An international and multidisciplinary drilling project into a young complex impact structure: The 2004 ICDP Bosumtwi Crater Drilling Project—An overview

Abstract— The Bosumtwi impact crater in Ghana, arguably the best‐preserved complex young impact structure known on Earth, displays a pronounced rim and is almost completely filled by Lake Bosumtwi, a hydrologically closed basin. It is the source crater of the Ivory Coast tektites. The structure was excavated in 2.1–2.2 Gyr old metasediments and metavolcanics of the Birimian Supergroup. A drilling project was conceived that would combine two major scientific interests in this crater: 1) to obtain a complete paleoenvironmental record from the time of crater formation about one million years ago, at a near‐equatorial location in Africa for which very few data are available so far, and 2) to obtain a complete record of impactites at the central uplift and in the crater moat, for ground truthing and comparison with other structures.

[1]  C. Koeberl,et al.  Detailed structural analysis of the rim of a large, complex impact crater: Bosumtwi Crater, Ghana , 1998 .

[2]  M. Talbot,et al.  Holocene variations in the level of Lake Bosumtwi, Ghana , 1977, Nature.

[3]  R. Grieve,et al.  Classification and Nomenclature of Impact Metamorphic Rocks: A Proposal to the IUGS Subcommission on the Systematics of Metamorphic Rocks , 1994 .

[4]  M. Cintala,et al.  An analysis of differential impact melt‐crater scaling and implications for the terrestrial impact record , 1992 .

[5]  Donald W. Davis,et al.  UPb age constraints on deposition and provenance of Birimian and gold-bearing Tarkwaian sediments in Ghana, West Africa , 1994 .

[6]  G. Wagner,et al.  New K-Ar and fission track ages of impact glasses and tektites , 1967 .

[7]  J. Garvin,et al.  The Zhamanshin impact feature: A new class of complex crater? , 1992 .

[8]  C. Koeberl,et al.  The Lake Bosumtwi impact structure in Ghana: A brief environmental assessment and discussion of ecotourism potential , 2007 .

[9]  J. Overpeck,et al.  The 2004 ICDP Bosumtwi Impact Crater, Ghana, West Africa, Drilling Project: A First Report , 2005 .

[10]  A. Goresy Metallic spherules in Bosumtwi crater glasses , 1966 .

[11]  R. Wagner,et al.  Bosumtwi Impact Crater, Ghana: A Remote Sensing Investigation , 2002 .

[12]  D. Davis,et al.  Reassessment of Proterozoic granitoid ages in Ghana on the basis of U/Pb zircon and monazite dating , 1992 .

[13]  T. Elbra,et al.  Characterization of the log lithology of cores LB‐07A and LB‐08A of the Bosumtwi impact structure by using the anisotropy of magnetic susceptibility , 2007 .

[14]  B. Glass Glassy Objects (Microtektites?) from Deep-Sea Sediments near the Ivory Coast , 1968, Science.

[15]  D. Stöffler Glasses formed by hypervelocity impact , 1984 .

[16]  H. Newsom,et al.  Hydrothermal alteration in the Bosumtwi impact structure: Evidence from 2M1‐muscovite, alteration veins, and fracture fillings , 2007 .

[17]  J. Overpeck,et al.  A magnetic mineral record of Late Quaternary tropical climate variability from Lake Bosumtwi, Ghana , 2004 .

[18]  H. Rohleder Lake Bosumtwi, Ashanti , 1936 .

[19]  J. Melack,et al.  Preliminary results from sediment cores from lake Bosumtwi, Ghana , 1984 .

[20]  Vladimir V. Shuvalov,et al.  3D hydrodynamic code sova for multimaterial flows, application to Shoemakerlevy 9 comet impact problem , 1999 .

[21]  K. Brooks,et al.  Pronounced central uplift identified in the Bosumtwi impact structure, Ghana, using multichannel seismic reflection data , 2002 .

[22]  David A. Hastings,et al.  The Lake Bosumtwi impact crater, Ghana , 1981 .

[23]  Gareth S. Collins,et al.  A strain-based porosity model for use in hydrocode simulations of impacts and implications for transient crater growth in porous targets , 2006 .

[24]  W. B. Jones,et al.  Chemical analyses of Bosumtwi crater target rocks compared with the Ivory Coast tektites , 1985 .

[25]  J. Saul,et al.  RbSr study on country rocks of the Bosumtwi crater, Ghana , 1967 .

[26]  J. Overpeck,et al.  Paleoclimatic variations in West Africa from a record of late Pleistocene and Holocene lake level stands of Lake Bosumtwi, Ghana , 2006 .

[27]  C. Koeberl,et al.  Bosumtwi impact structure, Ghana: Geochemistry of impactites and target rocks, and search for a meteoritic component , 2005 .

[28]  C. Schnetzler,et al.  Rubidium-Strontium Age of the Bosumtwi Crater Area, Ghana, Compared with the Age of the Ivory Coast Tektites , 1966, Science.

[29]  G. Wasserburg,et al.  Age and provenance of the target materials for tektites and possible impactites as inferred from Sm-Nd and Rb-Sr systematics , 1982 .

[30]  R. P. Lyons,et al.  Structure and morphology of the Bosumtwi impact structure from seismic reflection data , 2007 .

[31]  C. Koeberl,et al.  Beryllium-10 concentrations of tektites from the Ivory Coast and from Central Europe: Evidence for near-surface residence of precursor materials , 2007 .

[32]  R. Dietz,et al.  Coesite from the Lake Bosumtwi Crater, Ashanti, Ghana , 1977 .

[33]  H. H. Thomas,et al.  Rare-earth and barium abundances in Ivory Coast tektites and rocks from the Bosumtwi Crater area, Ghana , 1967 .

[34]  M. Talbot,et al.  Mid-holocene climate change in Lake Bosumtwi, Ghana , 2003, Quaternary Research.

[35]  O. Müller,et al.  Notizen: Das Kalium-Argon-Alter des Bosumtwi-Kraters in Ghana und die chemische Beschaffenheit seiner Gläser , 1964 .

[36]  M. Maclaren Lake Bosumtwi, Ashanti , 1931 .

[37]  J. Overpeck,et al.  The ICDP Lake Bosumtwi Drilling Project: A First Report , 2005 .

[38]  M. Talbot,et al.  A new late Pleistocene-Holocene water-level curve for Lake Bosumtwi, Ghana [Earth Planet. Sci. Lett. 47 (1980) 336-344. , 1980 .

[39]  C. Koeberl,et al.  Lithostratigraphic and petrographic analysis of ICDP drill core LB‐07A, Bosumtwi impact structure, Ghana , 2007 .

[40]  M. Swaine,et al.  An early holocene leaf flora from Lake Bosumtwi, Ghana , 1978 .

[41]  C. Guerrot,et al.  The paleoproterozoic Ghanaian province: Geodynamic model and ore controls, including regional stress modeling , 2006 .

[42]  J. Erzinger,et al.  Platinum group elements provide no indication of a meteoritic component in ICDP cores from the Bosumtwi crater, Ghana , 2007 .

[43]  D. Kent,et al.  Ivory Coast microtektite strewn field: description and relation to the Jaramillo geomagnetic event , 1991 .

[44]  C. Koeberl,et al.  Detection of a Meteoritic Component in Ivory Coast Tektites with Rhenium-Osmium Isotopes , 1993, Science.

[45]  A. Kontny,et al.  Petrography and shock‐related remagnetization of pyrrhotite in drill cores from the Bosumtwi Impact Crater Drilling Project, Ghana , 2007 .

[46]  N. Artemieva Tektite Origin in Oblique Impacts: Numerical Modeling of the Initial Stage , 2002 .

[47]  A. Deutsch,et al.  The ICDP Lake Bosumtwi impact crater scientific drilling project (Ghana): Core LB‐08A litho‐log, related ejecta, and shock recovery experiments , 2007 .

[48]  L. Pesonen,et al.  The Bosumtwi meteorite impact structure, Ghana: A magnetic model , 2000 .

[49]  C. Koeberl,et al.  Geology and geochemistry of shallow drill cores from the Bosumtwi impact structure, Ghana , 2003 .

[50]  D. Schmitt,et al.  In situ seismic measurements in borehole LB‐08A in the Bosumtwi impact structure, Ghana: Preliminary interpretation , 2007 .

[51]  C. Koeberl,et al.  Chromium isotopic studies of terrestrial impact craters: Identification of meteoritic components at Bosumtwi, Clearwater East, Lappajärvi, and Rochechouart , 2007 .

[52]  J. Peck,et al.  Uppermost Impact Fallout Layer in a Drillcore at the Bosumtwi Impact Crater (Ghana): A Preliminary Study , 2006 .

[53]  M. Rampino,et al.  Comparison of Bosumtwi Impact Crater (Ghana) and Crater Lake Volcanic Caldera (Oregon, USA): Implications for Biotic Recovery after Catastrophic Events , 2006 .

[54]  M. Talbot,et al.  Primary and diagenetic carbonates in the anoxic sediments of Lake Bosumtwi, Ghana , 1986 .

[55]  Hernan Ugalde,et al.  The Lake Bosumtwi meteorite impact structure, Ghana—Where is the magnetic source? , 2007 .

[56]  T. Johannessen,et al.  A high resolution palaeoclimatic record for the last 27,500 years in tropical West Africa from the carbon and nitrogen isotopic composition of lacustrine organic matter , 1992 .

[57]  H. J. Lippolt,et al.  Rubidium-Strontium-Messungen an Gläsern vom Bosumtwi-Krater und an Elfenbeinküsten-Tektiten , 1966 .

[58]  H. J. Melosh,et al.  Planetary science: Meteor Crater formed by low-velocity impact , 2005, Nature.

[59]  R. Ketcham,et al.  High-resolution X-ray computed tomography of impactites , 2002 .

[60]  C. Koeberl,et al.  Petrology and geochemistry of target rocks from the Bosumtwi impact structure, Ghana, and comparison with Ivory Coast tektites , 1998 .

[61]  Benjamin F. Turner,et al.  The geochemistry of Lake Bosumtwi, a hydrologically closed basin in the humid zone of tropical Ghana , 1996 .

[62]  P. Fox A 1 Ma West African Climate Change Record From Lake Bosumtwi, Ghana , 2006 .

[63]  John B. Wright,et al.  Geology and Mineral Resources of West Africa , 1985 .

[64]  C. Koeberl,et al.  Geochemistry and age of Ivory Coast tektites and microtektites , 1997 .

[65]  Benjamin F. Turner,et al.  The hydrology of Lake Bosumtwi, a climate-sensitive lake in Ghana, West Africa , 1996 .

[66]  A. E. Kitson The Gold Coast: Some Considerations of Its Structure, People and Natural History , 1916 .

[67]  B. Milkereit,et al.  Impactites as a random medium—Using variations in physical properties to assess heterogeneity within the Bosumtwi meteorite impact crater , 2007 .

[68]  C. Koeberl,et al.  Geochemistry of Cenozoic microtektites and clinopyroxene-bearing spherules , 2004 .

[69]  B. Milkereit,et al.  The Lake Bosumtwi meteorite impact structure, Ghana—A magnetic image from a third observational level , 2007 .

[70]  S. Danuor,et al.  Seismic investigation of the Lake Bosumtwi impact crater: Preliminary results , 2002 .

[71]  C. Koeberl,et al.  Petrographic studies of “fallout” suevite from outside the Bosumtwi impact structure, Ghana , 2006 .

[72]  M. Talbot,et al.  Sensitivity of carbon isotopic proxies to paleoclimatic forcing: A case study from Lake Bosumtwi, Ghana, over the last 32,000 years , 2003 .

[73]  L. Pesonen,et al.  New Studies of the Bosumtwi Impact Structure, Ghana: The 1997 Field Season , 1997 .

[74]  J. Overpeck,et al.  Late-Quaternary lowstands of lake Bosumtwi, Ghana: evidence from high-resolution seismic-reflection and sediment-core data , 2005 .

[75]  S. Moorbath,et al.  Early Proterozoic crustal evolution in the birimian of Ghana: constraints from geochronology and isotope geochemistry , 1992 .

[76]  J. Morrow Shock‐metamorphic petrography and microRaman spectroscopy of quartz in upper impactite interval, ICDP drill core LB‐07A, Bosumtwi impact crater, Ghana , 2007 .

[77]  L. Hecht,et al.  Uppermost impact fallback layer in the Bosumtwi crater (Ghana): Mineralogy, geochemistry, and comparison with Ivory Coast tektites , 2007 .

[78]  A. Menyeh,et al.  Results of pre‐drilling potential field measurements at the Bosumtwi crater , 2007 .

[79]  A. Leube,et al.  The early Proterozoic Birimian Supergroup of Ghana and some aspects of its associated gold mineralization , 1990 .

[80]  Christian Koeberl,et al.  Drill core LB‐08A, Bosumtwi impact structure, Ghana: Petrographic and shock metamorphic studies of material from the central uplift , 2007 .

[81]  L. Pesonen,et al.  Airborne geophysical survey of the lake Bosumtwi meteorite impact structure, ( southern Ghana): geophysical maps with descriptions , 2003 .

[82]  N. Artemieva,et al.  Investigating the Lake Bosumtwi impact structure: Insight from numerical modeling , 2004 .

[83]  H. Newsom,et al.  AN INTERNATIONAL AND MULTIDISCIPLINARY DRILLING PROJECT INTO A YOUNG COMPLEX IMPACT STRUCTURE: THE 2004 ICDP BOSUMTWI IMPACT CRATER, GHANA, , 2006 .

[84]  B. Glass Chemical composition of Ivory Coast microtektites. , 1969 .

[85]  E. Anders,et al.  Meteoritic material at five large impact craters , 1978 .

[86]  C. Koeberl,et al.  Geochemistry of impactites and basement lithologies from ICDP borehole LB‐07A, Bosumtwi impact structure, Ghana , 2007 .

[87]  C. Koeberl,et al.  Geochemistry of Soils from the Bosumtwi Impact Structure, Ghana, and Relationship to Radiometric Airborne Geophysical Data , 2002 .

[88]  N. Artemieva Possible reasons of shock melt deficiency in the Bosumtwi drill cores , 2007 .

[89]  B. Peucker‐Ehrenbrink,et al.  Search for a meteoritic component in drill cores from the Bosumtwi impact structure, Ghana: Platinum group element contents and osmium isotopic characteristics , 2007 .

[90]  W. Reimold Bosumtwi Impact Crater , Ghana ( West Africa ) : An Updated and Revised Geological Map , with Explanations , 2005 .

[91]  W. Morris,et al.  Physical property measurements: ICDP boreholes LB‐07A and LB‐08A, Lake Bosumtwi impact structure, Ghana , 2007 .

[92]  W. Morris,et al.  Clast fabric examination of impact‐generated breccias, borehole LB‐07A, Bosumtwi, Ghana , 2007 .

[93]  T. Wonik,et al.  Lithological and structural characteristics of the Lake Bosumtwi impact crater, Ghana: Interpretation of acoustic televiewer images , 2007 .

[94]  A. Kontny,et al.  Petrophysical and paleomagnetic data of drill cores from the Bosumtwi impact structure, Ghana , 2007 .

[95]  C. Koeberl,et al.  Petrography, geochemistry, and alteration of country rocks from the Bosumtwi impact structure, Ghana , 2007 .

[96]  C. Koeberl,et al.  Beryllium-10 in Ivory Coast Tektites , 2005 .

[97]  B. Glass,et al.  The Ivory Coast microtektite strewnfield: new data , 1979 .