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Ngorora Formation | |
---|---|
Stratigraphic range: Miocene | |
Type | Formation |
Underlies | Ngerngerwa Formation [1] |
Overlies | Tiim Formation |
Thickness | 400 m (type) |
Lithology | |
Primary | clay, clastic rock, tuff, silt, shale, sand [2] |
Location | |
Coordinates | 0°54′N35°48′E / 0.9°N 35.8°E |
Approximate paleocoordinates | 0°06′N34°18′E / 0.1°N 34.3°E |
Region | Rift Valley |
Country | Kenya |
Type section | |
Named for | Ngorora Administrative Location |
Named by | W.W. Bishop & G.R. Chapman |
Year defined | 1970 |
The Ngorora Formation is a geological formation in Kenya preserving fossils dating to the Miocene. The uppermost member of the formation shows sign of a faunal turnover that occurred around 11 to 10.5 million years ago, coinciding with faunal changes elsewhere in the world. This turnover includes the arrival of the horse Hipparion in East Africa. [1] The Ngorora Formation was initially mapped by G.R. Chapman in collaboration with the East African Geological Research Unit (EAGRU) and formally described by Bishop & Chapman in 1970. Major fossil finds were made in the early 1970s, with expeditions to the area recovering thousands of mammal, fish and mollusc remains alongside less common fossil material of birds and reptiles. [3] [2]
The formation is bordered to the west by the Elgeyo Escarpment, the east by the Laikipia Plateau and to the north by the Tiati volcanic center. To the south the formation is limited by the rising floor of the rift. During its deposition the formation contained two prominent upland areas, the topographic high of the Saimo Horst and Sidekh towards the north east, separated from the Saimo Horst by 8 km of lowland. The formation is roughly separated into four areas. Area I, the Kabarsero Type Area, split into Area Ia and Area Ib by the Kito Pass Fault; Area II west of the Cherial Fault, which includes the Tugen Hills, Kapkiamu Graben and Kaption Volcanic Complex; and Area III just south of the Saimo Horst. [2]
The basin the Ngorora Formation was deposited in is floored by the rocks of the underlying Tiim Formation and has seen repeated tectonic and volcanic activity around and during its deposition.
During the deposition of the Ngorora Formation the area shows several signs of volcanic activity. The Kaption volcano in Area II is likely responsible for much of the lahar and tuff found in Area I. The Laikipia Area and Tiati volcanic center likewise contributed to the volcanic material of the formation. [2]
The Ngorora Formation shows a great variety of environments and conditions throughout its stratigraphy. Mudcracks, Caliche, plant remains, bird footprints, channeling, signs of evaporation as well as various algae-based sediments all show signs of varying dry and wet conditions during the Miocene.
Member A preserves the bones of proboscideans and rhinos as well as the remains of reptiles and fish and represents an originally lacustrine environment with minor fluvial elements, all affected by lahas and other volcanic activity.
During the deposition of Member B Kaption Volcano was still active at irregular intervals. Member B shows signs of channeling caused by flowing water and flourishing plant growth (evidenced by root casts). At Kalimale weathering and plant growth were so extreme that all of the lapilli in a 45 cm thick layer was destroyed. The fauna of the member is of little use however, as the presence of channels means that animal material was likely derived from various localities over a great distance. Ruminant remains however have been used to derive an open or lightly wooded grassland habitat.
After increased volcanic and tectonic activity at the beginning of Member C's deposition, three lakes formed in various regions of the formation. At least Kabarsero Lake in Area Ia was freshwater, evidence of which can be found in the presence of diatoms and freshwater crabs. Kapkiamu Lake meanwhile was likely alkaline and inhabited by cichlids of the genus Oreochromis . [4] Similar conditions can be observed in the modern-day Lake Magadi, home to Alcolapia grahami . The rhythmic nature of the shale and clay deposits of Member C indicate seasonally fluctuating climate conditions, further supported by the growth rings of fossil wood. The two lakes were separated by 8 kilometers, which is not unusual given similar occurrences of freshwater and alkaline lakes in the modern day Rift Valley. The area between the lakes was covered by vigorously growing plant life, which lead to the creation of paleosol. The third lake west of Kaption Volcano was also freshwater.
Member D shows increased channeling indicative of rejuvenation through freshwater, which suggests a return of fluvial conditions as present in Member B. Also like in Member B, ruminants are used to infer an open or lightly wooded grassland environment in Area Ia. In Area Ib, ostracods, fish and crabs are all found in marginal lacustrine deposits at Kalimale. This lake underwent varying water levels and frequently dried up. [2]
One particular locality within the lower members (12.6 Ma) of the Ngorora Formation is interpreted to have been a submontaine to lowland rainforest environment preserved by the ash from a local volcanic eruption. The presence of mostly microphyllous (small sized, single veined) leaves and only one leptophyllous (long, slender) leaf indicate a moist to wet environment for the preserved forest habitat. Of the preserved plant fossils, 15% can be classified as herbs, 5% as herbs or shrubs, 12% lianas and 62% as shrubs or trees. Some bias towards herbaceous plants is present due to the preservation through ashfall and the preserved leaves of shrubs and trees are consistent with leaf fall that occurs in forests. The locality shows no signs of a present leaflitter, either due to decomposition following ashfall or due to the rapid decay of plant material in tropical, wet forest environments (in particular during the wet season, prior to increased leaf fall with the onset of the dry season). [5]
Color key
| Notes Uncertain or tentative taxa are in small text; |
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
Bellamya [2] | B. sp. | ||||
Lanistes [2] | L. sp. | ||||
Melanoides [2] | M. tuberculata | ||||
Mutela [2] | M. sp. | ||||
Pleiodon [2] | P. sp. | ||||
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
Annelidae indet. [2] | Member C Member D Member E | ||||
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
Candona [2] | C. sp. | ||||
Coleoptera indet. [2] | |||||
Diptera indet. [2] | |||||
Heterocypris ? [2] | H. sp.? | ||||
Isoptera indet. [2] | |||||
Lepidoptera indet. [2] | |||||
Limnicythere [2] | L. sp. | ||||
Metacypris [2] | M. sp. | ||||
Potamon [2] | C. sp. | ||||
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
cf. Clarias [2] | cf. C. sp. | Member D Member E | |||
Cyprinidae indet. [2] | Member C | ||||
Baringochromis [6] | B. senutae | Member E | more than a dozen skeletons | species flock of haplochromine cichlids | |
B. sonyii | Member E | five skeletons | |||
B. tallamae | Member E | several skeletons | |||
Oreochromis [4] | O. martyni | Member C | also known as "Sarotherodon" martyni, inhabitant of an alkaline lake | ||
Oreochromimos [7] | O. kabchorensis | Member C | several complete skeletons | oldest known member of the Oreochromini | |
Rebekkachromis [8] | P. kiptalami | Member D | a nearly complete skeleton | pseudocrenilabrine cichlid likely inhabiting alkaline lakes, possible species flock | |
P. ngororus | Member D | a nearly complete skeleton | |||
P. valyricus | Member C | a skeleton | |||
P. vancouveringae | Member C | a skeleton | |||
P. spp. | Member A Member C | a skeleton | |||
Tugenchromis [9] | T. pickfordi | Member E | partially complete skeleton | pseudocrenilabrine cichlid | |
Warilochromis [10] | W. unicuspidatus | Member E | a single skeleton | pseudocrenilabrine cichlid | |
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
Crocodylus [2] | C. sp. | Member A Member B Member C Member D Member E | |||
Ophidia indet. [2] | |||||
Pelusios [2] | P. cf. sinuatus | Member A Member B Member E | |||
Testudo [2] | T. sp. | Member D | |||
Trionyx [2] | T. sp. | Member B Member D Member E | |||
Varanidae indet. | Member B [2] Member D | ||||
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
Anhinga [11] | A. cf. pannonica | proximal end of the humerus | |||
Leptoptilos [12] | L. sp. | Member C | a partial skeleton composed mostly of limb bones | one of the oldest known marabou skeletons | |
Struthio [13] | S. sp. | Member C | limb bones | distinct from the roughly contemporary S. coppensi | |
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
Deinotherium [2] | D. bozasi | Member D | |||
Afrochoerodon [14] | A. ngorora | Member A Member D Member E | a choerolophodontine gomphothere | ||
Gomphotherium [15] | G. ngorora | Member A | An early gomphothere. | ||
Macroscelididae indet. [2] | an indetermined elephant shrew | ||||
Myorycteropus [16] | M. chemeldoi | Member B | a type of aardvark | ||
Parapliohyrax [17] | P. ngororaensis | Member B Member C Member D Member E | a type of hyrax | ||
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
Albanohyus [18] | A. cf. castellensis | skull without teeth | a possible ancestor of Cainochoerus | ||
Anthracotheriidae indet. [16] | |||||
Climacoceras [16] | C. gentryi | a giraffid | |||
Cephalophini? indet. [2] | an indetermined species of duiker | ||||
Dorcatherium [16] | D. sp. | a genus of mouse deer | |||
Gazella [2] | G. sp. | ||||
Homoiodorcas [19] | H. tugenicum | ||||
Kenyapotamus [20] [21] | K. sp. | Member D Member E | molars | the possible ancestor of the modern hippos | |
Kipsigicerus [19] | K. labidotus | a close relative of the Four-horned antelope | |||
Lagomerycidae indet. [2] | |||||
Listriodon [22] | L. bartulensis | Member A | mandible and teeth | the molars of this species are notably smaller than that of Eurasian taxa | |
Lopholistriodon [22] | L. kidogosana | Member B Member C Member D | skull and teeth as well as a fragment of a mandibular symphysis | Lopholistriodon marks another decrease in size within the African listriodontine lineage | |
"Palaeotragus" [23] | "P. primaevus" | a potential new genus and species in need of revision | |||
Protoryx [19] | P. sp. | ||||
Pseudotragus ? [16] | P.? gentryi | ||||
Samotherium ? [2] | S. sp. | a genus of giraffid | |||
Sivoreas [24] | S. eremita | Member A Member C Member D | horn cores | a boselaphine bovid | |
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
Amphicyonidae indet. [25] | molar | ||||
Dissopsalis [26] | D. pyroclasticus | an incomplete first or second molar | A genus of teratodontine hyaenodontid. | ||
Eomellivora [27] | E. tugenensis | Member D | a broken snout | a relative of the modern honey badger of similar size | |
Herpestidae indet. [27] | Member A | a right mandible | an indetermined mongoose | ||
Megistotherium [27] | M. osteothlastes | Member A Member D | a damaged molar and distal end of a humerus | the youngest known remains of the genus | |
Myacyon [28] | M. kiptalami | Member D | a snout broken behind the second molar | a species as large or slightly larger than an African Lion, originally considered to belong to the genus Agnotherium [27] | |
Percrocuta [27] | P. tobieni | Member B Member D Member E | a left mandible fragment | a lioness-sized genus of percrocutids or true hyaenas | |
Tugenictis [27] | T. ngororaensis | Member A | a right molar | a genus of viverrid similar in size to the African Civet | |
Vishnuonyx [27] | V. chinjiensis | Member D | a premolar | a genus of otter | |
Viverridae indet. [27] | Member B | a mandible with fragments of the premolars | the morphology resembles the genus Genetta more than it does Viverra and is slightly larger | ||
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
Aceratherium / Dicerorhinus [2] | |||||
Brachypotherium [29] | B. sp. | although the genus was reported, no detailed description or figures were given, rendering a more detailed assignment not possible | |||
Chilotheridium [30] | C. sp. | Member E | a maxillary fragment including several teeth | originally described as C. pattersoni, subsequent research showed the fossil is not well preserved enough for such an assignment | |
Hipparion [1] | H. sp. | Member E | tooth fragments and other remains | dated to 11 to 10.5 Ma, the fossils at Ngorora indicate a rapid dispersal of the genus throughout Africa and Eurasia | |
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
Catarrhini indet. | canine | possible hominoid clearly distinct from Proconsul [16] | |||
Hominoidea indet. | Member C | incisor and premolar | a large hominoid similar to Proconsul or Equatorius [16] | ||
Microcolobus | M. tugenensis | a colombine monkey. | |||
Victoriapithecus | V. sp. | Member B Member C | various teeth | possibly a new species of the genus [16] | |
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
Cricetidae indet. A [2] | |||||
Cricetidae indet. B [2] | |||||
Dendromurinae indet. [2] | |||||
Pedetidae? [2] | Member B | ||||
Phiomyidae [2] | |||||
cf. Vulcanisciurus [31] | cf. Vulcanisciurus sp. | A genus of squirrel. | |||
Name | Species | Member | Material | Notes | Image |
---|---|---|---|---|---|
Acalypha [5] | A. sp. | a type of herb/shrub | |||
Acanthaceae [5] | |||||
Artabotrys [5] | A. sp. | a type of shrub | |||
Bignoniaceae [5] | |||||
cf. Cola [5] | cf. C. sp. | a species of the tree canopy | |||
Dioscorea [5] | D. sp. | a liana | |||
Graminae [5] | a type of grass | ||||
Icacinaceae [5] | |||||
Lasiodiscus [5] | L. sp. | an understory taxon | |||
Loganiaceae/Melastomataceae [5] | |||||
Menispermaceae [5] | |||||
Myrtaceae [5] | |||||
Mystroxylon [5] | M. sp. | a type of shrub/tree | |||
Olacaceae [5] | |||||
Pollia | P. tugenensis [32] | stems, leaves and fruit | a dominant plant of the herbaceous layer, Pollia tugenensis likely grew in clusters | ||
Rauvolfia [5] | R. sp. | a tree or shrub | |||
Rubiaceae [5] | |||||
Rutaceae [5] | |||||
Sapindaceae [5] | |||||
cf. Sapium [5] | cf. S. sp. | a type of milkree | |||
cf. Sapotaceae [5] | |||||
Tiliaceae [5] | |||||
Violaceae [5] | |||||
cf. Zizyphus [5] | cf. Z. sp. | a spiny shrub/tree of the buckthorn family | |||
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