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Benthic foraminiferal fauna and sediment provenance of Eocene syn-rift sequences in Taiwan: implication for onset of Asian epi-continental marginal seas off China coast

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Abstract

Early Cenozoic rift basins developed commonly on the Mesozoic basement along the SE Asia Continent. However, Eocene–Oligocene sequences were only exposed widely onshore Taiwan. We study benthic foraminifera and determine U–Pb geochronology of detrital zircon grains in the Early Cenozoic sequence onshore Taiwan for understanding if there was any significant change in faunal content and sediment provenance between the Eocene syn-rift sequences and the overlying Oligocene post-rift strata across the breakup unconformity. The Eocene syn-rift sequences are mostly of thick, cross-bedded sandstones of fluvial-deltaic depositions without marine fauna. Intensive study on the Eocene stratigraphy in more than ten sections all over the Taiwan mountain belt in the last three decades, shallow marine benthic foraminifera of Gaudryina hayasakai-Hanzawaia asterizana-Planularia okinoshimaensis-Heterolepa praecinta assemblage were found only in very limited exposures in the Western Foothills, central Taiwan. This study shows that the Eocene benthic foraminiferal assemblage is similar to the Shihtsaoan fauna in the overlying Oligocene post-rift marine strata. This indicates no significant faunal break across the breakup unconformity. As a consequence, Gaudryina hayasakai Zone of the Shihtsaoan age can extend downward to the Eocene and the Shihtsaoan Stage would be equivalent to the Hsuehshanian Stage established previously from northern Taiwan. The Taiwan Eocene marine sequences could be deposited in a normal-fault bounded narrow seaway or gulf connecting southeastward to the open Huatung Basin. U–Pb geochronology of detrital zircons in the Taiwan Eocene syn-rift sandstones shows a prominent age peak centered in Yenshanian (100–155 Ma) similar to the Paleocene–Oligocene fluvial-deltaic deposits in the East China Sea and is also comparable to the U–Pb zircon age spectrum of modern river sands of the Fujian Province, SE China. Petrographic study also suggests a prevailing sediment provenance of the Cathaysia granites and volcanics. These Cathaysia detritals were transported to the Taiwan Eocene grabens through some SE-flowing rivers. Structural reconstructions in previous study indicated that the mountain belt with the Eocene sequences in NE Taiwan had been shortened by imbricated thrusting westward for 160–200 km wide during the arc-continent collision in the last 6.5 Ma. Integrating paleontology and sedimentology evidence reveal that the Eocene coast was located along the modern shelf break of the East China Sea ~ 350–400 km east off the modern Chinese coast line. This implies that in the Eocene time (~ 40 Ma) there was no wide Asian epi-continental marginal seas off Chinese coast until the onset sedimentation of the Oligocene post-rift strata during opening of the South China Sea in the Early Oligocene time (~ 33 Ma).

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References

  • CAGS Research Party of Marine Geology (1989) Cenozoic paleobiota of the continental shelf of the East China Sea (Donghai): Paleozological, vol 1. Ministry of geology and Mineral Resources Institute of Geology Chinese Academy of Geological Science, Beijing, pp 6–136

    Google Scholar 

  • Chang LS (1960) Tertiary biostratigraphy of Taiwan with special reference to smaller foraminifera and its bearing on the Tertiary geohistory of Taiwan. Proc Geol Soc China 3:7–30

    Google Scholar 

  • Chang LS (1962a) A biostratigraphic study of the Oligocene in northern Taiwan based on smaller foraminifera. Proc Geol Soc China 5:47–64

    Google Scholar 

  • Chang LS (1962b) Some planktonic foraminifera from the Suo and Urai Groups of Taiwan and their stratigraphic significance. Proc Geol Soc China 5:127–133

    Google Scholar 

  • Chang LS (1963) A biostratigraphic study of the so-called Hori Slate in central Taiwan based on smaller foraminifera. Proc Geol Soc China 6:3–17

    Google Scholar 

  • Chang LS (1967) Tertiary biostratigraphy of Taiwan and its correlation. In: Kotora H (ed) Tertiary correlation and climatic changes in the Pacific. Sadaki Printing and Publishing Co. Ltd, Sendai, pp 57–65

    Google Scholar 

  • Chang LS (1972) Eocene/Miocene hiatus and N Conglomerate in the Central Range of Taiwan. Proc Geol Soc China 15:93–98

    Google Scholar 

  • Chang LS (1973) A biostratigraphic study of the so-called Slate Formation in Taiwan based on smaller foraminifera: III. Sankuang-Hsiuluan area along the upper courses of the Tanshuho and the Yulochi. Proc Geol Soc China 16:69–84

    Google Scholar 

  • Chang LS (1975) Biostratigraphy of Taiwan. Geol Paleontol Southeast Asia 15:337–361

    Google Scholar 

  • Chen MM, Yu NT, Chu HT, Shea KS, Hsieh YC (2009) Larger foraminifera in the so-called “Meichi Sandstone” of Wujie area, southern Hsuehshan Range. Central Geol Surv 22:227–242

    Google Scholar 

  • Chi WR (1979) Discussion on biohorizon of the Tsukeng Formation in the Nantou area. Chin Pet Co Explor Dev Res Bull 2:21–40 (in Chinese)

    Google Scholar 

  • Chiu HT (1972) Miocene stratigraphy of the Nantou area, central Taiwan. Pet Geol Taiwan 10:159–177

    Google Scholar 

  • Chiu HT (1975) Miocene stratigraphy and its relation to the Paleogene rocks in western-central Taiwan. Pet Geol Taiwan 12:51–80

    Google Scholar 

  • Chou JT (1988) Eocene formations in Taiwan. Pet Geol Taiwan 24:51–59

    Google Scholar 

  • Deschamps A, Monié P, Lallemand S, Hsu SK, Yeh KY (2000) Evidence for early Cretaceous oceanic crust trapped in the Philippine Sea Plate. Earth Planet Sci Lett 179:503–516

    Article  Google Scholar 

  • Folk RL (1974) Petrology of sedimentary rocks, vol 159. Hemphill Publ Co, Austin

    Google Scholar 

  • Fong CCK, Huang T, Shea KS (1994) New occurrence of larger foraminifera in northern Taiwan and its stratigraphic significance. Central Geol Surv 8:205–212

    Google Scholar 

  • Fu X, Zhu W, Chen C, Zhong K, Xu CH (2006) Detrital zircon provenance of the Upper Mingyuefeng Formation in the west slope of Lishui-Jiaojiang Sag, East China Sea Earth Science. J China Univ Geosci 40:1988–2001 (in Chinese)

    Google Scholar 

  • Hayasaka I, Tan K (1939) On the occurrence of Lepidocyclina (s.s.) in Taiwan (Formosa) with the description of species by Shoshiro Hanzawa. Imp Acad Tokyo Proc 5:182–185

    Article  Google Scholar 

  • Hohenegger J (2011) Lager foraminifera: greenhouse constructions and gardeners in the ocean microcosm. The Kagoshima University Museum, Kagoshima, p 81

    Google Scholar 

  • Hsiao PT, Lin KA, Lo SZ, Hsu SH, Chi WR, Huang ST, Shen JC, Chiu JH, Wang HJ (1991) Petroleum appraisal on Tungyintao Basin. Pet Geol Taiwan 26:183–213

    Google Scholar 

  • Huang TC (1977) Calcareous nannoplankton stratigraphy of the Upper Wulai Group (Oligocene) in northern Taiwan. Pet Geol Taiwan 14:147–179

    Google Scholar 

  • Huang TC (1978) Calcareous nannofossils of the subsurface Pre-Miocene rocks in the Peikang basement high and adjacent area in western central Taiwan (part I: Cretaceous). Pet Geol Taiwan 15:49–87

    Google Scholar 

  • Huang TC (1980) Calcareous nannofossils from the Slate terrane west of Yakou, Southern Cross-Island Highway. Pet Geol Taiwan 17:59–74

    Google Scholar 

  • Huang CY (1984) Late Oligocene benthic foraminiferal assemblages in northern Taiwan. In: the 2nd international symposium on Benthic Foraminifera, Pau, France, pp 317–323

  • Huang CY (1986) Oligocene and Miocene stratigraphy of the Kuohsing area, central Taiwan. Acta Geol Taiwan 24:281–318

    Google Scholar 

  • Huang CY (1989) Implication of the Post-Lushanian faunal change for the occurrence of Kuroshio Current in the early late Miocene: foraminiferal evidence from the Chuhuangkeng section, norther. Proc Geol Soc China 32:21–45

    Google Scholar 

  • Huang CY (1990) Upper Miocene stratigraphy and the horizon of Post-Lushanian faunal turnover in northeastern Taiwan. Proc Geol Soc China 33:303–328

    Google Scholar 

  • Huang TC, Chi WR (1979) Calcareous nannofossils of the subsurface Pre-Miocene rocks from the Peikang basement high and adjacent areas in western central Taiwan (part II: Paleocene). Pet Geol Taiwan 16:96–129

    Google Scholar 

  • Huang CY, Masuda K, Wu LC (1990) Miocene Pelecypoda in the Western Foothills of northern Taiwan (part I: stratigraphy, faunal occurrences and paleoceanographic significances). Bull Natl Mus Nat Sci 2:119–139

    Google Scholar 

  • Huang CY, Wu WY, Chang CP, Tsao S, Yuan PB, Lin CW, Xia KY (1997) Tectonic evolution of accretionary prism in the arc-continent collision terrane of Taiwan. Tectonophysics 281:31–51

    Article  Google Scholar 

  • Huang CY, Yuan PB, Tsao SJ (2006) Temporal-spatial records of active arc-continent collision in Taiwan: a synthesis. Geol Soc Am Bull 118:274–288. https://doi.org/10.1130/B25527.1

    Article  Google Scholar 

  • Huang CY, Yen Y, Zhao Q, Lin CT (2012) Cenozoic stratigraphy of Taiwan: window into rifting, stratigraphy and paleoceanography of South China Sea. Chin Sci Bull 57:3130–3149

    Article  Google Scholar 

  • Huang CY, Yen Y, Liew PM, He DJ, Chi WR, Wu MS, Zhao M (2013a) Significance of indigenous Eocene larger foraminifera Discocyclina dispansa in Western Foothills, Central Taiwan: a Paleogene marine rift basin in Chinese continental margin. J Asian Earth Sci 62:425–437

    Article  Google Scholar 

  • Huang CY, Chi WR, Yan Y, Yang KM, Liew PM, Wu MS, Wu JC, Zhang C (2013b) The first record of Eocene tuff in a Paleogene rift basin near Nantou, Western Foothills, central Taiwan. J Asian Earth Sci 69:3–16

    Article  Google Scholar 

  • Huang CY, Shea KH, Li Q (2017) A foraminiferal study on Middle Eocene-Oligocene break-up unconformity in northern Taiwan and its correlation with IODP Site U1435 to constrain the onset of South China Sea opening. J Asian Earth Sci 138:439–465

    Article  Google Scholar 

  • Kanno S, Chung CT (1973) Molluscan fauna from the so-called Paleogene formations in northern Taiwan. Geol Paleontol Southeast Asia 13:91–127

    Google Scholar 

  • Kanno S, Chung CT (1975) Tertiary formations and their molluscan faunas from the Central Range and Foothills areas of northern Taiwan. Geol Paleontol Southeast Asia 15:363–391

    Google Scholar 

  • Kennett JP, Keller G, Srinivasan MS (1985) Miocene planktonic foraminiferal biogeography and paleoceanographic development of the Indo-pacific region. Geol Soc Am Mem 163:197–236

    Google Scholar 

  • Lan Q, Yan Y, Huang CY, Clift PD, Li X, Chen W, Zhang X, Yu M (2014) Tectonics, topography, and river system transition in East Tibet: insights from the sedimentary record in Taiwan. Geochem Geophys Geosyst 15:3658–3674. https://doi.org/10.1002/2014GC005310

    Article  Google Scholar 

  • Lee CT, Wang Y (1985) Stratigraphy and structure of the slate terrane near Likuan, Southern Cross-Island Highway, Taiwan Ti-Chi. Geology 6:1–20 (in Chinese)

    Google Scholar 

  • Li XH (1997) Timing of the Cathaysia block formation: constraint from SHRIMP U-Pb zircon geochronology. Episode 20:188–192

    Google Scholar 

  • Li CF, Xu X, Lin J, Sun Z, Zhu J, Yao Y, Zhao Liu Q, Kulhanek D, Wang J, Song T, Zhao J, Qiu N, Guan Y, Zhou Z, Expedition 349 Scientists (2014) Ages and magnetic structures of the South China Sea basin constrained by deep to magnetic surveys and IODP Expedition 349. Geoch Geophy Geosys 15:4958–4983. https://doi.org/10.1002/2014GC005567

    Article  Google Scholar 

  • Li Q, Wu GX, Zhang L, Shu Y, Shao L (2016) Paleogene marine deposition records of rifting and breakup of the South China Sea: an overview. Sci China Earth Sci. https://doi.org/10.1007/s1143o-016-0163-x

    Google Scholar 

  • Lin AT, Watts AB, Hesselbo SP (2003) Cenozoic stratigraphy and subsidence history of the South China Sea margin in the Taiwan region. Basin Res 15:453–478. https://doi.org/10.1046/j.1365-2117.2003.00215.x

    Article  Google Scholar 

  • Lue YT (1983) Some consideration on the molluscan fauna in the Lungtung-Aoti section. Bull Inst Earth Sci Acad Sinica 3:201–208

    Google Scholar 

  • Masuda K, Huang CY (1990) Miocene Pelecypoda in the Western Foothills of northern Taiwan (part II: systematic description). Bull Natl Mus Nat Sci 2:141–189

    Google Scholar 

  • Masuda K, Huang CY (1994) Tertiary and Quaternary Pectinidae from northern Taiwan. J Geol Soc China 37:497–548

    Google Scholar 

  • Matsumoto T, Hayami I, Hashimoto W (1965) Some molluscan fossils from the buried Cretaceous of western Taiwan. Pet Geol Taiwan 4:1–24

    Google Scholar 

  • Miller KG, Wright JD, Katz ME, Wade BS, Browning JV, Cramer BS, Rosenthal Y (2009) Climate threshold at the Eocene-Oligocene transition: Antarctic ice influence on ocean circulation. Geol Soc Am Spec Pap 452:169–178. https://doi.org/10.1130/2009.2452(11)

    Google Scholar 

  • Pang X, Chen CM, Shi HS (2007) The Pearl river deep-water fan system and petroleum in South China Sea. Science Press, Beijing, pp 1–266

    Google Scholar 

  • Ren J, Niu B, Wang J, Jin X, Zhao L, Liu R (2013) Advances in research of Asian geology—a summary of 1:5 M International Geological Map of Asia Project

  • Shao L, Cao L, Qiao P, Zhang X, Li Q, Hinsbergen D (2017) Cretaceous–Eocene provenance connections between the Palawan Continental Terrane and the northern South China Sea margin. Earth Planet Sci Lett 477:97–107. https://doi.org/10.1016/j.epsl.2017.08.019

    Article  Google Scholar 

  • Sun SC (1982) The Tertiary basins of offshore Taiwan. In: Proceedings of the 2nd ASCOPE Conference and Exhibition Manila Philippines, pp 125–135

  • Sun X, Wang P (2005) How old is the Asian monsoon system—Paleobontanical records from China. Paleogeogr Paleoclimatol Paleoecol 232:181–232

    Article  Google Scholar 

  • Suppe J (1980) A retrodeformable cross section of northern Taiwan. Proc Geol Soc China 23:46–55

    Google Scholar 

  • Tan K (1944) Contemporaneity of the formations of the Urai Series, especially of the Yonryo Sandstone, the Hakurei Formation and the Niitaka Formation (I). Trans Nat Hist Soc Formosa 34:48–249

    Google Scholar 

  • Taylor B, Hayes DE (1983) Origin and history of the South China Sea. In: Hayes DE (ed) The Tectonic and Geologic evolution of Southeast Asian Seas and Islands (Part 2), Geophysical Monograph Series, vol 27. AGU, Washington DC, pp 23–56

    Chapter  Google Scholar 

  • Wan YS, Liu DY, Xu MH, Zhang JM, Song B, Shi YR, Du LL (2007) SHRIMP U-Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks in northwestern Fujian, Cathaysia Block, China: tectonic implications and the need to redefine lithostratigraphic units. Gondwana Res 12:166–183. https://doi.org/10.1016/j.gr.2006.10.016

    Article  Google Scholar 

  • Wang P, Li Q, Li CF (2014) Geology of the China Seas. Developments in Marine Geology, vol 6. Elsevier, Amsterdam

    Google Scholar 

  • Wong J, Sun M, Xing G, Li XH, Zhao G, Wong K, Yuan C, Xia X, Li L, Wu F (2009) Geochemical and zircon U-Pb and Hf isotopic study of the Baijuajian metaluminous A-type granite: extension at 125–100 Ma and its tectonic significance for south China. Lithos 112:289–305

    Article  Google Scholar 

  • Xu XS, O’Reilly SY, Griffin WL, Wang XL, Pearson NJ (2007) The crust of Cathaysia: age, assembly and reworking of two terranes. Precambr Res 158:51–78. https://doi.org/10.1016/j.precamres.2007.04.010

    Article  Google Scholar 

  • Xu Y, Sun Q, Yi L, Yin X, Wang A, Li Y, Chen J (2014) Detrital zircons U-Pb age and Hf isotope from the western side of the Taiwan Strait: implications for sediment provenance and crustal evolution of the northeast Cathaysia block. Terr Atmos Ocean Sci 25:505–535. https://doi.org/10.3319/TAO.2014.02.18.01(TT)

    Article  Google Scholar 

  • Yang X, Li A, Qin Y, Wu S, Wu Z, Zhang J (2006) U-Pb dating of zircons from Cenozoic sandstone: constrain on the geodynamic setting of East China Sea shelf basin. Mar Geol Quat Geol 26:75–85

    Google Scholar 

  • Yen TP (1973) The Eocene sandstones in the Hsüehshan Range Terrain, northern Taiwan. Proc Geol Soc China 16:97–110

    Google Scholar 

  • Zachos J, Pagami M, Stoan L, Thomas E, Billups K (2001) Trends, rhythms, and aberrations in global climate 65 Ma to present. Science 292:686–693

    Article  Google Scholar 

  • Zhou H, Xiao L, Dong Y, Wang C, Wang F, Ni P (2009) Geochemical and geochronological study of the Sanshui basin bimodal volcanic rock suite, China: implications for basin dynamics in southeastern China. J Asian Earth Sci 34:178–189

    Article  Google Scholar 

  • Zhu W (2009) Paleolimnology and source rock studies of Cenozoic hydrocarbon-bearing offshore basins in China. Geological Publishing House, Beijing, pp 1–237

    Google Scholar 

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Acknowledgements

This study was supported by Grants from the National Natural Science Foundation of China (U1505231, 41472093, 91528301) and from the Guangzhou Marine Geological Survey, China (DD20160138-01, 20161972) to C.Y. Huang and the Fundamental Research Funds for the Central Universities to L Shao.

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Authors and Affiliations

  1. State Key Laboratory of Marine Geology, Tongji University, Shanghai, 200092, China

    Chi-Yue Huang, Lei Shao, Pei-Jun Qiao, Yu-Chi Cui & Yuan-Li Hou

  2. Department of Earth Sciences, National Cheng Kung University, 701, Tainan, Taiwan

    Chi-Yue Huang

  3. Exploration and Development Research Institute, Chinese Petroleum Corporation, 36042, Miaoli, Taiwan

    Ming-Huei Wang

  4. Fujian Institute of Geological Survey, Fuzhou, 350013, Fujian, China

    Wei-Guang Xue

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  1. Chi-Yue Huang
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Huang, CY., Shao, L., Wang, MH. et al. Benthic foraminiferal fauna and sediment provenance of Eocene syn-rift sequences in Taiwan: implication for onset of Asian epi-continental marginal seas off China coast. Mar Geophys Res 40, 111–127 (2019). https://doi.org/10.1007/s11001-018-9366-3

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