TY - JOUR
T1 - An unusual occurrence of the trace fossil Vagorichnus preserved in hydrothermal silica at Lake Baringo, Kenya Rift Valley
T2 - Taphonomic and paleoenvironmental significance
AU - Buatois, Luis A.
AU - Renaut, Robin W.
AU - Scott, Jennifer J.
AU - Owen, R Bernhart
N1 - Funding Information:
We thank Caroline Le Turdu and Jean-Jacques Tiercelin (then at Universit? de Bretagne Occidentale), who first noticed these rare trace fossils during our visit in 1996. Our research was funded by the Natural Sciences and Engineering Research Council of Canada (NSERC to LAB: grant 311726-13; RWR: grant GP629) and the Hong Kong Research Grants Council (to RBO: grant HKBU12300815). This research was authorised by many permits from the Office of the President and Ministry of Science and Technology, Government of Kenya. We especially thank William Kimosop (Chief Warden, North Kenya Rift) and his staff for their continuing support, and the local community at Kampi-ya-Samaki at Lake Baringo, who welcomed us and gave valuable local knowledge. We thank Dirk Verschuren (U. Gent) for his helpful comments in interpreting the possible trace maker but we accept responsibility for errors. RWR thanks Julian Andrews and the School of Environmental Sciences, University of East Anglia, for their help with this study. Nic Minter, Sebastian Voigt and two anonymous reviewers provided very useful feedback.
Funding Information:
We thank Caroline Le Turdu and Jean-Jacques Tiercelin (then at Université de Bretagne Occidentale), who first noticed these rare trace fossils during our visit in 1996. Our research was funded by the Natural Sciences and Engineering Research Council of Canada (NSERC to LAB: grant 311726-13 ; RWR: grant GP629 ) and the Hong Kong Research Grants Council (to RBO: grant HKBU12300815 ). This research was authorised by many permits from the Office of the President and Ministry of Science and Technology, Government of Kenya. We especially thank William Kimosop (Chief Warden, North Kenya Rift) and his staff for their continuing support, and the local community at Kampi-ya-Samaki at Lake Baringo, who welcomed us and gave valuable local knowledge. We thank Dirk Verschuren (U. Gent) for his helpful comments in interpreting the possible trace maker but we accept responsibility for errors. RWR thanks Julian Andrews and the School of Environmental Sciences, University of East Anglia, for their help with this study. Nic Minter, Sebastian Voigt and two anonymous reviewers provided very useful feedback.
PY - 2017/11/1
Y1 - 2017/11/1
N2 - An unusual occurrence of the ichnogenus Vagorichnus is documented in the sublacustrine hydrothermal silica cement of conglomerate at Lake Baringo in the central Kenya Rift. The outcrop with ichnofossils lies at Soro on the NE shoreline of Ol Kokwe island, a Pleistocene volcanic centre in Lake Baringo. There, onshore and offshore hot-springs discharge hot and boiling (83–97.5 °C), alkaline Na-HCO3 water, steam and volcanic gases (mainly CO2). The ichnofossils are preserved in full relief in diatomaceous opaline silica cement precipitated between immature gravel clasts. The trace fossils comprise horizontal and subhorizontal burrow-systems with straight, curved, and loosely meandering segments, which locally show poorly defined constrictions. The preserved features are diagnostic of the ichnospecies Vagorichnus anyao. Vagorichnus, a feeding structure (fodinichnion), may have been produced by insect larvae (Diptera, Coleoptera or other insects), which are common in modern East African lakes including Lake Baringo. A probable body fossil of a Diptera larva is preserved in one of the burrows. Hydrothermal silica is an unlikely host for macroscale ichnofossils, but the soft silica that precipitated near hot-spring vents on the shallow gravelly lake-floor was cool enough for colonisation by microbes and higher organisms. The trace-makers burrowed into cohesive, but still soft, silica; the trace fossils are therefore bioturbation structures rather than bioerosion structures. The soft silica contained organic matter from phytoplankton and detrital plant debris, and was locally covered by benthic microbial mats, all of which were potential food sources for the burrowers. The presence of Vagorichnus near modern and former hot springs confirms the broad ecological, hydrological and environmental conditions represented by this ichnogenus, and shows that Vagorichnus is not restricted to a specific environment, substrate, or type of lake basin.
AB - An unusual occurrence of the ichnogenus Vagorichnus is documented in the sublacustrine hydrothermal silica cement of conglomerate at Lake Baringo in the central Kenya Rift. The outcrop with ichnofossils lies at Soro on the NE shoreline of Ol Kokwe island, a Pleistocene volcanic centre in Lake Baringo. There, onshore and offshore hot-springs discharge hot and boiling (83–97.5 °C), alkaline Na-HCO3 water, steam and volcanic gases (mainly CO2). The ichnofossils are preserved in full relief in diatomaceous opaline silica cement precipitated between immature gravel clasts. The trace fossils comprise horizontal and subhorizontal burrow-systems with straight, curved, and loosely meandering segments, which locally show poorly defined constrictions. The preserved features are diagnostic of the ichnospecies Vagorichnus anyao. Vagorichnus, a feeding structure (fodinichnion), may have been produced by insect larvae (Diptera, Coleoptera or other insects), which are common in modern East African lakes including Lake Baringo. A probable body fossil of a Diptera larva is preserved in one of the burrows. Hydrothermal silica is an unlikely host for macroscale ichnofossils, but the soft silica that precipitated near hot-spring vents on the shallow gravelly lake-floor was cool enough for colonisation by microbes and higher organisms. The trace-makers burrowed into cohesive, but still soft, silica; the trace fossils are therefore bioturbation structures rather than bioerosion structures. The soft silica contained organic matter from phytoplankton and detrital plant debris, and was locally covered by benthic microbial mats, all of which were potential food sources for the burrowers. The presence of Vagorichnus near modern and former hot springs confirms the broad ecological, hydrological and environmental conditions represented by this ichnogenus, and shows that Vagorichnus is not restricted to a specific environment, substrate, or type of lake basin.
KW - Continental rift
KW - Hot springs
KW - Ichnology
KW - Insects
KW - Lacustrine
KW - Opaline silica
UR - http://www.scopus.com/inward/record.url?scp=85027228047&partnerID=8YFLogxK
U2 - 10.1016/j.palaeo.2017.08.002
DO - 10.1016/j.palaeo.2017.08.002
M3 - Journal article
AN - SCOPUS:85027228047
SN - 0031-0182
VL - 485
SP - 843
EP - 853
JO - Palaeogeography, Palaeoclimatology, Palaeoecology
JF - Palaeogeography, Palaeoclimatology, Palaeoecology
ER -