-
1
-
-
0031739949
-
The history of ALH 84001 revised: Multiple shock events
-
This paper presents a chronology of ALH84001, including shock events that occurred before ejection from the Martian surface.
-
Treiman A.H. The history of ALH 84001 revised: multiple shock events. Meteorit Planet Sci. 33:1998;753-764. This paper presents a chronology of ALH84001, including shock events that occurred before ejection from the Martian surface.
-
(1998)
Meteorit Planet Sci
, vol.33
, pp. 753-764
-
-
Treiman, A.H.1
-
2
-
-
1842378043
-
Characterization of the Martian surface deposits by the Mars Pathfinder rover, Sojourner. Rover Team
-
Characterization of the Martian surface deposits by the Mars Pathfinder rover, Sojourner. Rover Team. Science. 278:1997;1765-1768.
-
(1997)
Science
, vol.278
, pp. 1765-1768
-
-
-
3
-
-
0033213911
-
The age of the carbonates in Martian meteorite ALH84001
-
Isotopic dating of carbonate mineralization in ALH84001 indicates an age of 4.0 billion years. Thus, the carbonates formed on Mars at a time when liquid water is thought to have been present on the planet.
-
Borg L.E., Connelly J.N., Nyquist L.E., Shih C.-Y., Wiesmann H., Reese Y. The age of the carbonates in Martian meteorite ALH84001. Science. 286:1999;90-94. Isotopic dating of carbonate mineralization in ALH84001 indicates an age of 4.0 billion years. Thus, the carbonates formed on Mars at a time when liquid water is thought to have been present on the planet.
-
(1999)
Science
, vol.286
, pp. 90-94
-
-
Borg, L.E.1
Connelly, J.N.2
Nyquist, L.E.3
Shih, C.-Y.4
Wiesmann, H.5
Reese, Y.6
-
4
-
-
0029663175
-
Search for past life on Mars: Possible relic biogenic activity in martian meteorite ALH 84001
-
McKay D.S., Gibson E.K. Jr., Thomas-Keprta K.L., Vali H., Romanek C.S., Clemett S.J., Chillier X.D.F., Maechling C.R., Zare R.N. Search for past life on Mars: possible relic biogenic activity in martian meteorite ALH 84001. Science. 273:1996;924-930.
-
(1996)
Science
, vol.273
, pp. 924-930
-
-
McKay, D.S.1
Gibson E.K., Jr.2
Thomas-Keprta, K.L.3
Vali, H.4
Romanek, C.S.5
Clemett, S.J.6
Chillier, X.D.F.7
Maechling, C.R.8
Zare, R.N.9
-
5
-
-
0033616889
-
The origin of organic matter in the martian meteorite ALH84001
-
A variety of organic materials including PAHs and kerogen are found in different locales in ALH84001. Isotopic analysis of organic carbon associated with carbonates is consistent with terrestrial contamination. The analysis shows that the kerogen is similar to organic material in carbonaceous chondrites. The authors propose that the extraterrestrial organic material in ALH84001 originated in meteorites that fell on Mars.
-
Becker L., Popp B., Rust T., Bada J.L. The origin of organic matter in the martian meteorite ALH84001. Earth Planet Sci Lett. 167:1999;71-79. A variety of organic materials including PAHs and kerogen are found in different locales in ALH84001. Isotopic analysis of organic carbon associated with carbonates is consistent with terrestrial contamination. The analysis shows that the kerogen is similar to organic material in carbonaceous chondrites. The authors propose that the extraterrestrial organic material in ALH84001 originated in meteorites that fell on Mars.
-
(1999)
Earth Planet Sci Lett
, vol.167
, pp. 71-79
-
-
Becker, L.1
Popp, B.2
Rust, T.3
Bada, J.L.4
-
6
-
-
0032536042
-
Isotopic evidence for a terrestrial source of organic compounds found in Martian meteorites Allan Hills 84001 and Elephant Moraine 79001
-
The organic fraction obtained by heating ALH84001 has a carbon isotopic composition that is consistent with a terrestrial origin, whereas the higher-temperature, carbonate-rich fraction has a carbon isotopic composition consistent with an extraterrestrial origin.
-
Jull A.J., Courtney C., Jeffrey D.A., Beck J.W. Isotopic evidence for a terrestrial source of organic compounds found in Martian meteorites Allan Hills 84001 and Elephant Moraine 79001. Science. 279:1998;366-369. The organic fraction obtained by heating ALH84001 has a carbon isotopic composition that is consistent with a terrestrial origin, whereas the higher-temperature, carbonate-rich fraction has a carbon isotopic composition consistent with an extraterrestrial origin.
-
(1998)
Science
, vol.279
, pp. 366-369
-
-
Jull, A.J.1
Courtney, C.2
Jeffrey, D.A.3
Beck, J.W.4
-
7
-
-
0030595860
-
Evaluating the evidence for past life on Mars
-
Bell J.F. Evaluating the evidence for past life on Mars. Science. 274:1996;2121-2122.
-
(1996)
Science
, vol.274
, pp. 2121-2122
-
-
Bell, J.F.1
-
8
-
-
0030849891
-
Polycyclic aromatic hydrocarbons (PAHs) in Antarctic Martian meteorites, carbonaceous chondrites, and polar ice
-
Becker L., Glavin D.P., Bada J.L. Polycyclic aromatic hydrocarbons (PAHs) in Antarctic Martian meteorites, carbonaceous chondrites, and polar ice. Geochim Cosmochim Acta. 61:1997;475-481.
-
(1997)
Geochim Cosmochim Acta
, vol.61
, pp. 475-481
-
-
Becker, L.1
Glavin, D.P.2
Bada, J.L.3
-
9
-
-
0031604807
-
Evidence for the extraterrestrial origin of polycyclic aromatic hydrocarbons (PAHs) in the Martian meteorite ALH 84001
-
PAHs are depleted in the fusion crust compared to sites within the meteorite, contrary to what would be expected for contamination in Antarctica. Moreover, the PAH concentration in ice from the Allan Hills glacier is too low to account for the concentration within the meteorite. Finally, carbonates do not preferentially absorb PAHs. The authors argue that these features indicate a Martian origin of at least some of the PAHs.
-
Clemett S.J., Dulay M.T., Gilette J.S., Chillier X.D.F., Mahajan T.B., Zare R.N. Evidence for the extraterrestrial origin of polycyclic aromatic hydrocarbons (PAHs) in the Martian meteorite ALH 84001. Faraday Discuss. 109:1998;417-436. PAHs are depleted in the fusion crust compared to sites within the meteorite, contrary to what would be expected for contamination in Antarctica. Moreover, the PAH concentration in ice from the Allan Hills glacier is too low to account for the concentration within the meteorite. Finally, carbonates do not preferentially absorb PAHs. The authors argue that these features indicate a Martian origin of at least some of the PAHs.
-
(1998)
Faraday Discuss
, vol.109
, pp. 417-436
-
-
Clemett, S.J.1
Dulay, M.T.2
Gilette, J.S.3
Chillier, X.D.F.4
Mahajan, T.B.5
Zare, R.N.6
-
10
-
-
0032728695
-
Abiotic synthesis of polycyclic aromatic hydrocarbons on Mars
-
Thermochemical calculations of condensed PAHs in cooling thermal gases and hydrothermal fluids on ancient Mars suggest that PAHs and aliphatic hydrocarbons could have formed without biogenic intervention. Thus, Martian PAHs in ALH84001 are not necessarily biogenic.
-
Zolotov M., Shock E. Abiotic synthesis of polycyclic aromatic hydrocarbons on Mars. J Geophys Res. 104:1999;14033-14049. Thermochemical calculations of condensed PAHs in cooling thermal gases and hydrothermal fluids on ancient Mars suggest that PAHs and aliphatic hydrocarbons could have formed without biogenic intervention. Thus, Martian PAHs in ALH84001 are not necessarily biogenic.
-
(1999)
J Geophys Res
, vol.104
, pp. 14033-14049
-
-
Zolotov, M.1
Shock, E.2
-
13
-
-
84874968970
-
Alternative origins for nanobacteria-like objects in calcite
-
Scanning electron microscope images of the surfaces of calcite crystals grown in the laboratory show sub-micron surface structures that are similar to the BSOs in ALH84001. This suggests that the BSOs in ALH84001 are not necessarily microfossils.
-
Kirkland B.L., Lynch F.L., Rahnis M.A., Folk R.L., Molineux I.J., McLean R.J.C. Alternative origins for nanobacteria-like objects in calcite. Geology. 27:1999;347-350. Scanning electron microscope images of the surfaces of calcite crystals grown in the laboratory show sub-micron surface structures that are similar to the BSOs in ALH84001. This suggests that the BSOs in ALH84001 are not necessarily microfossils.
-
(1999)
Geology
, vol.27
, pp. 347-350
-
-
Kirkland, B.L.1
Lynch, F.L.2
Rahnis, M.A.3
Folk, R.L.4
Molineux, I.J.5
McLean, R.J.C.6
-
14
-
-
0031794515
-
Martian "microfossils" in lunar meteorites?
-
Scanning electron microscope images of minerals in four Antarctic meteorites of lunar origin show sub-micron surface structures that are similar to the BSOs in ALH84001. The surface structures in the lunar meteorites might have formed during residence in Antarctica, suggesting that the BSOs in ALH84001 might have formed in Antarctica and thus may not be fossilized Martian microorganisms
-
Sears D.W.G., Kral T.A. Martian "microfossils" in lunar meteorites? Meteorit Planet Sci. 33:1998;791-794. Scanning electron microscope images of minerals in four Antarctic meteorites of lunar origin show sub-micron surface structures that are similar to the BSOs in ALH84001. The surface structures in the lunar meteorites might have formed during residence in Antarctica, suggesting that the BSOs in ALH84001 might have formed in Antarctica and thus may not be fossilized Martian microorganisms.
-
(1998)
Meteorit Planet Sci
, vol.33
, pp. 791-794
-
-
Sears, D.W.G.1
Kral, T.A.2
-
15
-
-
0029662503
-
A possible high-temperature origin for the carbonates in the Martian meteorite ALH84001
-
Harvey R.P., McSween H.Y. Jr. A possible high-temperature origin for the carbonates in the Martian meteorite ALH84001. Nature. 382:1996;49-51.
-
(1996)
Nature
, vol.382
, pp. 49-51
-
-
Harvey, R.P.1
McSween H.Y., Jr.2
-
16
-
-
0033134199
-
Olivine in Martian meteorite ALH84001: Evidence for high-temperature origin and implications for signs of life
-
4) near disrupted carbonates apparently formed at high temperature (> 900°C), possibly during an impact event, which suggests high-temperature formation of the magnetite crystals.
-
4) near disrupted carbonates apparently formed at high temperature (> 900°C), possibly during an impact event, which suggests high-temperature formation of the magnetite crystals.
-
(1999)
Meteorit Planet Sci
, vol.34
, pp. 331-340
-
-
Shearer, C.K.1
Leshin, L.A.2
Adcock, C.T.3
-
17
-
-
0033602157
-
Origin of carbonate-magnetite-sulfide assemblages in Martian meteorite ALH84001
-
Arguments for nonbiological, shock formation of the carbonates, magnetite and iron sulfides are summarized.
-
Scott E.R.D. Origin of carbonate-magnetite-sulfide assemblages in Martian meteorite ALH84001. J Geophys Res. 104:1999;3803-3813. Arguments for nonbiological, shock formation of the carbonates, magnetite and iron sulfides are summarized.
-
(1999)
J Geophys Res
, vol.104
, pp. 3803-3813
-
-
Scott, E.R.D.1
-
18
-
-
0032566150
-
Petrologic evidence for low-temperature, possibly flood-evaporitic origin of carbonates in the ALH84001 meteorite
-
Formation of the carbonate globules in ALH84001 by high-temperature chemical reactions or from carbonate-rich magma is not supported by petrologic data. Deposition of the carbonates from hot water is also not consistent with the lack of clays and other water-bearing silicate minerals. The author suggests precipitation of the carbonate from evaporating brine at ambient temperature. The proposal is neutral on biological involvment.
-
Warren P.H. Petrologic evidence for low-temperature, possibly flood-evaporitic origin of carbonates in the ALH84001 meteorite. J Geophys Res. 103:1998;16759-16773. Formation of the carbonate globules in ALH84001 by high-temperature chemical reactions or from carbonate-rich magma is not supported by petrologic data. Deposition of the carbonates from hot water is also not consistent with the lack of clays and other water-bearing silicate minerals. The author suggests precipitation of the carbonate from evaporating brine at ambient temperature. The proposal is neutral on biological involvment.
-
(1998)
J Geophys Res
, vol.103
, pp. 16759-16773
-
-
Warren, P.H.1
-
19
-
-
0032451858
-
An evaporation model for formation of carbonates in the ALH84001 Martian meteorite
-
McSween H.Y. Jr., Harvey R.P. An evaporation model for formation of carbonates in the ALH84001 Martian meteorite. Intl Geol Rev. 40:1998;774-783.
-
(1998)
Intl Geol Rev
, vol.40
, pp. 774-783
-
-
McSween H.Y., Jr.1
Harvey, R.P.2
-
20
-
-
0030620644
-
Low-temperature carbonate concretions in the Martian meteorite ALH84001: Evidence from stable isotopes and mineralogy
-
Valley J.W., Eiler J.M., Graham C.M., Gibson E.K., Romanek C.S., Stolper E.M. Low-temperature carbonate concretions in the Martian meteorite ALH84001: evidence from stable isotopes and mineralogy. Science. 275:1997;1633-1638.
-
(1997)
Science
, vol.275
, pp. 1633-1638
-
-
Valley, J.W.1
Eiler, J.M.2
Graham, C.M.3
Gibson, E.K.4
Romanek, C.S.5
Stolper, E.M.6
-
21
-
-
0031769808
-
Chemical and stable isotopic disequilibrium in carbonate minerals of Martian meteorite ALH 84001: Inconsistent with high formation temperature
-
Treiman A.H., Romanek C.S. Chemical and stable isotopic disequilibrium in carbonate minerals of Martian meteorite ALH 84001: inconsistent with high formation temperature. Meteorit Planet Sci. 33:1998;737-742.
-
(1998)
Meteorit Planet Sci
, vol.33
, pp. 737-742
-
-
Treiman, A.H.1
Romanek, C.S.2
-
22
-
-
0030620642
-
Paleomagnetic evidence of a low-temperature origin of carbonates in the Martian meteorite ALH 84001
-
Kirschvink J.L., Maine A.T., Vali H. Paleomagnetic evidence of a low-temperature origin of carbonates in the Martian meteorite ALH 84001. Science. 275:1997;1629-1633.
-
(1997)
Science
, vol.275
, pp. 1629-1633
-
-
Kirschvink, J.L.1
Maine, A.T.2
Vali, H.3
-
23
-
-
0030620966
-
Petrological evidence for shock melting of carbonates in the Martian meteorite ALH 84001
-
Scott E.R.D., Yamaguchi A., Krot A.N. Petrological evidence for shock melting of carbonates in the Martian meteorite ALH 84001. Nature. 387:1997;377-379.
-
(1997)
Nature
, vol.387
, pp. 377-379
-
-
Scott, E.R.D.1
Yamaguchi, A.2
Krot, A.N.3
-
24
-
-
85031638791
-
Microstructures of feldspathic glass in ALH84001 and evidence for post-carbonate formation shock melting
-
Houston, March 16-20
-
Brearley, A.J.: Microstructures of feldspathic glass in ALH84001 and evidence for post-carbonate formation shock melting. Abstract 1451, 29th Lunar Planet Sci Conference, Houston, March 16-20 1998. [ http://cass.jsc.nasa.gov/lpi/meteorites/29thlpscabs.html].
-
(1998)
Abstract 1451, 29th Lunar Planet Sci Conference
-
-
Brearley, A.J.1
-
25
-
-
0031429903
-
Sulfide isotope compositions in shergottites and ALH 84001, and possible implications for life on Mars
-
Greenwood J.P., Riciputi L.R., McSween H.Y. Jr. Sulfide isotope compositions in shergottites and ALH 84001, and possible implications for life on Mars. Geochim Cosmochim Acta. 61:1997;4449-4453.
-
(1997)
Geochim Cosmochim Acta
, vol.61
, pp. 4449-4453
-
-
Greenwood, J.P.1
Riciputi, L.R.2
McSween H.Y., Jr.3
-
26
-
-
0042562443
-
Reaction sequence of iron sulfide minerals in bacteria and their use as biomarkers
-
Studies of iron sulfide magnetosomes in marine magnetotactic bacteria show greigite to be the most abundant mineral. Non-magnetic mackinawite (tetragonal FeS) and putative cubic FeS were also found and shown to be precursors to greigite mineralization. Neither pyrrhotite nor pyrite were found.
-
Pósfai M., Buseck P.R., Bazylinski D.A., Frankel R.B. Reaction sequence of iron sulfide minerals in bacteria and their use as biomarkers. Science. 280:1998;880-883. Studies of iron sulfide magnetosomes in marine magnetotactic bacteria show greigite to be the most abundant mineral. Non-magnetic mackinawite (tetragonal FeS) and putative cubic FeS were also found and shown to be precursors to greigite mineralization. Neither pyrrhotite nor pyrite were found.
-
(1998)
Science
, vol.280
, pp. 880-883
-
-
Pósfai, M.1
Buseck, P.R.2
Bazylinski, D.A.3
Frankel, R.B.4
-
28
-
-
7444250476
-
Characterization of magnetite within carbonate in ALH84001
-
Houston, March 16-20
-
Blake, D.F., Treiman, A.H., Cady, S., Nelson, C., Krishnan, K.: Characterization of magnetite within carbonate in ALH84001. Abstract 1347, 29th Lunar Planet Sci Conference, Houston, 1998 March 16-20. [ http://cass.jsc.nasa.gov/lpi/meteorites/29thlpscabs.html].
-
(1998)
Abstract 1347, 29th Lunar Planet Sci Conference
-
-
Blake, D.F.1
Treiman, A.H.2
Cady, S.3
Nelson, C.4
Krishnan, K.5
-
29
-
-
0030310386
-
Magnetite whiskers and platelets in ALH 840001 Martian meteorite: Evidence of vapor phase growth
-
Bradley J.P., Harvey R.P., McSween H.Y. Jr. Magnetite whiskers and platelets in ALH 840001 Martian meteorite: evidence of vapor phase growth. Geochim Cosmochim Acta. 60:1996;5149-5155.
-
(1996)
Geochim Cosmochim Acta
, vol.60
, pp. 5149-5155
-
-
Bradley, J.P.1
Harvey, R.P.2
McSween H.Y., Jr.3
-
30
-
-
0001533027
-
Magnetite in ALH 84001: product of the decomposition of ferroan carbonate
-
March 16-20, Houston. Transmission electron microscope and scanning electron microscope observations of magnetite in carbonate imbedded in feldspathic glass suggest formation by thermal decomposition of iron carbonates
-
Brearley, A.J.: Magnetite in ALH 84001: product of the decomposition of ferroan carbonate. Abstract 1757 of the 29th Lunar Planet Sci Conference, 1998 March 16-20, Houston. [ http://cass.jsc.nasa.gov/lpi/meteorites/29thlpscabs.html] . Transmission electron microscope and scanning electron microscope observations of magnetite in carbonate imbedded in feldspathic glass suggest formation by thermal decomposition of iron carbonates.
-
(1998)
Abstract 1757 of the 29th Lunar Planet Sci Conference
-
-
Brearley, A.J.1
-
31
-
-
0346096152
-
Magnetite from ALH84001 carbonate globules: evidence of biogenic signatures?
-
March 16-20, Houston
-
Thomas-Keprta, K.L., Bazylinski, D.A., Golden, D.C., Wentworth, S.J., Gibson, E.K., Jr., McKay, D.S.: Magnetite from ALH84001 carbonate globules: evidence of biogenic signatures? Abstract 1494 of the 29th Lunar Planet Sci Conference, 1998 March 16-20, Houston. [ http://cass.jsc.nasa.gov/lpi/meteorites/29thlpscabs.html].
-
(1998)
Abstract 1494 of the 29th Lunar Planet Sci Conference
-
-
Thomas-Keprta, K.L.1
Bazylinski, D.A.2
Golden, D.C.3
Wentworth, S.J.4
Gibson E.K., Jr.5
McKay, D.S.6
-
32
-
-
85031643236
-
On the origins of magnetite in Martian meteorite ALH 84001
-
March 14-19, Houston
-
Thomas-Keprta, K.L., Wentworth, S.J., McKay, D.S., Bazylinski, D.A., Bell, M.S., Romanek, C.S., Golden, D.C., Gibson, E.K., Jr.: On the origins of magnetite in Martian meteorite ALH 84001. Abstract 1856, 30th Lunar Planet Sci Conference, 1999 March 14-19, Houston. [ http://cass.jsc.nasa.gov/lpi/meteorites/30thlpscabs,html].
-
(1999)
Abstract 1856, 30th Lunar Planet Sci Conference
-
-
Thomas-Keprta, K.L.1
Wentworth, S.J.2
McKay, D.S.3
Bazylinski, D.A.4
Bell, M.S.5
Romanek, C.S.6
Golden, D.C.7
Gibson E.K., Jr.8
-
33
-
-
85031646636
-
Biogenic magnetite in Martian meteorite ALH84001
-
July 18-23, Pasadena. This extended abstract describes the magnetite crystals in ALH84001 and argues that about 25% of the crystals have habits that are similar to those in some species of magnetotactic bacteria
-
Thomas-Keprta, K.L., Bazylinski, D.A., Wentworth, S.J., McKay, D.S., Kirschvink, J.L., Clemett, S.J., Bell, M.S., Golden, D.C., Gibson, E.K., Jr.: Biogenic magnetite in Martian meteorite ALH84001. Abstract 6158 of the 5th International Conference on Mars, July 18-23, Pasadena. [ http://mars.jsc.jpl.nasa.gov/mgs/sci/fifthconf99/bio.htmlmeteorites/30thlpscabs, html] . This extended abstract describes the magnetite crystals in ALH84001 and argues that about 25% of the crystals have habits that are similar to those in some species of magnetotactic bacteria.
-
Abstract 6158 of the 5th International Conference on Mars
-
-
Thomas-Keprta, K.L.1
Bazylinski, D.A.2
Wentworth, S.J.3
McKay, D.S.4
Kirschvink, J.L.5
Clemett, S.J.6
Bell, M.S.7
Golden, D.C.8
Gibson E.K., Jr.9
-
34
-
-
0031771404
-
Epitaxial growth of nanophase magnetite in Martian meteorite ALH 84001: Implications for biogenic mineralization
-
Some magnetite crystals have axial screw dislocations and others are epitaxially intergrown with carbonates, suggesting vapor-phase growth and exposure of the carbonates to high temperatures.
-
Bradley J.P., McSween H.Y. Jr., Harvey R.P. Epitaxial growth of nanophase magnetite in Martian meteorite ALH 84001: implications for biogenic mineralization. Meteorit Planet Sci. 33:1998;765-773. Some magnetite crystals have axial screw dislocations and others are epitaxially intergrown with carbonates, suggesting vapor-phase growth and exposure of the carbonates to high temperatures.
-
(1998)
Meteorit Planet Sci
, vol.33
, pp. 765-773
-
-
Bradley, J.P.1
McSween H.Y., Jr.2
Harvey, R.P.3
-
35
-
-
0001484681
-
Unusual forms of magnetite in the Orgueil carbonaceous chondrite
-
Hua X., Buseck P.R. Unusual forms of magnetite in the Orgueil carbonaceous chondrite. Meteorit Planet Sci. 33:1998;215-220.
-
(1998)
Meteorit Planet Sci
, vol.33
, pp. 215-220
-
-
Hua, X.1
Buseck, P.R.2
-
36
-
-
0030834146
-
Carbide-magnetite assemblages in type-3 ordinary chondrites
-
Krot A.N., Zolensky M.E., Wasson J.T., Scott E.R.D., Keil K., Ohsumi K. Carbide-magnetite assemblages in type-3 ordinary chondrites. Geochim Cosmochim Acta. 61:1997;219-237.
-
(1997)
Geochim Cosmochim Acta
, vol.61
, pp. 219-237
-
-
Krot, A.N.1
Zolensky, M.E.2
Wasson, J.T.3
Scott, E.R.D.4
Keil, K.5
Ohsumi, K.6
-
37
-
-
0032499261
-
Extreme oxygen-isotope compositions in magnetite from unequilibrated ordinary chondrites
-
Choi B.-G., McKeegan K.D., Krot A.N., Wasson J.T. Extreme oxygen-isotope compositions in magnetite from unequilibrated ordinary chondrites. Nature. 392:1998;577-579.
-
(1998)
Nature
, vol.392
, pp. 577-579
-
-
Choi, B.-G.1
McKeegan, K.D.2
Krot, A.N.3
Wasson, J.T.4
-
38
-
-
85061004198
-
Microbial biomineralization of magnetic iron minerals: Microbiology, magnetism and environmental significance
-
J.F. Banfield, & K.H. Nealson. Washington DC: Mineralogical Society of America. [Ribbe PH (Series Editor): Reviews in Mineralogy, vol 35.]
-
Bazylinski D.A., Moskowitz B.M. Microbial biomineralization of magnetic iron minerals: microbiology, magnetism and environmental significance. Banfield J.F., Nealson K.H. Geomicrobiology: Interactions between Microbes and Minerals. 1997;181-223 Mineralogical Society of America, Washington DC. [Ribbe PH (Series Editor): Reviews in Mineralogy, vol 35.].
-
(1997)
Geomicrobiology: Interactions between Microbes and Minerals
, pp. 181-223
-
-
Bazylinski, D.A.1
Moskowitz, B.M.2
-
39
-
-
0030478419
-
Magnetofossils in the sediments of Lake Baikal, Siberia
-
Peck J.A., King J.W. Magnetofossils in the sediments of Lake Baikal, Siberia. Earth Planet Sci Lett. 140:1996;159-172.
-
(1996)
Earth Planet Sci Lett
, vol.140
, pp. 159-172
-
-
Peck, J.A.1
King, J.W.2
-
40
-
-
0033578925
-
Iron isotope biosignatures
-
Isotopic fractionation in Fe(II) produced by dissimilatory iron-reduction was observed and is thought to be incorporated into subsequently precipitated magnetite, which might provide a signature of biogenic BIM magnetite.
-
Beard B.L., Johnson C.M., Cox L., Sun H., Nealson K.H., Aguilar C. Iron isotope biosignatures. Science. 285:1999;1889-1892. Isotopic fractionation in Fe(II) produced by dissimilatory iron-reduction was observed and is thought to be incorporated into subsequently precipitated magnetite, which might provide a signature of biogenic BIM magnetite.
-
(1999)
Science
, vol.285
, pp. 1889-1892
-
-
Beard, B.L.1
Johnson, C.M.2
Cox, L.3
Sun, H.4
Nealson, K.H.5
Aguilar, C.6
-
41
-
-
0033578926
-
Oxygen and iron isotope studies of magnetite produced by magnetotactic bacteria
-
In contrast to dissimilatory iron reduction, the uptake of iron and BCM of magnetite in magnetosomes does not result in fractionation of iron isotopes.
-
Mandernack K.W., Bazylinski D.A., Shanks W.C. Jr., Bullen T.D. Oxygen and iron isotope studies of magnetite produced by magnetotactic bacteria. Science. 285:1999;1892-1896. In contrast to dissimilatory iron reduction, the uptake of iron and BCM of magnetite in magnetosomes does not result in fractionation of iron isotopes.
-
(1999)
Science
, vol.285
, pp. 1892-1896
-
-
Mandernack, K.W.1
Bazylinski, D.A.2
Shanks W.C., Jr.3
Bullen, T.D.4
-
42
-
-
0032745555
-
Bacterial magnetosomes: Microbiology, biomineralization, and biotechnical applications
-
The physiology and biochemistry of magnetite mineralization in magnetotactic bacteria are discussed.
-
Schüler D., Frankel R. Bacterial magnetosomes: microbiology, biomineralization, and biotechnical applications. Appl Microbiol Biotechnol. 52:1999;464-473. The physiology and biochemistry of magnetite mineralization in magnetotactic bacteria are discussed.
-
(1999)
Appl Microbiol Biotechnol
, vol.52
, pp. 464-473
-
-
Schüler, D.1
Frankel, R.2
-
43
-
-
0032445692
-
Magnetite from magnetotactic bacteria: Size limitations and twinning
-
Crystal habits, size distributions and structural features of magnetosome magnetite from five cultured strains of magnetotactic bacteria and synthetic magnetite suggest that size and shape distributions are useful in distinguishing BCM magnetite from non-biogenic magnetite.
-
Devouard B., Pósfai M., Hua X., Bazylinski D.A., Frankel R.B., Buseck P.R. Magnetite from magnetotactic bacteria: size limitations and twinning. Am Mineral. 83:1998;1387-1398. Crystal habits, size distributions and structural features of magnetosome magnetite from five cultured strains of magnetotactic bacteria and synthetic magnetite suggest that size and shape distributions are useful in distinguishing BCM magnetite from non-biogenic magnetite.
-
(1998)
Am Mineral
, vol.83
, pp. 1387-1398
-
-
Devouard, B.1
Pósfai, M.2
Hua, X.3
Bazylinski, D.A.4
Frankel, R.B.5
Buseck, P.R.6
-
44
-
-
0031984106
-
4 mineralization during aerobic and microaerobic growth of Magnetospirillum gryphiswaldense
-
4 mineralization during aerobic and microaerobic growth of Magnetospirillum gryphiswaldense. J Bacteriol. 180:1998;159-162.
-
(1998)
J Bacteriol
, vol.180
, pp. 159-162
-
-
Schüler, D.1
Baeuerlein, E.2
-
45
-
-
0032484202
-
Magnetic microstructure of magnetotactic bacteria by electron holography
-
Electron holography was used to visualize the magnetic field lines associated with a chain of magnetosomes within a magnetotactic bacterium.
-
Dunin-Borkowski R.E., McCartney M.R., Frankel R.B., Bazylinski D.A., Pósfai M., Buseck P.R. Magnetic microstructure of magnetotactic bacteria by electron holography. Science. 282:1998;1868-1870. Electron holography was used to visualize the magnetic field lines associated with a chain of magnetosomes within a magnetotactic bacterium.
-
(1998)
Science
, vol.282
, pp. 1868-1870
-
-
Dunin-Borkowski, R.E.1
McCartney, M.R.2
Frankel, R.B.3
Bazylinski, D.A.4
Pósfai, M.5
Buseck, P.R.6
-
46
-
-
0030872053
-
Magneto-aerotaxis in marine, coccoid bacteria
-
Frankel R.B., Bazylinski D.A., Johnson M., Taylor B.L. Magneto-aerotaxis in marine, coccoid bacteria. Biophys J. 73:1997;994-1000.
-
(1997)
Biophys J
, vol.73
, pp. 994-1000
-
-
Frankel, R.B.1
Bazylinski, D.A.2
Johnson, M.3
Taylor, B.L.4
-
47
-
-
0032362906
-
Deducing growth mechanisms for minerals from the shapes of crystal size distributions
-
Eberl D.D., Drits V.A., Srodon J. Deducing growth mechanisms for minerals from the shapes of crystal size distributions. Am J Sci. 298:1998;499-533.
-
(1998)
Am J Sci
, vol.298
, pp. 499-533
-
-
Eberl, D.D.1
Drits, V.A.2
Srodon, J.3
-
48
-
-
0003900588
-
Inorganic formation of zoned Mg-Fe-Ca carbonate globules with magnetite and sulfide rims similar to those in Martian meteorite ALH84001
-
March 13-17, Houston. Carbonate globules with 10-1000 nm magnetite and pyrrhotite grains were synthesized in a multi-step process that included precipitation of chemically zoned carbonates followed by heating to simulate a shock event. This work suggests that the carbonate assemblages in ALH84001 may have formed inorganically
-
Golden, D.C., Ming, D.W., Schwandt, C.S., Lauer, H.V., Socki, R.A., Morris, R.V., Lofgren, G.E., McKay, G.A.: Inorganic formation of zoned Mg-Fe-Ca carbonate globules with magnetite and sulfide rims similar to those in Martian meteorite ALH84001. Abstract 1799 of the 31st Lunar and Planetary Science Conference, 2000 March 13-17, Houston. [ http://www.lpi.usra.edu/meetings/lpsc2000/pdf/sess79.pdf] . Carbonate globules with 10-1000 nm magnetite and pyrrhotite grains were synthesized in a multi-step process that included precipitation of chemically zoned carbonates followed by heating to simulate a shock event. This work suggests that the carbonate assemblages in ALH84001 may have formed inorganically.
-
(2000)
Abstract 1799 of the 31st Lunar and Planetary Science Conference
-
-
Golden, D.C.1
Ming, D.W.2
Schwandt, C.S.3
Lauer, H.V.4
Socki, R.A.5
Morris, R.V.6
Lofgren, G.E.7
McKay, G.A.8
-
49
-
-
85031642384
-
Reconciliation of magnetic and petrographic constraints on ALH84001? Panspermia lives on!
-
March 13-17, Houston. The effects of thermal demagnetization on the natural remanent magnetization of slices of ALH84001 were studied by scanning SQUID microscopy. The results suggest that the carbonate globules in ALH84001 formed at low temperature and that the meteorite was transferred from Mars to Earth, including ejection from the Martian surface and passage through the Earth atmosphere, without interior heating above 40°C
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Weiss, B.P., Kirschvink, J.L., Baudenbacher, F.J., Vali, H., Peters, N.T., Macdonald, F.A., Wikswo, J.P.: Reconciliation of magnetic and petrographic constraints on ALH84001? Panspermia lives on! Abstract 2078 of the 31st Lunar and Planetary Science Conference, 2000 March 13-17, Houston. [ http://www.lpi.usra.edu/meetings/lpsc2000/pdf/sess79.pdf] . The effects of thermal demagnetization on the natural remanent magnetization of slices of ALH84001 were studied by scanning SQUID microscopy. The results suggest that the carbonate globules in ALH84001 formed at low temperature and that the meteorite was transferred from Mars to Earth, including ejection from the Martian surface and passage through the Earth atmosphere, without interior heating above 40°C.
-
(2000)
Abstract 2078 of the 31st Lunar and Planetary Science Conference
-
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Weiss, B.P.1
Kirschvink, J.L.2
Baudenbacher, F.J.3
Vali, H.4
Peters, N.T.5
Macdonald, F.A.6
Wikswo, J.P.7
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