yin et al., 1990. (9) Yin and Xue, 1993. (10) Yuan et al., 1993. (11) Xue et al., 1995. (12) Yin, 1996. (13) Yuan and Hofmann, 1998. (14) Zhang et al., 1998. (15) Xiao and Knoll, 1999. (16) Yin, 1999. (17) Xiao and Knoll, 2000. (18) Yin, 2001. (19) Yin et al., 2001. (20) Zhou et al., 2001. (21) Zhou et al., 2002. (22) Yin et al., 2003. (23) Xiao, 2004b. (24) Yin et al., 2004. (25) Zhou et al., 2004b. (26) Liu and Yin, 2005. (27) Xiao et al., 2007. (28) Yin et al., 2007. (29) Zhou et al., 2007. (30) Xie et al., 2008. (31) Liu et al., 2009. (32) McFadden et al., 2009. (33) Yin et al., 2009a. (34) Yin et al., 2009b. (35) Chen et al., 2010. (36) C. Yin et al., 2011. (37) L. Yin et al., 2011. (38) Liu et al., 2012. (39) Wang et al., 2012. (40) Liu et al., 2013. (41) Zeng et al., 2013. (42) Liu et al., 2014a. (43) Liu et al., 2014b. (44) Xiao et al., 2014. (45) Ouyang et al., 2015. (46) Ye et al., 2015. (47) Hawkins et al., 2017. (48) Nie et al., 2017. (49) Liu and Moczydłowska, 2019. (50) Ouyang et al., 2019. (51) Shang et al., 2019. (52) Shang and Liu, 2020. (53) Yang et al., 2020. (54) Liu et al., 2021. (55) Ouyang et al., 2021. (56) Ye et al., 2022.

Figure 41

Figure 39. Comparison of acanthomorph diversity among different depositional facies at species and genus levels.

Figure 42

Figure 40. Rarefaction analysis of Doushantuo acanthomorphs. (1) Rarefaction curves with 1σ error bars of Doushantuo acanthomorph assemblages published with abundance data from 10 sections in inner shelf, shelf-lagoon, and slope facies. (2) Magnification of gray box in bottom-left of (1), showing rarefied species richness with subsampled size of 1–40 specimens. Sample sizes of Lianghekou section and basinal facies sections are small, therefore they were not rarefied. Rather, observed specimen number and species richness are plotted for Lianghekou section and pooled basinal facies data.

Figure 43

Figure 41. Taxonomic ordination plots based on NMDS analysis of taxonomically updated occurrence data from 82 collections of Doushantuo acanthomorphs in South China (see Supplemental Materials for data). (1) NMDS scatter plots and convex hulls differentiated by depositional facies. (2) NMDS scatter plots and convex hulls differentiated by depositional facies and stratigraphic intervals. (3) Species loading diagram. Note that some species are not labeled because of the limited space; see Supplemental Materials for loading data. Red and green circled points represent eponymous species of the lower and upper biozones of the Doushantuo Formation (Liu et al., 2013, 2014b; Xiao et al., 2014), respectively. Blue filled points represent eponymous species of the biozones of Liu and Moczydłowska (2019). See Figure 42 for abbreviations.

Figure 44

Figure 42. Bipartite network analysis of the same dataset of Doushantuo acanthomorph occurrences used in NMDS analysis (Fig. 41; see Supplemental Materials for data). Lettered nodes represent acritarch species. Numbered and colored nodes represent collections, with numbers matching source reference numbers in Table 3, and colors matching those of Figure 41.2: red = Member II of the Doushantuo Formation, shelf lagoon; green = Member III of the Doushantuo Formation, shelf lagoon; gray = stratigraphic interval not specified, shelf lagoon; yellow = correlated with upper Member II in shelf-lagoon facies, inner shelf (the Zhangcunping and Shennongjia areas); light blue = stratigraphic correlation relationship unclear, inner shelf (other areas such as Baokang, Chadian, and Chaoyang); orange = correlated with upper Member II or Member II–III transitional interval in shelf-lagoon facies, shelf margin (the Weng'an area); olive = roughly correlated with Member III in shelf-lagoon facies, shelf margin (the Caojunba section); lime, Doushantuo Formation, upper slope (the Lujiayuanzi section); blue = correlated with Member II in shelf-lagoon facies, slope (the Zhangjiajie area); dark blue = basinal facies. Each species is linked to a collection by a straight line if the species is present in the collection. Each acritarch taxon is linked to collections in which it is present. The network shows variation in occurrence frequency among acritarch species of the Doushantuo Formation. Species in the central area of the network generally occur in a greater number of areas, stratigraphic intervals, or studies, than species in the periphery area of the network. Abbreviations: CY-Changyang area, YG-Yangtze Gorges area. Species abbreviations: Alm = Alicesphaeridium medusoidum; Anm = Ancorosphaeridium magnum; Ani = Annularidens inconditus; Apob = Apodastoides basileus; Apa = Appendisphaera anguina; Apc1 = Appendisphaera clava; Apc2 = Appendisphaera clustera; Apf = Appendisphaera fragilis; Apg = Appendisphaera grandis; Aph1 = Appendisphaera heliaca; Apl1 = Appendisphaera lemniscata; Apl2 = Appendisphaera longispina; Apl3 = Appendisphaera longitubularis; Apm = Appendisphaera magnifica; Aps = Appendisphaera setosa; Apt1 = Appendisphaera tabifica; Apt2 = Appendisphaera tenuis; Apb = Appendisphaera? brevispina; Aph2 = Appendisphaera? hemisphaerica; Assd = Asseserium diversum; Assf = Asseserium fusulentum; Astf = Asterocapsoides fluctuensis; Astr = Asterocapsoides robustus; Asts = Asterocapsoides sinensis; Astw = Asterocapsoides wenganensis; Bab = Bacatisphaera baokangensis; Bas = Bacatisphaera sparga; Bip = Bispinosphaera peregrina; Biv = Bispinosphaera vacua; Brb = Briareus borealis; Brr = Briareus robustus; Brv = Briareus vasformis; Buc = Bullatosphaera? colliformis n. sp.; Calx = Calyxia xandaros; Caa = Cavaspina acumincata; Cab = Cavaspina basiconica; Cac = Cavaspina conica; Cau = Cavaspina uria; Cavc = Caveasphaera costata; Ceg = Ceratosphaeridium glaberosum; Crc = Crassimembrana crispans; Crm = Crassimembrana multitunica; Crip = Crinita paucispinosa; Cyf = Cymatiosphaeroides forabilatus; Cyk = Cymatiosphaeroides kullingii; Cyy = Cymatiosphaeroides yinii; Dici = Dicrospinasphaera improcera; Dicv = Dicrospinasphaera virgata; Dicz = Dicrospinasphaera zhangii; Disj = Distosphaera jinguadunensis; Diss = Distosphaera speciosa; Disc = Distosphaera? corniculata; Dub = Duospinosphaera biformis; Dus = Duospinosphaera shennongjiaensis; Eoa = Eotylotopalla apophysa; Eoda = Eotylotopalla dactylos; Eode = Eotylotopalla delicata; Eoi = Eotylotopalla inflata n. sp.; Eoq = Eotylotopalla quadrata; Eos = Eotylotopalla strobilata; Erc = Ericiasphaera crispa; Erd = Ericiasphaera densispina; Erf = Ericiasphaera fibrilla; Erm = Ericiasphaera magna; Err = Ericiasphaera rigida; Ers1 = Ericiasphaera sparsa; Ers2 = Ericiasphaera spjeldnaesii; Esg = Estrella greyae; Esr = Estrella recta; Gyp = Gyalosphaeridium pulchrum; Hew = Helicoforamina wenganica; Hoa = Hocosphaeridium anozos; Hod = Hocosphaeridium dilatatum; Hos = Hocosphaeridium scaberfacium; Knb = Knollisphaeridium bifurcatum; Knc = Knollisphaeridium coniformum; Knd = Knollisphaeridium denticulatum; Knl = Knollisphaeridium longilatum; Knm = Knollisphaeridium maximum; Kno = Knollisphaeridium obtusum; Knp = Knollisphaeridium parvum; Knt = Knollisphaeridium triangulum; Lac = Laminasphaera capillata; Mac = Matosphaera changyangensis; Megc = Megasphaera cymbala; Megi = Megasphaera inornata; Mego = Megasphaera ornata; Megp1 = Megasphaera patella; Megp2 = Megasphaera puncticulosa; Memf = Membranosphaera formosa; Mea = Mengeosphaera angusta; Meb = Mengeosphaera bellula; Mech = Mengeosphaera chadianensis; Meco = Mengeosphaera constricta; Mee = Mengeosphaera eccentrica; Mef = Mengeosphaera flammelata; Meg1 = Mengeosphaera gracilis; Meg2 = Mengeosphaera grandispina; Mela = Mengeosphaera latibasis; Melu = Mengeosphaera lunula; Mem1 = Mengeosphaera mamma; Mem2 = Mengeosphaera matryoshkaformis; Mem3 = Mengeosphaera membranifera; Mem4 = Mengeosphaera minima; Mer = Mengeosphaera reticulata; Mesp = Mengeosphaera spinula; Mest = Mengeosphaera stegosauriformis; Meu = Mengeosphaera uniformis; Mup = Multifronsphaeridium pelorium; Mur = Multifronsphaeridium ramosum; Pab = Papillomembrana boletiformis; Pac = Papillomembrana compta; Poc = Polygonium cratum; Sia = Sinosphaera asteriformis; Sie = Sinosphaera exilis; Sir = Sinosphaera rupina; Sis = Sinosphaera speciosa; Siv = Sinosphaera variabilis; Spb = Spiralicellula bulbifera; Tael = Taedigerasphaera lappacea; Taa = Tanarium acus; Tac1 = Tanarium capitatum; Tac2 = Tanarium columnatum; Tac3 = Tanarium conoideum; Tac4 = Tanarium cuspisatum; Tad = Tanarium digitiforme; Tae = Tanarium elegans; Tag = Tanarium gracilentum; Tai = Tanarium irregulare; Tami = Tanarium minimum; Tamu = Tanarium muntense; Tao = Tanarium obesum; Tap1 = Tanarium paucispinosum; Tap2 = Tanarium pilosiusculum; Tap3 = Tanarium pluriprotensum; Tap4 = Tanarium pycnacanthum; Tatr = Tanarium triangulare; Tatu = Tanarium tuberosum; Tau = Tanarium uniformum; Tava = Tanarium varium; Tavi = Tanarium victor; Tip = Tianzhushania polysiphonia; Tir = Tianzhushania rara; Tis = Tianzhushania spinosa; Scz = Schizofusa zangwenlongii; Urc = Urasphaera capitalis; Urf = Urasphaera fungiformis; Urn = Urasphaera nupta; Vaf = Variomargosphaeridium floridum; Vag = Variomargosphaeridium gracile; Val = Variomargosphaeridium litoschum; Vav = Variomargosphaeridium varietatum; Vem = Verrucosphaera minima; Veu = Verrucosphaera? undulata n. sp.; Web = Weissiella brevis; Wec = Weissiella concentrica; Weg = Weissiella cf. W. grandistella; Xel = Xenosphaera liantuoensis; Yit = Yinitianzhushania tuberifera; Yur = Yushengia ramispinsa.

Figure 45

Table 4. Occurrence of eponymous species of the two previously proposed biozonation schemes for the Doushantuo Formation in South China. Abbreviations for biozones: A1 = Tianzhushania spinosa zone of Liu et al. (2013, 2014a) and Xiao et al. (2014), corresponding to Member II in the Yangtze Gorges area; A2 = Hocosphaeridium anozos Zone (or the Tanarium conoideum–Hocosphaeridium scaberfacium–H. anozos Zone) of Liu et al. (2013, 2014a) and Xiao et al. (2014), corresponding to Member III in the Yangtze Gorges area; B1 = Appendisphaera grandis–Weissiella grandistella–Tianzhushania spinosa Zone of Liu and Moczydłowska (2019), corresponding to lowermost Member II in the Yangtze Gorges area; B2 = Tanarium tuberosum–Schizofusa zangwenlongii Zone of Liu and Moczydłowska (2019), corresponding to lower–middle Member II in the Yangtze Gorges area; B3 = Tanarium conoideum–Cavaspina basiconica Zone of Liu and Moczydłowska (2019), corresponding to middle–upper Member II in the Yangtze Gorges area; B4 = Tanarium pycnacanthum–Ceratosphaeridium glaberosum Zone of Liu and Moczydłowska (2019), corresponding to lower Member III in the Yangtze Gorges area.