6533b82dfe1ef96bd1291d73
RESEARCH PRODUCT
Macrofossil evidence of Late Holocene presence of Aldrovanda vesiculosa L. in Central-Eastern Europe (Poland) and East Africa (Tanzania)
David WilliamsonCatherine Aloyce MasaoAmos MajuleMariusz GałkaMariusz GałkaArnaud HuguetArnaud HuguetLaurent Bergonzinisubject
0106 biological sciences010506 paleontologyPeatCarnivorous plant[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010603 evolutionary biology01 natural sciencesAldrovanda vesiculosaBogHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesgeographyEemiangeography.geographical_feature_categorySubfossilHolocenebiologyEcologyPeatMacrofossilPlant macrofossilbiology.organism_classificationWaterwheel plantInterglacialGeologydescription
International audience; To date, the seeds of waterwheel plant (Aldrovanda vesiculosa) were only found in Europe, in sediments of the Eemian and Mazovian Interglacials. The absence of A. vesiculosa seeds in European Holocene deposits is probably due to unfavorable climatic conditions, i.e. lower temperature, during this period: in temperate zones, A. vesiculosa reproduces mainly in a vegetative way; it rarely blooms and only occasionally produces seeds. In this paper, subfossil seeds of A. vesiculosa were identified in two peat bogs: one (Sucha Kobyła) in SE Poland and another one (Kyambangunguru) in SW Tanzania. Single seeds of this plant were found in a peat layer from the Polish site formed after 1600 AD as well as in sediments accumulated around 440 AD in the Tanzanian one. To our knowledge, this is the first time that seeds of A. vesiculosa are found in Holocene deposits in the world. Our findings provide new data on the distribution of A. vesiculosa over the Late Holocene.Keywords
| year | journal | country | edition | language |
|---|---|---|---|---|
| 2015-11-01 |