2018
DOI: 10.2478/acpa-2018-0001
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Groenlandia pescheri sp. nov. (Potamogetonaceae) from the Late Oligocene Fossil-Lagerstätte Enspel (Westerwald, Germany)

Abstract: The new species Groenlandia pescheri D. Uhl & Poschmann sp. nov., belonging to the family Potamogetonaceae, is described from the Late Oligocene Fossil-Lagerstätte Enspel (Westerwald, Germany). The species is characterized by sub-oppositely arranged leaves without observable stipule-like appendages at the leaf bases and a very thin exocarp (both characteristics of the aquatic genus Groenlandia J. Gay) with a spiked crest (which differs from the only other species included in this genus, the modern Groenlan… Show more

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Cited by 9 publications
(21 citation statements)
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“…The existence of such zones is furthermore indicated by the occurrence of e.g., crocodiles (Frey & Monninger, 2010), relatively abundant caddisfly larvae (Poschmann, 2006), and the well preserved macroflora (Köhler & uhl, 2014). For example, the aquatic plant Groenlandia has its richest occurrence at the base of layer S14 (uhl & Poschmann, 2018) just as the (gomphid) dragonfly larvae. Assuming that these larvae lived in these vegetation-rich, shallow-water zones furthermore explains their rareness as fossils, because the vegetation may form a kind of taphonomic filter by preventing dead larvae or exuviae from entering the open lake and eventually from reaching the anoxic lake bottom where they could be finally buried and subsequently fossilized (cf., Wuttke & Poschmann, 2010).…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…The existence of such zones is furthermore indicated by the occurrence of e.g., crocodiles (Frey & Monninger, 2010), relatively abundant caddisfly larvae (Poschmann, 2006), and the well preserved macroflora (Köhler & uhl, 2014). For example, the aquatic plant Groenlandia has its richest occurrence at the base of layer S14 (uhl & Poschmann, 2018) just as the (gomphid) dragonfly larvae. Assuming that these larvae lived in these vegetation-rich, shallow-water zones furthermore explains their rareness as fossils, because the vegetation may form a kind of taphonomic filter by preventing dead larvae or exuviae from entering the open lake and eventually from reaching the anoxic lake bottom where they could be finally buried and subsequently fossilized (cf., Wuttke & Poschmann, 2010).…”
Section: Discussionmentioning
confidence: 99%
“…2). However, this is probably due to favourable preservational factors present in the basal layer of S14 (Poschmann & Wedmann, 2005;uhl & Poschmann, 2018), which yielded at least 28 specimens (for some, the exact position within S14 has not been recorded).…”
Section: Methodsmentioning
confidence: 99%
“…These include physiological‐biochemical parameters (such as q ) as well as environmental parameters. Information on leaf size indicating ranges of characteristic leaf length l c can be obtained from available data based on the fossil record (Uhl et al., 2007; West et al., 2015). Biochemical parameters have to be borrowed from ecologically representative relatives.…”
Section: Methodsmentioning
confidence: 99%
“…Frankenhäuser and Wilde 1993;Wilde andFrankenhäuser 1993, 1998), as well as the late Oligocene maar lakes of Enspel (e.g. Köhler and Uhl 2014;Uhl 2015;Uhl and Poschmann 2018), Rott (e.g. Mosbrugger 1996;Winterscheid et al 2018), and Kleinsaubernitz (e.g.…”
Section: Introductionmentioning
confidence: 99%