Palynological and sedimentary analysis of the Igarape Ipiranga and Querru 1 outcrops of the Itapecuru Formation (Lower Cretaceous, Parnaiba Basin), Brazil

被引:15
作者
Ferreira, Neila N. [1 ]
Ferreira, Elizabete P. [2 ]
Ramos, Renato R. C. [3 ]
Carvalho, Ismar S. [1 ]
机构
[1] Univ Fed Rio de Janeiro, Inst Geociencias, Ave Athos Silveira Ramos,274,Ilha Fundao, BR-21910200 Rio De Janeiro, RJ, Brazil
[2] Petrobras Cenpes, Rua Horacio Macedo,950,Ilha Fundao,Predio 32, BR-21941915 Rio De Janeiro, RJ, Brazil
[3] Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, Sao Cristovao S-N, BR-20940040 Rio De Janeiro, RJ, Brazil
关键词
Lower Cretaceous; Parnaiba Basin; Itapecuru Formation; Maranhao State; Palynology; ACRITARCHS; EGYPT; WELL; USA;
D O I
10.1016/j.jsames.2015.12.005
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The siliciclastic sediments of the Itapecuru Formation occur in a large area of the Parnaiba Basin and its deposits crop out along the Itapecuru River, in Maranhao State, northern Brazil. The palynological analysis of the Igarape Ipiranga and Querru 1 outcrops strata yields a rich and diversified data. The presence of index-palynofloras in assemblages allows the identification of the Complicatisaccus cearensis Zone, of Late Aptian-Early Albian age. Terrestrial palynomorphs are abundant in the assemblages, being represented by bryophytes and pteridophytes, especially perisporate trilete spores (Crybelosporites and Perotrilites), and gymnosperms and angiosperms (Afropollis and Elaterosporites). The composition of palynological assemblages suggests the presence of moist soils for both outcrops. Acritarchs were recovered in the Querru 1 outcrop, which suggest a marine setting supporting a tidal flat environment indicated by facies associations. Furthermore, reworked Paleozoic palynomorphs were observed in the Querru 1 outcrop. The microflora from Igarape Ipiranga outcrop suggests terrestrial environment corroborating with floodplain environment indicated by facies association. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:15 / 31
页数:17
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共 83 条
  • [1] A report on the occurrence of Albian-Cenomanian elater-bearing pollen in Nasara-1 well, Upper Benue Trough, Nigeria: Biostratigraphic and palaeoclimatological implications
    Abubakar, M. B.
    Obaje, N. G.
    Luterbacher, H. P.
    Dike, E. F. C.
    Ashraf, A. R.
    [J]. JOURNAL OF AFRICAN EARTH SCIENCES, 2006, 45 (03) : 347 - 354
  • [2] [Anonymous], 1994, Bol. Geocienc. Petrobras
  • [3] [Anonymous], 1982, Bol. Inst. Geociencia. Univ. USP, DOI DOI 10.11606/ISSN.2316-8978.V13I0P116-128
  • [4] [Anonymous], 2001, ATLAS EARTH HIST
  • [5] [Anonymous], 2007, Boletim de Geociencias da Petrobras, Rio de Janeiro
  • [6] [Anonymous], 1996, REV GEOLOGIA
  • [7] [Anonymous], 1990, Origem and Evolucao de Bacias Sedimentares
  • [8] Antonioli L., 2001, THESIS FEDERAL U RIO
  • [9] Occurrences of elaterate pollen from the Lower Cretaceous of Ghana: Implications for biostratigraphy and palaeoclimatology
    Atta-Peters, D.
    [J]. INTERNATIONAL LETTERS OF NATURAL SCIENCES, 2013, 4 : 54 - 66
  • [10] Palynology of Aptian and upper Albian (Lower Cretaceous) amber-bearing outcrops of the southern margin of the Basque-Cantabrian basin (northern Spain)
    Barron, Eduardo
    Peyrot, Daniel
    Pedro Rodriguez-Lopez, Juan
    Melendez, Nieves
    Lopez del Valle, Rafael
    Najarro, Maria
    Rosales, Idoia
    Jose Comas-Rengifo, Ma
    [J]. CRETACEOUS RESEARCH, 2015, 52 : 292 - 312