Late Cretaceous Diatoms (Bacillariophyta) from the Teshio-Nakagawa Area, Hokkaido, Northern Japan: Significance for Their Origin and Biostratigraphy

Abstract. Well-preserved marine diatoms are documented for the first time from authigenic carbonate rocks induced by cold methane (hydrocarbon) seepage in the Omagari Formation (latest Santonian to earliest Campanian in age, Late Cretaceous Epoch; around 83.6 Ma) of the upper part of the Yezo Group in the Teshio-Nakagawa area, northern Hokkaido (northern Japan). The diatom flora is rich in species of Hemiaulus and Triceratium, associated with a few other extinct diatom genera. An araphid genus (Sceptroneis) was also observed; this is one of the earliest fossil records of “pennate” (Bacillariophyceae) diatoms. Although valve ultrastructures have been mostly dissolved, the preservation of these diatoms is much better than that in the few previous reports of Cretaceous siliceous photosynthetic organisms from Japan and adjacent regions in the northwestern Pacific Ocean. Because of their common generic composition in the mid- to high-latitude regions in both hemispheres, diatoms are suggested to have experienced a global radiation by early Campanian time. Thus, our diatom records provide insights into the Late Cretaceous floral adaptive radiation around the northwestern Pacific margin, where the radiation history of diatoms is yet unclear. As Gladius antiquus was confirmed but Basilicostephanus species were absent from the present material, the flora from the Teshio-Nakagawa area is tentatively regarded as belonging to the G. antiquus Concurrent Range Zone, an interval extending from an undetermined Late Cretaceous Epoch to the latest Santonian Age. However, this floral correlation is inaccurate because our materials are latest Santonian to earliest Campanian in age, as dated by the molluscan (ammonoids and inoceramids) biostratigraphy. Hence, further research is required to clarify the sensitivity of different chronological proxies and the stratigraphic ranges of age-diagnostic diatoms in different geographic provinces.

[1]  R. Jenkins,et al.  Well-preserved diatoms (Bacillariophyta) from the lower Oligocene Nuibetsu Formation in the Urahoro area, eastern Hokkaido , 2016 .

[2]  I. Maruyama,et al.  Early post-mortem formation of carbonate concretions around tusk-shells over week-month timescales , 2015, Scientific Reports.

[3]  T. V. Oreshkina,et al.  Diatoms and silicoflagellates of the Upper Cretaceous from Saratov Region: Biostratigraphy and sedimentation settings , 2013, Stratigraphy and Geological Correlation.

[4]  D. Pirrie,et al.  Carbonate concretions—explained , 2013 .

[5]  M. Yamasaki,et al.  Well-preserved Late Cretaceous diatoms (Bacillariophyta) from the Teshio-Nakagawa area, northern Japan , 2013 .

[6]  C. Shimada,et al.  Two New Extinct Basal Phocoenids (Cetacea, Odontoceti, Delphinoidea), from the Upper Miocene Koetoi Formation of Japan and Their Phylogenetic Significance , 2012 .

[7]  D. Harwood,et al.  Taxonomic composition, paleoecology and biostratigraphy of Late Cretaceous diatoms from Devon Island, Nunavut, Canadian High Arctic , 2011 .

[8]  R. Jenkins,et al.  Carbonate Sediments Microbially Induced by Anaerobic Oxidation of Methane in Hydrocarbon-Seeps , 2011 .

[9]  R. Jenkins,et al.  Gastropods from Late Cretaceous Omagari and Yasukawa Hydrocarbon Seep Deposits in the Nakagawa Area, Hokkaido, Japan , 2009 .

[10]  J. Pike,et al.  Late Cretaceous seasonal ocean variability from the Arctic , 2009, Nature.

[11]  E. Virginia Armbrust,et al.  The life of diatoms in the world's oceans , 2009, Nature.

[12]  R. Jenkins,et al.  Microbially induced formation of ooid‐like coated grains in the Late Cretaceous methane‐seep deposits of the Nakagawa area, Hokkaido, northern Japan , 2008 .

[13]  R. Jenkins,et al.  Methane‐flux‐dependent lateral faunal changes in a Late Cretaceous chemosymbiotic assemblage from the Nakagawa area of Hokkaido, Japan , 2007 .

[14]  R. Majima,et al.  Review of fossil chemosynthetic assemblages in Japan , 2005 .

[15]  A. Ijiri,et al.  An exceptionally well-preserved fossil seep community from the Cretaceous Yezo Group in the Nakagawa area, Hokkaido, northern Japan , 2003 .

[16]  A. Takahashi,et al.  Stratigraphy and fossil assemblage of the Upper Cretaceous in the Teshionakagawa area, Hokkaido, northern Japan. , 2003 .

[17]  R. Crawford,et al.  THE MORPHOLOGY AND TAXONOMY OF THE MARINE CENTRIC DIATOM GENUS PARALIA. II. PARALIA CRENULATA, P. FAUSTA AND THE NEW SPECIES, P. HENDEYI , 2002 .

[18]  D. Harwood,et al.  Upper Cretaceous diatom biostratigraphy of the Arctic archipelago and northern continental margin, Canada , 2002 .

[19]  L. Medlin,et al.  Evolution of the diatoms (Bacillariophyta). IV. A reconstruction of their age from small subunit rRNA coding regions and the fossil record. , 1996, Molecular phylogenetics and evolution.

[20]  S. Toshimitsu Towards an integrated mega-, micro- and magneto-stratigraphy of the Upper Cretaceous in Japan. , 1995 .

[21]  D. L. Clark,et al.  Siliceous microfossils from the warm Late Cretaceous and early Cenozoic Arctic Ocean , 1994, Journal of Paleontology.

[22]  E. Fourtanier Diatom Biostratigraphy of Equatorial Indian Ocean Site 758 , 1991 .

[23]  R. Gersonde,et al.  Lower Cretaceous diatoms from ODP Leg 113 Site 693 (Weddell Sea). Part 1. Vegetative cells , 1990 .

[24]  D. Harwood Upper Cretaceous and lower Paleocene diatom and silicoflagellate biostratigraphy of Seymour Island, eastern Antarctic Peninsula , 1988 .

[25]  G. Hasle,et al.  TWO CRETACEOUS STELLARIMA SPECIES: S. STEINYI AND S. DISTINCTA; THEIR MORPHOLOGY, PALAEOGEOGRAPHY AND PHYLOGENY , 1987 .

[26]  C. Blome,et al.  Carbonate concretions: an ideal sedimentary host for microfossils. , 1985 .

[27]  J. Barron Diatom biostratigraphy of the CESAR 6 core, Alpha Ridge , 1985 .

[28]  S. Blasco,et al.  Initial geological report on CESAR: the Canadian expedition to study the Alpha Ridge, Arctic Ocean , 1985 .

[29]  J. Fenner Eocene-Oligocene planktic diatom stratigraphy in the low latitudes and the high southern latitudes , 1984 .

[30]  D. Soudry,et al.  Siliceous microfossils of the Upper Cretaceous Mishash Formation, Central Negev, Israel , 1983 .

[31]  J. Fenner Cenozoic Diatom Biostratigraphy of the Equatorial and Southern Atlantic Ocean , 1978 .

[32]  N. I. Strelnikova,et al.  Diatom and Radiolarian Cenozoic Stratigraphy, Norwegian Basin; DSDP Leg 38 , 1978 .

[33]  M. Hajós Late Cretaceous Archaeomonadaceae, Diatomaceae, and Silicoflagellata from the South Pacific Ocean, Deep Sea Drilling Project, Leg 29, Site 275 , 1975 .

[34]  T. Kanaya Eocene Diatom Assemblages from the Kellogg and "Sidney" Shales, Mt. Diablo Area, California , 1957 .

[35]  G. D. Hanna Cretaceous diatoms from California , 1927 .

[36]  A. Rothpletz Ueber die Flysch-Fucoiden und einige andere fossile Algen, sowie über liasische, Diatomeen führende Hornschwämme. , 1896 .

[37]  F. Hustedt,et al.  Atlas der Diatomaceen-Kunde , 1874 .