2014
DOI: 10.1080/08912963.2014.933212
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Non-pollen palynomorphs from the late Quaternary sediments of southwestern Madhya Pradesh (India) and their palaeoenvironmental implications

Abstract: Non-pollen palynomorphs comprising algal remains, namely Botryococcus, Chara, Concentricystis, Pediastrum, Spirogyra and Zygnema as well as fungal spores such as ascospore types, Alternaria, Cookeina, Curvularia, Diplodia, Glomus, Helminthosporium, Nigrospora, Microthyriaceae and Tetraploa, well identified from the palynoslides prepared basically for the study of palaeovegetational succession and palaeoclimatic reconstructions, are discussed and illustrated from the late Quaternary sediments collected from sou… Show more

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Cited by 26 publications
(9 citation statements)
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“…This period (~1550–800 cal. yr BP) begins with a remarkable wide deforestation event, which led to a major expansion of grasslands, likely related to a drier climate, but also to an increase of temperature, as suggested by open water indicators (Cook et al, 2011; Quamar, 2015; Van Geel, 2001). They also point to an increasing seasonality against the more continuous water availability indicated by aquatic taxa (Amami et al, 2010; Oertli et al, 2010).…”
Section: Discussionmentioning
confidence: 99%
“…This period (~1550–800 cal. yr BP) begins with a remarkable wide deforestation event, which led to a major expansion of grasslands, likely related to a drier climate, but also to an increase of temperature, as suggested by open water indicators (Cook et al, 2011; Quamar, 2015; Van Geel, 2001). They also point to an increasing seasonality against the more continuous water availability indicated by aquatic taxa (Amami et al, 2010; Oertli et al, 2010).…”
Section: Discussionmentioning
confidence: 99%
“…Identification of modern palynomorphs recovered from the surface soil, mud and moss-cushion samples was carried out through the consultation of reference slides available in the sporothek of Birbal Sahni Institute of Palaeobotany (BSIP), Lucknow, and the scant published literature related to pollen and non-pollen palynomorph study (Chauhan & Bera 1990;Nayar 1990;Bera et al 2009;Quamar 2014). Betweem 280 to 316 pollen grains were counted in each sample.…”
Section: Methodsmentioning
confidence: 99%
“…The high percentages of Glomus may indicate local soil erosion (Medeanic and Silva, 2010). The presence of Glomus, Diplodia, Curvularia, Tetraploa, Nigrospora, Cookeina, Alternaria and Helminthosporium reflects warm and humid climate around the study areas (Quamar, 2015).…”
Section: Discussion Inferences On the Modern Pollen Rain-vegetation Relationshipmentioning
confidence: 98%