Am. J. Bot. Cross-Journal Searching
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Submit a response
Right arrow Alert me when this article is cited
Right arrow Alert me when eLetters are posted
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (15)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Herendeen, P. S.
Right arrow Articles by Jacobs, B. F.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Herendeen, P. S.
Right arrow Articles by Jacobs, B. F.
Agricola
Right arrow Articles by Herendeen, P. S.
Right arrow Articles by Jacobs, B. F.
(American Journal of Botany. 2000;87:1358-1366.)
© 2000 Botanical Society of America, Inc.

Fossil legumes from the Middle Eocene (46.0 Ma) Mahenge Flora of Singida, Tanzania1

Patrick S. Herendeen1 and Bonnie F. Jacobs1

1 Department of Biological Sciences, The George Washington University, 2023 G Street NW, Washington, DC 20052 USA; and Department of Geological Sciences, P.O. Box 750395, Southern Methodist University, Dallas, Texas 75275-0395 USA

Middle Eocene age caesalpinioid and mimosoid legume leaves are reported from the Mahenge site in north-central Tanzania. The Mahenge flora complements a sparse Paleogene tropical African fossil plant record, which until now consisted of a single macrobotanical assemblage, limited palynological studies in West Africa and Egypt, and fossil wood studies primarily from poorly dated deposits. Mahenge leaf macrofossils have the potential to add significantly to what is known of the evolutionary history of extant African plant groups and to expand our currently limited knowledge of African Paleogene environments. The site is associated with a kimberlite eruption and demonstrates the potential value of kimberlite-associated lake deposits as much-needed resources for African Paleogene floras. In this report we document a relatively diverse component of the flora consisting of the leaves of at least five species of Leguminosae. A new species of the extant genus Acacia (Mimosoideae), described herein, is represented by a bipinnate leaf. Another taxon is described as a new species of the extant genus Aphanocalyx (Caesalpinioideae), and a third leaf type may be related to the extant genus Cynometra (Caesalpinioideae). Two additional leaf types are less well understood: one appears to be referable to the Caesalpinioideae and subfamily affinities of the other taxon are unknown.

Key Words: Caesalpinioideae • Eocene • Leguminosae • Mimosoideae • paleobotany • Paleogene • Tanzania




This article has been cited by other articles:


Home page
ScienceHome page
P. Wilf, N. R. Cuneo, K. R. Johnson, J. F. Hicks, S. L. Wing, and J. D. Obradovich
High Plant Diversity in Eocene South America: Evidence from Patagonia
Science, April 4, 2003; 300(5616): 122 - 125.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2000 by the Botanical Society of America, Inc.