Sclerosperma fossils from the late Oligocene of Chilga, north-western Ethiopia. Issue 2 (4th March 2019)

• Record Type: Journal Article
• Authors: Grímsson, Friðgeir; Jacobs, Bonnie F.; Van Valkenburg, Johan L. C. H.; Wieringa, Jan J.; Xafis, Alexandros; Tabor, Neil; Pan, Aaron D.; Zetter, Reinhard
• Is Part Of: Grana. Volume 58:Issue 2(2019)
• Page Start: 81
• Page End: 98
• Publication Date: 2019-03-04
• Subjects: Arecaceae -- palm leaf -- light microscopy -- palaeovegetation -- palms -- pollen morphology -- rainforest -- scanning electron microscopy -- swamp element; Palynology -- Periodicals; 571.8452
• DOI: 10.1080/00173134.2018.1510977
• Languages: English
• ISSNs: 0017-3134

Abstract

Abstract: The palm family, Arecaceae, is notoriously depauperate in Africa today, and its evolutionary, paleobiogeographic, and extinction history there are not well documented by fossils. In this article we report the pollen of two new extinct species of the small genus, Sclerosperma (Arecoideae), from a late Oligocene (27–28 Ma) stratum exposed along the Guang River in Chilga Wereda of north-western Ethiopia. The pollen are triporate, and the two taxa can be distinguished from each other and from modern species using a combination of light and scanning electron microscopy, which reveals variations in the finer details of their reticulate to perforate exine sculpture. We also report a palm leaf fragment from a stratum higher in the same section that is in the Arecoideae subfamily, and most likely belongs to Sclerosperma . The implications of these discoveries for the evolutionary history of this clade of African arecoid palms is that their diversification was well underway by the middle to late Oligocene, and they were much more widespread in Africa at that time than they are now, limited to West and Central Africa. Sclerosperma exhibits ecological conservatism, as today it occurs primarily in swamps and flooded forests, and the sedimentology of the Guang River deposits at Chilga indicate a heterogeneous landscape with a high water table. The matrix containing the fossil pollen is lignite, which itself indicates standing water, and a variety of plant macrofossils from higher in the section have been interpreted as representing moist tropical forest or seasonally inundated forest communities.