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Titlebook: Neogene Paleontology of the Manonga Valley, Tanzania; A Window into the Ev Terry Harrison Book 1997 Springer Science+Business Media New Yor

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Fossil Suids from the Manonga Valley, Tanzania,ered 65 suid specimens from ten sites (Table I). Fossils suids derive from horizons throughout the Wembere-Manonga Formation, although the majority were recovered from the Ibole Member (Harrison 1991, 1993, 1994; Harrison and Verniers, 1993; Harrison .., 1993; Haileab and Harrison, 1993; Mbago .., 1
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Later Neogene Hipparions from the Manonga Valley, Tanzania,Pliocene (Harrison, 1991, 1993; Harrison .., 1993; Harrison and Verniers, 1993; Verniers, this volume, Chapter 2; Harrison and Baker, this volume, Chapter 13). Fossil mammals were first recorded in the Manonga Valley during the 1920s and 1930s (Stockley, 1929; Grace and Stockley, 1930; Williams and
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Fossil Proboscidea from the Wembere-Manonga Formation, Manonga Valley, Tanzania,and possibly . from fossil localities in the Manonga Valley, north-central Tanzania. The inferred age of these localities is late Miocene-early Pliocene (see below). African proboscideans underwent rapid morphological transformation and taxonomic diversification during and subsequent to the late Ter
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