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Miocene fern spores and pollen grains from the Solimões Basin, Amazon Region, Brazil

ABSTRACT

This work documents fern spores and pollen grains (miospores) recovered from rocks of the Solimões Formation (Solimões Basin), their botanical affinities, ecology and distribution in the Miocene of the Amazon Region. The assemblage of miospores is well preserved and diverse. They are identified, illustrated and assigned to the ten families of ferns and 22 families of spermatophytes. All miospores were identified to the taxonomic level of species except for two taxa (Perinomonoletes and Podocarpidites). The families Pteridaceae and Arecaceae were most representative of ferns and spermatophytes, respectively. This work contributes to the knowledge of the paleoflora and will aid in paleoenvironmental, paleoecological and biostratigraphic interpretations of the Miocene of the Amazon Region.

Keywords
Miocene; miospores; Neogene; palynology; Solimões; vegetation

Introduction

The Amazon is the largest tropical rainforest ecosystem and its high diversity can be explained by ecological, environmental and paleontological models. Climate changes in the Pleistocene caused the expansion and retraction of the rainforest cycles. The changes were considered the triggers for the speciation and accumulation of species (Haffer 1969Haffer J. 1969. Speciation in amazonian forest birds. Science 165: 131-137.) and this theory has long been the basis for interpreting the current diversity patterns. However, numerous studies (e.g., Gentry 1982Gentry AH. 1982. Neotropical floristic diversity: phytogeographical connections between Central and South America, Pleistocene climatic fluctuations, or an accident of the andean orogeny? Annals of the Missouri Botanical Garden 69: 557-593.; Frailey 1986Frailey CD. 1986. Late Miocene and Holocene mammals, exclusive of the Notoungulata, of the Rio Acre region, Western Amazonia. Contribution in Science, Natural History Museum of Los Angeles County 374: 1-46.; Hooghiemstra & Hammen 1998Hooghiemstra H, Hammen T. 1998. Neogene and Quaternary development of the Neotropical rain forest: the forest refugia hypothesis, and a literature overview. Earth - Science Review 44: 147-183.; Monsch 1998Monsch KA. 1998. Miocene fish faunas from the northwestern Amazonia basin (Colombia, Peru, Brazil) with evidence of marine incursions. Palaeogeography, Palaeoclimatology, Palaeoecology 143: 31-50.;Jaramillo et al. 2006Jaramillo C, Rueda M, Mora G. 2006. Cenozoic plant diversity in the Neotropics. Science 311: 1893-1896. ; Cozzuol 2006Cozzuol M. 2006. The Acre vertebrate fauna: diversity, geography and time. Journal of South American Earth Sciences 21: 185-203.; Hoorn et al. 2010aHoorn C, Wesselingh FP, Steege H, et al. 2010a. Amazonia Through Time: Andean uplift, climate change, landscape evolution, and biodiversity. Science 330: 927-931.) have shown that the diversification of biota is pre-Quaternary, reassembling to the last 60 Ma (million years).

The Neogene of Amazon region shows a flora very diversified. The records of this flora are based mainly on fossil woods and palynomorphs (e.g., spores, pollen grains) and a large part of this material allows establishing botanical affinities. For Miocene age, the palynology has been the most used technique to understand the past of the Amazon, especially miospores, which inform about the diversity and richness of the paleoflora. Several studies (e.g. Lorente 1986Lorente M. 1986. Palynology and palynofacies of the Upper Tertiary in Venezuela. Cramer, Berlin/Stuttgart Band, Dissertationes Botanicae. ; Hoorn 1993Hoorn C. 1993. Marine incursions and the influence of Andean tectonics on the Miocene depositional history of northwestern Amazônia: results of Palynostratigraphic study. Palaegeography, Palaeoclimatology, Palaeocology 105: 267-309. ; 1994aHoorn C. 1994a. Fluvial palaeoenvironments in intracratonic Amazonas Basin (Early Miocene-Early Middle Miocene, Colombia). Palaegeography, Palaeoclimatology, Palaeocology 109: 1-54. ; bHoorn C. 1994b. An environmental reconstruction of the palaeo-Amazon River sytem (Middle to Late Miocene, NW Amazonia). Palaeogeography, Palaeoclimatology, Paleoecology 112: 187-238.; cHoorn C. 1994c. Miocene palynostratigraphy and paleoenvironments of Northwestern Amazonia. PhD Thesis, University of Amsterdan, Amsterdan. ; Hoorn et al. 1995Hoorn C, Guerreiro J, Sarmiento G. 1995. Andean tectonics as a cause for changing drainage patterns in Miocene Northern South America. Geology 23: 237-240. ; Silva-Caminha et al. 2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67.; Hoorn et al. 2010bHoorn C, Wesselingh FP, Hovikoski J, Guerrero J. 2010b. The Amazonian mega-wetland (Miocene; Brazil, Colombia, Peru, Bolivia). In: Hoorn C, Wesselingh FP. (eds.) Amazonia, Landscape and Species Evolution: Look into the Past. Oxford, Wiley-Blackwell. p. 123-143. ; Silveira & Souza 2015Silveira RR, Souza PA. 2015. Palinologia (grãos de pólen de angiospermas) das formações Solimões e Içá (bacia do Solimões), nas regiões de Coari e Alto Solimões, Amazonas. Revista Brasileira de Paleontologia, 18: 455-474.; 2016Silveira RR, Souza PA. 2016. Palinologia (esporos de fungo e pteridófitas, grãos de pólen de gimnospermas, cistos de algas e escolecodonte) das formações Solimões e Içá (Neógeno e Pleistoceno, Bacia do Solimões), Amazonas, Brasil. Pesquisas em Geociências 43:17-39.; Leite et al. 2016Leite FPR, Paz J, Carmo DA, Silva-Caminha S. 2016. The effects of the inception of Amazonian transcontinental drainage during the Neogene on the landscape and vegetation of the Solimões Basin, Brazil. Palynology 40: 1-11.; D’Apolito 2016D’Apolito C. 2016. Landscape evolution in Western Amazonia: palynostratigraphy, palaeoenvironments and diversity of the Miocene Solimões formation, Brazil. PhD Thesis, University of Birmingham, Birmingham.) show a paleoflora rich in pteridophytes (Anemiaceae, Cyatheaceae, Polypodiaceae, Pteridaceae) and gymnosperms (Araucariaceae and Podocarpaceae). Angiosperms are a separate case because it is currently the most important flora in the Amazon region. Since the Miocene, almost all the families (e.g. Annonaceae, Arecaceae, Asteraceae, Bombacaceae, Euphorbiaceae, Fabaceae, Malvaceae, Melastomataceae, Malpighiaceae, Sapotaceae) were already present in the region (Gentry 1982Gentry AH. 1982. Neotropical floristic diversity: phytogeographical connections between Central and South America, Pleistocene climatic fluctuations, or an accident of the andean orogeny? Annals of the Missouri Botanical Garden 69: 557-593.; Burnham & Graham 1999Burnham RJ, Graham A. 1999. The history of Neotropical vegetation: new developments and status. Annais Missouri Botanical Garden 86: 546-589.; Jaramillo et al. 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334; Hoorn et al. 2010cHoorn C, Bernardes-de-Oliveira MEC, Dino R, et al. 2010c. Neogene climate evolution in Amazonia and the Brazilian Northeast. In: Carvalho IS, Garcia MJ, Lana CC, Strohschoen Jr O. (eds.) Paleontologia: Cenários de Vida-Paleoclimas. Rio de Janeiro, Interciência. p. 277-310.; 2017Hoorn C, Bogotá-A GR, Romero-Baez M, et al. 2017. The Amazon at sea: Onset and stages of the Amazon River from a marine record, with special reference to Neogene plant turnover in the drainage basin. Global and Planetary Change 153: 51-65.).

The recognition of the Miocene flora also allows interpretations paleoecological and paleoenvironmental inferences, as well as support the biostratigraphy framework of the region (Lorente 1986Lorente M. 1986. Palynology and palynofacies of the Upper Tertiary in Venezuela. Cramer, Berlin/Stuttgart Band, Dissertationes Botanicae. ; Hoorn 1993Hoorn C. 1993. Marine incursions and the influence of Andean tectonics on the Miocene depositional history of northwestern Amazônia: results of Palynostratigraphic study. Palaegeography, Palaeoclimatology, Palaeocology 105: 267-309. ; 1994cHoorn C. 1994c. Miocene palynostratigraphy and paleoenvironments of Northwestern Amazonia. PhD Thesis, University of Amsterdan, Amsterdan. ; Silva-Caminha et al. 2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67.; Leandro 2012Leandro LM. 2012. Análises palinoestratigráficas da Formação Solimões na porção noroeste do Alto Solimões, Amazonas, Brasil. MSc Thesis, Universidade do Vale do Rio dos Sinos, São Leopoldo.; Silveira & Souza 2015Silveira RR, Souza PA. 2015. Palinologia (grãos de pólen de angiospermas) das formações Solimões e Içá (bacia do Solimões), nas regiões de Coari e Alto Solimões, Amazonas. Revista Brasileira de Paleontologia, 18: 455-474.; 2016Silveira RR, Souza PA. 2016. Palinologia (esporos de fungo e pteridófitas, grãos de pólen de gimnospermas, cistos de algas e escolecodonte) das formações Solimões e Içá (Neógeno e Pleistoceno, Bacia do Solimões), Amazonas, Brasil. Pesquisas em Geociências 43:17-39.; Leite et al. 2016Leite FPR, Paz J, Carmo DA, Silva-Caminha S. 2016. The effects of the inception of Amazonian transcontinental drainage during the Neogene on the landscape and vegetation of the Solimões Basin, Brazil. Palynology 40: 1-11.).

Therefore, this work seeks to inventory fern spores and pollen grains found in the Miocene rocks (Solimões Formation), their affinities and ecology in order to facilitate taxonomic identification and to support paleoenvironmental, paleoecological and biostratigraphic studies of the Miocene in the Amazon.

Materials and methods

Study area

The Solimões Basin is located in the western portion of the Amazon, bordered to the west by the Iquitos Arch and to the east by the Purus Arch. It is Paleozoic intracratonic depression, covering about 950,000 km2 (Barata & Caputo 2007Barata CF, Caputo MV. 2007. Geologia do petróleo da Bacia do Solimões - O Estado da Arte. Campinas, PDPETRO. ) is between 2°-8°S 62°-72°W (Fig. 1). Internally, there is a north-south regional control characterized to distribute the sediments in the basin, called the Carauari Arch. This subdivides the depression into the Juruá sub-basin to the east and the Jandiatuba sub-basin to the west (Wanderley-Filho et al. 2007Wanderley-Filho JR, Eiras JF, Vaz PT, et al 2007. Bacia do Solimões. Boletim de Geociências da Petrobrás 15: 217-225. , Fig. 1).

Figure 1
Solimões Basin location. A. Juruá sub-basin. B. Jandiatuba sub-basin. C. Carauari High. Legends: black dots 1-AS-37-AM (1) e 1-AS-46-AM (2); red dot: 1-AS-4a-AM (11); green dot: 1-AS-32-AM (10); yellow dots: 1-AS-19-AM (6) and 1-AS-27-AM (5); white dots: 1-AS-51-AM (4) and 1-AS-52-AM (3); blue dots: 1-AS-31-AM (7) and 1-AS-34-AM (8); pink dot: 1-AS-33-AM (9); brown dot: 1-AS-105-AM (12) and orange dot: Coari and Alto Solimões outcrops (13). Please see the PDF version for color reference.

According to Eiras et al. (1994Eiras JF, Becker CR, Souza EM, Gonzaga FG, Silva JGF, Daniel LMF. 1994. Bacia do Solimões. Boletim de Geociências da Petrobrás 8: 17-45.), the Solimões Basin covers six depositional sequences: Ordovician, Siluro-Devonian, Devonian-Carboniferous, Carboniferous-Permian, Cretaceous and Cenozoic. In the last sequence are recognizing the Solimões and Içá formations.

The Solimões Formation extends for about 500,000 km2, with sedimentary thickness ranging from 300 to 400 m, and can reach up to 1000 m near the Iquitos Arch. It covers Acre and west Amazonas, as well as the territories of Peru (Marañon and Putumayo basins) and Colombia (Caquetá and Putumayo basins) (Maia et al. 1977Maia RGN, Godoy HK, Yamaguti HS, et al. 1977. Projeto de carvão no Alto Solimões. Relatório Final. Manaus, CPRM-DNPM. ; Hoorn et al. 2010aHoorn C, Wesselingh FP, Steege H, et al. 2010a. Amazonia Through Time: Andean uplift, climate change, landscape evolution, and biodiversity. Science 330: 927-931.). The Solimões Formation rocks comprise shales, siltstones and sandy shales, clayey silts and medium to fine-grained sands, lignites, carbonaceous clays and limestones (Maia et al. 1977Maia RGN, Godoy HK, Yamaguti HS, et al. 1977. Projeto de carvão no Alto Solimões. Relatório Final. Manaus, CPRM-DNPM. ).

In relation to the paleoenvironments during the Miocene, several studies indicate a heterogeneous and dynamic environment composed of rivers, lakes, flood plains, mangroves and coastal plains. It is also found elements of transitional and / or marine environments such as microforaminifera linings, molluscs and dinoflagellate cysts (e.g. Hoorn 1993Hoorn C. 1993. Marine incursions and the influence of Andean tectonics on the Miocene depositional history of northwestern Amazônia: results of Palynostratigraphic study. Palaegeography, Palaeoclimatology, Palaeocology 105: 267-309. ; 1994aHoorn C. 1994a. Fluvial palaeoenvironments in intracratonic Amazonas Basin (Early Miocene-Early Middle Miocene, Colombia). Palaegeography, Palaeoclimatology, Palaeocology 109: 1-54. ; Räsänen et al. 1995Räsänen ME, Linna AM, Santos JCR, Negri FR. 1995. Late Miocene tidal deposits in the Amazonian foreland basin. Science 269: 386-389.; Latrubesse et al. 1997Latrubesse E, Bocquentin J, Santos JCR, Ramonell CG. 1997. Paleoenvironmental model for the late Cenozoic southwestern Amazonia paleontology and geology. Acta Amazonica 27: 103-118. ; 2007Latrubesse E, Caminha-Silva S, Cozzuol M, Absy M. 2007. Late Miocene continental sedimentation in the southwestern Amazonia and its regional significance: Biotic and geological evidence. Journal of South American Earth Science 23: 61-80. ; 2010Latrubesse E, Cozzuol M, Rigsby C, Silva S, Absy ML, Jaramillo C. 2010. The Late Miocene paleogeography of the Amazon Basin and the evolution of the Amazon River system. Earth-Science Reviews 99: 99-124.; Lovejoy 1998Lovejoy N. 1998. Marine incursion into South America. Nature 396: 421-422.; Vonhof et al. 1998Vonhof HB, Wesselingh FP, Ganssen GM. 1998. Reconstruction of the Miocene western Amazonian aquatic system using molluscan isotopic signatures. Palaeogeography, Palaeoclimatology, Paleoecology 141: 85-93. ; 2003Vonhof HB, Wesselingh FP, Kaandorp RJG. 2003. Paleogeography of Miocene western Amazonia: isotopic composition of molluscan shells constrains the influence of marine incursions. Geology Society of America Bulletin 115: 983-993.; Wesselingh et al. 2002Wesselingh FP, Räsänen ME, Irion G, et al. 2002. Lake Pebas: a palaeoecological reconstruction of a Miocene, a long-lived lake complex in western Amazonia. Cainozoic Research 1: 35-81. ; 2006Wesselingh FP, Ranzi A, Räsänen ME. 2006. Miocene freshwater Mollusca from western Brazilian Amazonia. Scripta Geologica 133: 419-437.; Wesselingh 2006Wesselingh FP. 2006. Molluscs from the Miocene Pebas Formation of Peruvian and Colombian Amazonia. Scripta Geologica 133: 19-290.; Wesselingh & Salo 2006Wesselingh FP, Salo JA. 2006. A Miocene perspective on the evolution of the Amazonian biota. Scripta Geologica 133: 439-458.; Ramos 2006Ramos M I. 2006. Ostracods from the Neogene Solimões Formation (Amazonas, Brazil). Journal of South American Earth Sciences 21: 87-95.; Hoorn et al. 2010aHoorn C, Wesselingh FP, Steege H, et al. 2010a. Amazonia Through Time: Andean uplift, climate change, landscape evolution, and biodiversity. Science 330: 927-931.; Gross et al. 2011Gross M, Piller WE, Ramos MI, Paz JDS. 2011. Late Miocene sedimentary environments in south-western Amazonia (Solimões Formation; Brasil). Journal of South American Earth Sciences 32: 169-181.; 2013Gross M, Ramos MI, Caporaletti M, Pilner WE. 2013. Ostracods (Crustacea) and their palaeoenviromental implication for the Solimões Formation (Late Miocene; Western Amazonia/Brazil). Journal of South American Earth Sciences 42: 216-241.; Linhares et al. 2011Linhares AP, Ramos MIF, Gross M, Piller WE. 2011. Evidence for marine influx during the Miocene in southwestern Amazonia, Brazil. Geología Colombiana 36: 91-104. ; Nogueira et al. 2013Nogueira ACR, Silveira R, Guimarães JTF. 2013. Neogenee-Quaternary sedimentary and paleovegetation history of the eastern Solimões Basin, central Amazon region. Journal of South American Earth Sciences 46: 89-99.; Boonstra et al. 2015Boonstra M, Ramos MIF, Lammertsma EI, Antonie PO, Hoorn C. 2015. Marine connections of Amazonia: Evidence from foraminífera and dinoflagellate cysts (early to middle Miocene, Colombia/Peru). Palaeogeography, Palaeoclimatology, Palaeoecology 417: 176-194. ).

Metodology

In the Solimões Basin investigations for energy resources were conducted by the federal government in the 1970s by the Geological Survey of Brazil (CPRM) and the National Department of Mineral Production (DNPM). The project entitled "Coal Alto Solimões" did a survey of areas with coal mining potential. A total of 84 wells was drilled in an area of 320,000 km2 in northwest Brazil and this material was deposited at CPRM/DNPM - Manaus - AM (Maia et al. 1977Maia RGN, Godoy HK, Yamaguti HS, et al. 1977. Projeto de carvão no Alto Solimões. Relatório Final. Manaus, CPRM-DNPM. ). The wells 1-AS-37-AM and 1-AS-46-AM were chosen for palynological analysis considering its position in the Solimões Basin and the state of conservation.

The well 1-AS-37-AM is at an altimetric elevation of 60 m and coordinates 03°30'S 68°51'W near the Jandiatuba River. Its thickness is 242.60 m, and the initial 12 m corresponds to Holocene deposits in contact with the top of the Solimões Formation. The lithology is predominantly pelitic with higher occurrence of lignite layers (Maia et al. 1977Maia RGN, Godoy HK, Yamaguti HS, et al. 1977. Projeto de carvão no Alto Solimões. Relatório Final. Manaus, CPRM-DNPM. ).

The well 1-AS-46-AM is located in the northwestern portion of the Solimões Basin, coordinates 02°23'S 68°28'W, altimetry 101 m and thickness of 200.90 m. In this well, the Içá Formation represents the initial 6.0 m in erosive contact with the Solimões Formation. The lithology is pelitic and there are fewer layers of lignite (Maia et al. 1977Maia RGN, Godoy HK, Yamaguti HS, et al. 1977. Projeto de carvão no Alto Solimões. Relatório Final. Manaus, CPRM-DNPM. ).

For the study were selected 100 core samples from each well, from which 10g/sample was processed by standard technique in palynology to eliminate the inorganic material by means of acidic attacks (see Uesugui 1979Uesugui N. 1979. Palinologia; técnicas de tratamento de amostras. Boletim Técnico da Petrobrás 22: 229-240.; Erdtman 1969Erdtman G. 1969. Handbook of palynology. Copenhagen, Scandinavian University Books.; Faegri & Iversen 1966Faegri K, Iversen J. 1966. Textbook of pollen analysis. Copenhagen, Scandinavian University Books.).

The miospores recovered from the cores were identified by comparison with works of Germeraad et al. (1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348.); Regali et al. (1974aRegali MSP, Uesugui N, Santos AS. 1974a. Palinologia dos sedimentos meso-cenozóicos do Brasil - I. Boletim Técnico da Petrobrás 17: 177-191. ; bRegali MSP, Uesugui N, Santos AS. 1974b. Palinologia dos sedimentos meso-cenozóicos do Brasil - II. Boletim Técnico da Petrobrás 17: 263-301.); Lorente (1986Lorente M. 1986. Palynology and palynofacies of the Upper Tertiary in Venezuela. Cramer, Berlin/Stuttgart Band, Dissertationes Botanicae. ); Hoorn (1993Hoorn C. 1993. Marine incursions and the influence of Andean tectonics on the Miocene depositional history of northwestern Amazônia: results of Palynostratigraphic study. Palaegeography, Palaeoclimatology, Palaeocology 105: 267-309. ; 1994cHoorn C. 1994c. Miocene palynostratigraphy and paleoenvironments of Northwestern Amazonia. PhD Thesis, University of Amsterdan, Amsterdan. ); Silva-Caminha et al. (2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67.); Jaramillo et al. (2011Jaramillo C, Rueda M, Torres V. 2011. A palynological zonation for the Cenozoic of the Llanos and Llanos Foothills of Colombia. Palynology 35: 46-84. ); D'Apolito (2016D’Apolito C. 2016. Landscape evolution in Western Amazonia: palynostratigraphy, palaeoenvironments and diversity of the Miocene Solimões formation, Brazil. PhD Thesis, University of Birmingham, Birmingham.) and the website http://biogeodb.stri.si.edu/jaramillo/palynomorph/pollen, which hosts an atlas with images of several publications of palynomorphs from North of South America. The botanical affinities, ecology and distribution of spores and pollen grains were attributed according to the studies above and Tryon & Lugardon (1991Tryon AF, Lugardon B. 1991. Spores of the Pteridophyta. Surface, wall structure and diversity based on electron microscope studies. New York, Springer.); Jaramillo et al. (2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334; 2011Jaramillo C, Rueda M, Torres V. 2011. A palynological zonation for the Cenozoic of the Llanos and Llanos Foothills of Colombia. Palynology 35: 46-84. ); Jaramillo & Rueda (2013)Jaramillo C, Rueda MJ. 2013. A morphological electronic database of Cretaceous Tertiary and extant pollen and spores from Northern South America. v. 2012/2013. http://biogeodb.stri.si.edu/jaramillo/palynomorph/. 25 Apr. 2017.
http://biogeodb.stri.si.edu/jaramillo/pa...
and Silveira & Souza (2015Silveira RR, Souza PA. 2015. Palinologia (grãos de pólen de angiospermas) das formações Solimões e Içá (bacia do Solimões), nas regiões de Coari e Alto Solimões, Amazonas. Revista Brasileira de Paleontologia, 18: 455-474.; 2016Silveira RR, Souza PA. 2016. Palinologia (esporos de fungo e pteridófitas, grãos de pólen de gimnospermas, cistos de algas e escolecodonte) das formações Solimões e Içá (Neógeno e Pleistoceno, Bacia do Solimões), Amazonas, Brasil. Pesquisas em Geociências 43:17-39.).

The photographs were obtained in Axioplan microscope and AxioCam MRc camera, with 1000x magnification by the program Axiovision and processed in the software Corel Draw 17.0. Each miospore was referenced using the "England Finder" coordinates associated with the number slides. The slides were deposited in the Laboratory of Plant Paleoecology of the Department of Geology and Paleontology of the National Museum of the Federal University of Rio de Janeiro.

Results

Sixty miospores were selected for this work, which include 19 fern spores and 41 pollen grains. The spores are distributed into 10 families, being the family Pteridaceae the most frequent. The pollen grains are distributed into 22 families (according to Cronquist 1988Cronquist A. 1988. The evolution and classification of flowering plants. 2nd. edn. New York, New York Botanical Garden.), with emphasis on the family Arecaceae. The miospores were systematized in two categories: spores and pollen grains, following the alphabetical order. Botanical affinity, ecology and distribution in the Solimões Formation (Tab. 1, Fig. 1) were attributed based on the literature.

Table 1
Miospores documented in this study and in the previous works for Solimões Formation. For the location of the wells, see Figure 1.

Anteturma SPORITES Potonié 1893

Genus Cingulatisporites Thomson emend. Potonié 1956

Cingulatisporites laevigatusSilva-Caminha et al. 2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67. (Fig. 2A)

Botanical affinity: unknown

Ecology: unknown

Figure 2
Fern spores recorded in the studied sections. A. Cingulatisporites laevigatus. B. Crassoretitriletes vanhadshoovenii. C. Deltoidospora adriennsis. D. Distaverrusporites margaritatus. E. Echinatisporis infantus. F. Echinatisporis muelleri. G. Kuylisporites waterbolkii. H. Laevigatosporites tibuiensis. I. Magnastriatites grandiosus. Scale bar= 20 µm.

Genus CrassoretitriletesGermeraad et al, 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348.

Crassoretitriletes vanraadshooveniiGermeraad et al. 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348. (Fig. 2B)

Ecology: pantropical, it occurs throughout South America (Tryon & Lugardon 1991Tryon AF, Lugardon B. 1991. Spores of the Pteridophyta. Surface, wall structure and diversity based on electron microscope studies. New York, Springer.), wetlands and swamps.

Genus Deltoidospora Miner 1935

Deltoidospora adriennis (Potonié & Gelletich 1933) Fredericksen 1983 (Fig. 2C)

Botanical affinity: family Pteridaceae, Acrostichum aureum

Ecology: pantropical, it occurs in coastal environments on all continents (Tryon & Lugardon 1991Tryon AF, Lugardon B. 1991. Spores of the Pteridophyta. Surface, wall structure and diversity based on electron microscope studies. New York, Springer.), mangrove (Jaramillo et al. 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334)

Genus Distaverrusporites Muller 1968

Distaverrusporites margaritatus Muller 1968 (Fig. 2D)

Botanical affinity: unknown

Ecology: unknown

Genus Echinatisporis Krutzsch 1959

Echinatisporis infantusD’Apolito 2016D’Apolito C. 2016. Landscape evolution in Western Amazonia: palynostratigraphy, palaeoenvironments and diversity of the Miocene Solimões formation, Brazil. PhD Thesis, University of Birmingham, Birmingham. (Fig. 2E)

Botanical affinity: families Thelypteraceae/Athyriaceae/Marathiaceae

Ecology: unknown

Echinatisporis muelleri Krutzsch 1967 (Fig. 2F)

Botanical affinity: families Thelypteraceae/Athyriaceae/Marathiaceae (D’Apolito 2016D’Apolito C. 2016. Landscape evolution in Western Amazonia: palynostratigraphy, palaeoenvironments and diversity of the Miocene Solimões formation, Brazil. PhD Thesis, University of Birmingham, Birmingham.)

Ecology: unknown

Genus Kuylisporites Potonié 1956

Kuylisporites waterbolkii Potonié 1956 (Fig. 2G)

Botanical affinity: family Cyatheaceae, Cyathea horrida

Ecology: mountain areas (Jaramillo et al. 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334)

Genus Laevigatoporites Ibrahim

Laevigatosporites tibuiensis (Van der Hammen 1956a) Jaramillo & Dilcher 2001 (Fig. 2H)

Botanical affinity: unknown

Ecology: unknown

Genus MagnastriatitesGermeraad et al. 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348., emend. Dettmann & Clifford 1992

Magnastriatites grandiosus (Kedves & Sole de Porta 1963) Dueñas 1980 (Fig. 2I)

Botanical affinity: Family Pteridaceae, genus Ceratopteris

Ecology: aquatic genus (Tryon & Lugardon 1991Tryon AF, Lugardon B. 1991. Spores of the Pteridophyta. Surface, wall structure and diversity based on electron microscope studies. New York, Springer.), rivers and shallow lakes (Jaramillo et al. 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334)

Genus Nijssenosporites

Nijssenosporites fossulatusLorente 1986Lorente M. 1986. Palynology and palynofacies of the Upper Tertiary in Venezuela. Cramer, Berlin/Stuttgart Band, Dissertationes Botanicae. (Fig. 3A)

Botanical affinity: Family Adianthaceae, Genus Pityrogramma

Ecology: pantropical genus (Tryon & Lugardon 1991Tryon AF, Lugardon B. 1991. Spores of the Pteridophyta. Surface, wall structure and diversity based on electron microscope studies. New York, Springer.), plain.

Figure 3
Fern spores recorded in the studied sections. A. Nijssenosporites fossulatus. B. Perinomonoletes. C. Polypodiaceoisporites amazonensis. D. Polypodiaceoisporites potoniei. E. Polypodiisporites aff. specious. F. Psilatriletes lobatus. G. Retitriletes sommeri. H. Verrucatoporites usmensis. I. Verrucatotriletes bullatus. J. Verrucatotriletes etayoi. Scale bar= 20µm.

Genus Perinomonoletes Krutzsch, 1967

Perinomonoletes sp. (Fig. 3B)

Botanical affinity: families Aspleniaceae/Thelypteraceae (Jaramillo et al. 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334)

Ecology: unknown

Genus Polypodiaceoisporites Potonié 1951 ex Potonié 1956

Polypodiaceoisporites amazonensisSilva-Caminha et al. 2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67. (Fig. 3C)

Botanical affinity: family Pteridaceae

Ecology: unknown

Polyapodiaceoisporites potoniei Kedves 1961 (Fig. 3D)

Botanical affinity: family Pteridaceae, Pteris

Ecology: open vegetation, riverine banks (Tryon & Lugardon 1991Tryon AF, Lugardon B. 1991. Spores of the Pteridophyta. Surface, wall structure and diversity based on electron microscope studies. New York, Springer.), plain and highland (Jaramillo et al. 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334)

Genus Polypodiisporites Potonié 1956 emend Khan and Martin 1971

Polypodiisporites aff. specious Sah 1967 1961 (Fig. 3E)

Botanical affinity: family Polypodiaceae

Ecology: plain (D’Apolito 2016D’Apolito C. 2016. Landscape evolution in Western Amazonia: palynostratigraphy, palaeoenvironments and diversity of the Miocene Solimões formation, Brazil. PhD Thesis, University of Birmingham, Birmingham.)

Genus Psilatriletes van der Hammen 1954 ex Potonié 1956

Psilatriletes lobatus Hoorn 1994 (Fig. 3F)

Botanical affinity: unknown

Ecology: unknown

Genus Retitriletes Pierce 1961

Retitriletes sommeri Regali et al. 1974 (Fig. 3G)

Botanical affinity: family Lycopodiaceae?

Ecology: unknown

Genus Verrucatosporites Thomson & Pflug 1953

Verrucatosporites usmensis (Van der Hammen 1956) Germeraad et al. 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348. (Fig. 3H)

Botanical affinity: family Polypodiaceae, Stenochlaena palustris

Ecology: highland forest and e plain (Jaramillo et al. 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334)

Genus Verrucatotriletes Van Hoeken-Klinkenberg 1964

Verrucatotriletes bullatus Van Hoeken-Klinkenberg 1964 (Fig. 3I)

Botanical affinity: family Cyatheaceae, Alsophyla

Ecology: pantropical genus (Tryon & Lugardon1991Tryon AF, Lugardon B. 1991. Spores of the Pteridophyta. Surface, wall structure and diversity based on electron microscope studies. New York, Springer.), highland (Jaramillo et al 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334).

Verrucatotriletes etayoi Dueñas, 1980 (Fig. 3J)

Botanical affinity: unknown

Ecology: unknown

Anteturma POLLENITES Potonié 1893

Gimnosperms pollen grains

Genus Cyclusphaera Elsik 1966

Cyclusphaera scabrata Jaramillo & Dilcher, 2001 (Fig. 4A)

Botanical affinity: Family Araucariaceae

Ecology: mountain area

Figure 4
Pollen grains recorded in the studied sections. A. Cyclusphaera scabrata. B. Podocarpidites. C. Arecipites perfectus. D. Bombacacidites baculatus. E. Bombacacidites fossulatus. F. Bombacacidites lorenteae. G. Bombacacidites nacimientoensis. H. Cichoreacidites longispinosus. I. Corsinipollenites oculusnoctis (tetrad). Scale bar= 20µm.

Genus Podocarpidites Cookson 1947

Podocarpidites sp. Cookson 1947 ex Couper 1953 (Fig. 4B)

Botanical affinity: family Podocarpaceae, Podocarpus

Ecology: mountain and lownland forest (Jaramillo et al. 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334)

Angiosperms pollen grains

Genus Arecipites Wodehouse 1933, emend. Nichols et al. 1973

Arecipites perfectusSilva-Caminha et al 2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67. (Fig. 4C)

Botanical affinity: family Arecaceae

Ecology: unknown

Genus Bombacacidites Couper 1960

Bombacacidites baculatus Muller et al. 1987 (Fig. 4D)

Botanical affinity: family Bombacaceae, Pachira aquatica

Ecology: tropical forest, swamps and along rivers

Bombacacidites fossulatusSilva-Caminha et al. 2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67. (Fig. 4E)

Botanical affinity: family Bombacaeae

Ecology: unknown

Bombacacidites lorenteae (Hoorn 1993Hoorn C. 1993. Marine incursions and the influence of Andean tectonics on the Miocene depositional history of northwestern Amazônia: results of Palynostratigraphic study. Palaegeography, Palaeoclimatology, Palaeocology 105: 267-309. ) D’Apolito 2016D’Apolito C. 2016. Landscape evolution in Western Amazonia: palynostratigraphy, palaeoenvironments and diversity of the Miocene Solimões formation, Brazil. PhD Thesis, University of Birmingham, Birmingham. (Fig. 4F)

Botanical affinity: family Bombacaeae, Bombax

Ecology: along creeks and rivers

Bombacacidites nacimientoensis (Anderson1960) Elsik 1968 (Fig. 4G)

Botanical affinity: Family Bombacaeae, genus Bombax

Ecology: plains, along watercourses (Jaramillo et al. 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334)

Genus Cichoreacidites Sah 1967

Cichoreacidites longispinosus (Lorente 1986Lorente M. 1986. Palynology and palynofacies of the Upper Tertiary in Venezuela. Cramer, Berlin/Stuttgart Band, Dissertationes Botanicae. ) Silva-Caminha 2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67. (Fig. 4H)

Botanical affinity: family Asteraceae

Ecology: swamps, open vegetation and savannahs

Genus Corsinipollenites Nakoman 1965

Corsinipollenites oculusnoctis (tétrade) (Thiergart 1940); Nakoman (Fig. 4I)

Botanical affinity: family Onagraceae, Ludwigia

Ecology: marshes (Jaramillo et al. 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334)

Genus Echiperiporites Van der Hammem & Wymstra 1964

Echiperiporites akanthos Van der Hammem & Wymstra 1964 (Fig. 5A)

Botanical affinity: family Alismataceae, Sagittaria/Echinodorus

Ecology: swamps and lakes (D’Apolito 2016D’Apolito C. 2016. Landscape evolution in Western Amazonia: palynostratigraphy, palaeoenvironments and diversity of the Miocene Solimões formation, Brazil. PhD Thesis, University of Birmingham, Birmingham.)

Figure 5
Pollen grains recorded in the studied sections. A. Echiperiporites akanthos. B. Echiperiporites estelae. C. Echiperiporites lophatus. D-E. Echiperiporites scrabrannulatus. F. Echitricolporites spinosus. G. Echitriporites trianguliformis. H. Fenestristes garciae. I. Fenestrites spinosus. J. Grimsdalea magnaclavata. K. Inaperturopollenites solimoensis. L. Ladakhipollenites? caribbiensis. Scale bar= 20µm.

Echiperiporites estelaeGermeraad et al. 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348. (Fig. 5B)

Botanical affinity: families Malvaceae/Convolvulaceae

Ecology: coastal vegetation

Echiperiporites lophatusSilva-Caminha et al. 2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67. (Fig. 5C)

Botanical affinity: family Convolvulaceae?

Ecology: herbaceous liana? (D’Apolito 2016D’Apolito C. 2016. Landscape evolution in Western Amazonia: palynostratigraphy, palaeoenvironments and diversity of the Miocene Solimões formation, Brazil. PhD Thesis, University of Birmingham, Birmingham.)

Echiperiporites scabrannulatusJaramillo et al. 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334 (Fig. 5D-E)

Botanical affinity: unknown

Ecology: unknown

Genus Echitricolporites Van der Hammen 1956 ex Germeraad et al. 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348.

Echitricolporites spinosus Van der Hammen 1956 ex Germeraad et al. 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348. (Fig. 5F)

Botanical affinity: family Asteraceae

Ecology: open vegetation

Genus Echitriporites Van der Hammen 1956

Echitriporites trianguliformis Van Hoeken Klinkenberg 1964 (Fig. 5G)

Botanical affinity: family Proteaceae (Jaramillo & Rueda 2013Jaramillo C, Rueda MJ. 2013. A morphological electronic database of Cretaceous Tertiary and extant pollen and spores from Northern South America. v. 2012/2013. http://biogeodb.stri.si.edu/jaramillo/palynomorph/. 25 Apr. 2017.
http://biogeodb.stri.si.edu/jaramillo/pa...
)

Ecology: unknown

Genus Fenestrites Van der Hammen, 1956

Fenestrites garciaeLeite 2006Leite FPR. 2006. Palinologia da Formação Solimões, Neógeno da Bacia do Solimões, estado do Amazonas: Implicação paleoambientais e bioestratigráficas. PhD Thesis, Universidade de Brasília, Brasília. (Fig. 5H)

Botanical affinity: family Amaranthaceae, Gomphrena

Ecology: unknown

Fenestrites spinosus Van der Hammen, 1956 (Fig. 5I)

Botanical affinity: family Asteraceae (Germeraad et al. 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348.)

Ecology: unknown

Genus GrimsdaleaGermeraad et al. 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348.

Grimsdalea magnaclavataGermeraad et al. 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348. (Fig. 5J)

Botanical affinity: family Arecaceae?

Ecology: unknown

Genus Inaperturopollenites Nilsson 1958

Inaperturopollenites solimoensisLeite 2006Leite FPR. 2006. Palinologia da Formação Solimões, Neógeno da Bacia do Solimões, estado do Amazonas: Implicação paleoambientais e bioestratigráficas. PhD Thesis, Universidade de Brasília, Brasília. (Fig. 5K)

Botanical affinity: family Rubiaceae, Psychotria?

Ecology: unknown

Genus Ladakhipollenites Mathur & Jain 1980

Ladakhipollenites? caribbiensis (Muller et al. 1987) Silva-Caminha et al. 2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67. (Fig. 5L)

Botanical affinity: family Euphorbiaceae, Sapium

Ecology: terra firme forest and varzea forest

Genus Loranthacites Mtchedlishvili in Samoilovitch & Mtchedlishvili 1961

Loranthacites digitatusSilva-Caminha et al. 2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67. (Fig. 6A)

Botanical affinity: family Loranthaceae (Jaramillo & Rueda 2013Jaramillo C, Rueda MJ. 2013. A morphological electronic database of Cretaceous Tertiary and extant pollen and spores from Northern South America. v. 2012/2013. http://biogeodb.stri.si.edu/jaramillo/palynomorph/. 25 Apr. 2017.
http://biogeodb.stri.si.edu/jaramillo/pa...
)

Ecology: unknown

Figure 6
Pollen grains recorded in the studied sections. A. Loranthacites digitatus. B-C. Malvacipollis spinulosa. D. Malvacipolloides maristellae. E. Margocolporites "hornii". F. Margocolporites vanwijhei. G. Mauritiidites franciscoi var. franciscoi. H. Perisyncolporites pokornyi. I. Polyadopollenites marileae. J. Proteacidites triangulatus. K. Proxapertites tertiaria. L. Psilamonocolpites amazonicus. M. Psilaperiporites multiporatus. Scale bar= 20µm.

Genus Malvacipollis Harris 1965

Malvacipollis spinulosa Frederiksen, 1983 (Fig. 6B-C)

Botanical affinity: family Euphorbiaceae (Leite 2006Leite FPR. 2006. Palinologia da Formação Solimões, Neógeno da Bacia do Solimões, estado do Amazonas: Implicação paleoambientais e bioestratigráficas. PhD Thesis, Universidade de Brasília, Brasília. )

Ecology: unknown

Genus Malvacipolloides Anzótegui & Garalla 1986

Malvacipolloides maristellae (Muller et al. 1987) Silva-Caminha et al 2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67. (Fig. 6D)

Botanical affinity: family Bombacaceae

Ecology: terra firme forest

Genus Margocolporites Ramanujam 1966 ex Srivastava 1969, emend. Pocknall & Mildenhall 1984

Margocolporites “hornii” (Fig. 6E)

Botanical affinity: family Apocynaceae?

Ecology: unknown

Margocolporites vanwijheiGermeraad et al. 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348. (Fig. 6F)

Botanical affinity: family Caesalpiniaceae, Caesalpinea

Ecology: coastal vegetation

Genus Mauritiidites van Hoeken-Klinkenberg 1964

Mauritiidites franciscoi var. franciscoi Van der Hammen, 1956) Van Hoeken Klinkenberg 1964 (Fig. 6G)

Botanical affinity: family Arecaceae, Mauritia

Ecology: plain and swamps

Genus PerisyncolporitesGermeraad et al. 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348.

Perisyncolporites pokornyiGermeraad et al. 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348. (Fig. 6H)

Botanical affinity: family Malpighiaceae

Ecology: plain and terra firme forest

Genus Polyadopollenites Pflug and Thomson 1953

Polyadopollenites marileaeLeite 2006Leite FPR. 2006. Palinologia da Formação Solimões, Neógeno da Bacia do Solimões, estado do Amazonas: Implicação paleoambientais e bioestratigráficas. PhD Thesis, Universidade de Brasília, Brasília. (Fig. 6I)

Botanical affinity: family Mimosaceae

Ecology: unknown

Genus Proteacidites Cookson emend. Couper 1953

Proteacidites triangulatusLorente 1986Lorente M. 1986. Palynology and palynofacies of the Upper Tertiary in Venezuela. Cramer, Berlin/Stuttgart Band, Dissertationes Botanicae. (Fig. 6J)

Botanical affinity: families Sapindaceae/Proteaeceae

Ecology: tropical forest and montane forest

Genus Proxapertites Van der Hammen 1956

Proxapertites tertiaria Van der Hammen & García de Mutis 1966 (Fig. 6K)

Botanical affinity: family Annonaceae, Crematosperma

Ecology: lowland forest (Jaramillo et al. 2010Jaramillo C, Hoorn C, Silva SAF, et al. 2010. The origin of the modern Amazon rainforest: implications of the palynological and paleobotanical record. In: Hoorn C, Wesselingh FP. (eds.) Amazonia: landscape and species evolution - a look into the past. Oxford, Blackwell Publishing. p. 317-334).

Genus Psilamonocolpites Van der Hammen & C. Garcia de Mutis 1966

Psilamonocolpites amazonicusHoorn 1993Hoorn C. 1993. Marine incursions and the influence of Andean tectonics on the Miocene depositional history of northwestern Amazônia: results of Palynostratigraphic study. Palaegeography, Palaeoclimatology, Palaeocology 105: 267-309. (Fig. 6L)

Botanical affinity: family Arecaceae, Euterpe

Ecology: várzea forest, plain and swamps

Genus Psilaperiporites Regali et al. 1974

Psilaperiporites multiporatus Hoorn 1994 (Fig. 6M)

Botanical affinity: unknown

Ecology: unknown

Genus Psilastephanoporites Van der Hammen 1956

Psilastephanoporites herngreeniiHoorn 1993Hoorn C. 1993. Marine incursions and the influence of Andean tectonics on the Miocene depositional history of northwestern Amazônia: results of Palynostratigraphic study. Palaegeography, Palaeoclimatology, Palaeocology 105: 267-309. (Fig. 7A)

Botanical affinity: family Apocynaceae

Ecology: lowland forest

Figure 7
Pollen grains recorded in the studied sections. A. Psilastephanoporites herngreenii. B. Psilastephanoporites tesseroporus. C. Psilatricolporites silvaticus. D. Retistephanoporites crassinanulatus. E. Retitrescolpites irregularis. F. Retitrescolpites traversei. G. Retitriporites dubiosus. H-I. Rhoipites guianensis. J. Rhoipites toigoi. Scale bar= 20 µm.

Psilastephanoporites tesseroporus Regali et al. 1974 (Fig. 7B)

Botanical affinity: family Apocynaceae, Prestonia? (Leite 2006Leite FPR. 2006. Palinologia da Formação Solimões, Neógeno da Bacia do Solimões, estado do Amazonas: Implicação paleoambientais e bioestratigráficas. PhD Thesis, Universidade de Brasília, Brasília. )

Ecology: unknown

Genus Psilatricolporites Pierce 1961

Psilatricolporites silvaticusHoorn 1993Hoorn C. 1993. Marine incursions and the influence of Andean tectonics on the Miocene depositional history of northwestern Amazônia: results of Palynostratigraphic study. Palaegeography, Palaeoclimatology, Palaeocology 105: 267-309. (Fig. 7C)

Botanical affinity: family Burseraceae/Sapotaceae

Ecology: lowland forest

Genus Retistephanoporites González-Guzmán 1967

Retistephanoporites crassinanulatusLorente 1986Lorente M. 1986. Palynology and palynofacies of the Upper Tertiary in Venezuela. Cramer, Berlin/Stuttgart Band, Dissertationes Botanicae. (Fig. 7D)

Botanical affinity: family Malvaceae, Quararibea

Ecology: lowland forest

Genus Retitrescolpites Sah 1967

Retitrescolpites irregulares (Van der Hammen & Wymstra 1964) Jaramillo & Dilcher 2001 (Fig. 7E)

Botanical affinity: family Euphorbiaceae, Amanoa

Ecology: lowland forest, along watercourses (Jaramillo & Rueda 2013Jaramillo C, Rueda MJ. 2013. A morphological electronic database of Cretaceous Tertiary and extant pollen and spores from Northern South America. v. 2012/2013. http://biogeodb.stri.si.edu/jaramillo/palynomorph/. 25 Apr. 2017.
http://biogeodb.stri.si.edu/jaramillo/pa...
)

Retitrescolpites traverseiSilva-Caminha et al 2010Silva-Caminha SAF, Jaramillo CA, Absy ML. 2010. Neogene palynology of the Solimões Basin, Brazilian Amazonia. Palaeontographica 283: 1-67. (Fig. 7F)

Botanical affinity: family Acanthaceae, Teliostachya

Ecology: lowland forest

Genus Retitriporites (Van der Hammen, 1956) Gonzalez-Guzmán, 1967

Retitriporites dubiosus Gonzalez-Guzmán, 1967 (Fig. 7G)

Botanical affinity: family Rubiaceae, Psychotria/Alibertia (Leite 2006Leite FPR. 2006. Palinologia da Formação Solimões, Neógeno da Bacia do Solimões, estado do Amazonas: Implicação paleoambientais e bioestratigráficas. PhD Thesis, Universidade de Brasília, Brasília. )

Ecology: unknown

Genus Rhoipites Wodehouse 1933

Rhoipites guianensis (Van der Hammen & Wymstra 1964) Jaramillo & Dilcher 2001(Fig. 7H-I)

Botanical affinity: family Malvaceae, Firmiana/Hildegardia/Glossostemon/ Trichospermum (Germeraad et al 1968Germeraad JH, Hopping CA, Muller J. 1968. Palynology of Tertiary sediments from tropical areas. Review of Paleobotany and Palynology 6: 189-348.)

Ecology: unknown

Rhoipites toigoiD’Apolito 2016D’Apolito C. 2016. Landscape evolution in Western Amazonia: palynostratigraphy, palaeoenvironments and diversity of the Miocene Solimões formation, Brazil. PhD Thesis, University of Birmingham, Birmingham. (Fig. 7J)

Botanical affinity: family Rubiaceae?

Ecology: unknown

Discussion

This catalogue lists 60 taxa miospores present in the Miocene of the Brazilian Amazon, with photomicrographs and brief description of botanical affinity, ecology and distribution. This serves to support for paleoenvironmental and biostratigraphic studies for the region.

The assemblage of miospores is well preserved and well diversified. The spores are arranged in 16 genera and 19 species, included in ten families, with Pteridaceae the most representative family followed by Polypodiaceae and Cyatheaceae.

In Solimões Formation, the fern spores Crassoretitriletes vanhadshoovenii Magnastriatites grandiosus and Deltoidospora adriennis were recorded in almost all those previous studies. These species have habitats related to the aquatic environment as mangroves, swamps, rivers and lakes.

The spermatophytes group (pollen grains) encompasses two families of Gymnosperms: Aracauariaceae (Cyclusphaera scabrata) and Podocarpaceaeae (Podocarpidites). It is the second record of the family Araucariaceae of the Solimões Formation. And the Angiosperms are represented by 20 families, containing 31 genera and 41 species. The genus Bombacacidites and Echiperiporites exhibit the largest number of species.

The angiosperms species with numerous records in the Solimões Formation were Bombacacidites baculatus, Corsinipollenites oculusnoctis, Echiperiporites estelae, Echitricolporites spinosus, Grimsdalea magnaclavata, Mauritiidites franciscoi and Perisyncolporites pokornyi, which indicate water-related environments such as plains, mangroves, marshes and coast vegetation, except E. spinosus, typical of open vegetation.

Two new miospores were recorded for Solimões Formation: the fern spore Retitriletes sommeri and the pollen grain Echiperiporites scabrannulatus.

Acknowledgements

We express our thanks to the Geological Survey of Brazil (CPRM) for giving N.P. Sá the opportunity to study the material and the Brazilian National Council for Scientific and Technological Development (Conselho Nacional de Desenvolvimento Científico e Tecnológico - CNPq) for the scholarship and the financial support to N.P. Sá (Grant no. 140408/2013-4). We thank three anonymous reviewers for helpful suggestions.

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Publication Dates

  • Publication in this collection
    Oct-Dec 2017

History

  • Received
    27 Apr 2017
  • Accepted
    11 July 2017
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