2006
DOI: 10.1016/j.palaeo.2005.07.002
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Millennial-scale climatic cycles in the Early Pliocene pollen record of Ptolemais, northern Greece

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Cited by 31 publications
(17 citation statements)
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“…In older records, the heliomagnetic origin is inferred from the correspondence in time between the recorded period and an ~2.4 k.y. period in the Pliocene (Kloosterboer-van Hoeve et al, 2006), Miocene (Kern et al, 2013), Eocene (Lenz et al, 2017), Permian (Franco et al, 2012), and Devonian (this work; Elrick and Hinnov, 2007).…”
Section: Discussionmentioning
confidence: 71%
“…In older records, the heliomagnetic origin is inferred from the correspondence in time between the recorded period and an ~2.4 k.y. period in the Pliocene (Kloosterboer-van Hoeve et al, 2006), Miocene (Kern et al, 2013), Eocene (Lenz et al, 2017), Permian (Franco et al, 2012), and Devonian (this work; Elrick and Hinnov, 2007).…”
Section: Discussionmentioning
confidence: 71%
“…There has been much geological evidence of millennium-scale cycles, from North America to Europe and from the Middle East to East Asia. A 1500 a cycle was found in deep-sea sediment records for the North Atlantic [3], lake sediment records for Alaska [1], pollen records for the Ptolemais basin, Greece [38], loess records for Jiuzhoutai, China [39] and sea surface temperature records for the North Pacific at mid-latitudes [40]. 1450 and 1150 a cycles were detected for the 74K1 hole in the Arabian Sea [41].…”
Section: Periodicity Of Temperature Variationmentioning
confidence: 99%
“…Anatolinites dongyingensis (Ke & Shi, 1978) Elsik et al, 1990 Brachysporisporites catinus (Elsik & Jansonius, 1974) Kalgutkar & Jansonius, 2000Dicellaesporites inaequabilis Martínez-Hernández & Tomasini-Ortiz, 1989 Dicellaesporites keralensis Kumar, 1990Dictyosporites morularis (Salard-Cheboldaeff & Locquin, 1980) Kalgutkar & Jansonius, 2000Dictyosporites moruloides (Salard-Cheboldaeff & Locquin, 1980 Kalgutkar & Jansonius, 2000 Dyadosporites bhardwaji (Varma & Rawat, 1963) Kalgutkar & Jansonius, 2000 Dyadosporites reticulatus (Ramanujam & Rao, 1979) Kalgutkar & Jansonius, 2000Dyadosporites solidus (Ke & Shi, 1978) Song in Song et al, 1999 Exesisporites annulatus Kalgutkar, 1993 Exesisporites neogenicus Elsik, 1969Inapertisporites circularis (Sheffy & Dilcher, 1971) Kalgutkar & Jansonius, 2000Inapertisporites communis Song & Li in Song et al, 1989 Meliolinites nivalis Selkirk, 1975Monoporisporites macrosporus (Salard-Cheboldaeff & Locquin, 1980 Kalgutkar & Jansonius, 2000 Monoporisporites traversii (Ediger & Alisan, 1989) Kalgutkar & Jansonius, 2000Palaeoamphisphaerella pirozynskii Ramanujam & Srisailam, 1980 Papulosporonites enormis (Ediger, 1981) Kalgutkar & Jansonius, 2000 Paragranatisporites vermiculus (Ediger, 1981 remains is interpreted as an indication of the prevalence of a humid climate in the area of deposition (Singh & Chauhan, 2008). In addition, changes in diversity and relative abundance of fungal palynomorphs can reflect palaeoclimatic as well as other palaeoenvironmental changes/fluctuations (Elsik, 1996;Kloosterboer-van Hoeve et al, 2006).…”
Section: Palaeoenvironmental Interpretationmentioning
confidence: 99%