Geology Reference
In-Depth Information
Kuznetsov, V. G. (2000): Some features of the evolution of
carbonate accumulation in earth's history. Communica-
tion 1. Evolution of the intensity, mechanism and setting
of carbonate accumulations. - Lithology and Mineral
Resources,
35
, 32-46
Mackenzie, F.T., Morse, J.W. (1992): Sedimentary carbon-
ates through Phanerozoic time. - Geochimica et Cosmo-
chimica Acta,
56
, 3281-3295
Martin, R.E. (1995): Cyclic and secular variation in micro-
fossil biomineralization: clues to the biogeochemical evo-
lution of Phanerozoic oceans. - Global and Planetary
Change,
11
, 1-12
Milliman, J.D., Droxler, A.W. (1986): Neritic and pelagic
carbonate sedimentation in the marine environment: ig-
norance is not bliss. - Geol. Rundschau,
85
, 496-504
Montanez, I.P. (2002): Biological skeletal carbonate record
changes in major-ion chemistry of the paleo-oceans. -
PNAS,
99
, 15832-15854
Sandberg, P.A. (1983): An oscillating trend in Phanerozoic
non-skeletal carbonate mineralogy. - Nature,
305
, 19-22
Sandberg, P.A. (1985): Aragonite cements and their occur-
rence in ancient limestones. - In: Schneidermann, N., Har-
ris, P.M. (eds.): Carbonate cements. - Society of Economic
Paleontologists and Mineralogists, Special Publication,
36
,
33-57
Sandberg, P.A. (1991): Nonskeletal aragonite and pCO
2
in
the Phanerozoic and Proterozoic. - In: Sundquist, E.T.,
Broecker, W.S. (eds.): The carbon cycle and atmospheric
CO
2
: Natural variations Archean to Present. - Geophysi-
cal Monograph,
32
,585-594
Schlager, W. (2000): Sedimentation rates and growth poten-
tial of tropical, cool-water and mud-mound carbonate sys-
tems. - In: Insalaco, E., Skelton, P.W., Palmer, T.J. (eds.):
Carbonate platform systems; components and interactions.
- Geological Society of London, Special Publication,
178
,
217-227
Schlager, W. (2003): Benthic carbonate factories in the Phan-
erozoic. - Int. Journal of Earth Sciences,
92
, 445-464
Stanley, S.M., Hardie, L.A. (1998): Secular oscillations in
the carbonate mineralogy of reef-building and sediment-
producing organisms driven by tectonically forced shifts
in sea-water chemistry. - Palaeogeography, Palaeoclimat-
ology, Palaeoecology,
144
, 3-19
Stanley, S.M., Hardie, L.A. (1999): Hypercalcification: pa-
leontology links plate tectonics and geochemistry to sedi-
mentology. - GSA Today,
9
, 1-7
Steuber, T. (2002): Plate tectonic control on the evolution of
Cretaceous platform-carbonate production. - Geology,
30
,
259-262
Van de Poel, H.H., Schlager, W. (1994): Variations in Meso-
zoic and Cenozoic skeletal carbonate mineralogy. -
Geologie en Mijnbouw,
73
, 31-51
Walker, L.C., Wilkinson, B.H., Ivany, L.C. (2002): Conti-
nental drift and Phanerozoic carbonate accumulation in
shallow-shelf and deep-marine settings. - Journal of Ge-
ology,
110
, 75-87
Wilkinson, B.H., Given, R.K. (1986): Secular variation in
abiotic marine carbonates: constraints on Phanerozoic at-
mospheric carbon dioxide contents and oceanic Mg/Ca
ratios. - Journal of Geology,
94
, 321-333
Wilkinson, B.H., Walker, J.C.G. (1989): Phanerozoic cycling
of sedimentary carbonate. - American Journal of Science,
289
, 525-548
Further reading:
K185
10.2.4.1 and Sect. 10.2.4.2). Similarly, the evaluation
of crinoid accumulations should regard the changes in
preferred environments and associated differences in
taphonomy over time (Sect. 10.2.4.9).
Burrowing and bioturbation.
Using burrowing or
bioturbation fabrics (Sect. 5.1.4) as paleoenvironmen-
tal proxies, e.g. in recognizing substrate types (Sect.
12.1.3.2) means considering significant changes at the
Precambrian-Cambrian boundary and the quantitative
increase during the Phanerozoic (Bottjer and Droser
1994).
Basics: Secular variations in carbonate deposition
Barnes, C.R. (1999): Paleocenography and paleoclimatology:
an Earth system perspective. - Chemical Geology,
161
,
17-35
Bates, N.R., Brand, U. (1990): Secular variations of calcium
carbonate mineralogy: an evaluation of ooid and micrite
chemistries. - Geologische Rundschau,
79
, 27-46
Boss, S.K., Wilkinson, B.H. (1991): Planktogenic/eustatic
control on cratonic/oceanic carbonate accumulation. -
Journal of Geology,
99
, 497-513
Bosscher, H., Schlager, W. (1993): Accumulation rates of
carbonate platforms. - Journal of Geology,
101
, 345-355
Burns, S.J., McKenzie, J.A., Casconcelos, G. (2000): Dolo-
mite formation and biogeochemical cycles in the Phan-
erozoic. - Sedimentology,
47
, 49-61
Cowen, R. (1988): The role of algal symbiosis in reefs through
time. - Palaios,
3
, 221-227
Fischer, A.G. (1982): The two Phanerozoic supercycles. -
In: Bergren, W.A., van Couvering, J.A. (eds.): Catastro-
phes and Earth history. - 129-150, Princeton (Princeton
University Press)
Fischer, A.G., Arthur, M.A. (1977): Secular variation in the
pelagic realm. - In: Cook, H.E., Enos, P. (eds.): Deep-
water carbonate environments. - Society of Economic Pa-
leontologists and Mineralogists, Special Publication,
25
,
19-50
Flügel, E., Kiessling, W. (2002): Patterns of Phanerozoic reef
crises. - In: Kiessling, W., Flügel, E., Golonka, J. (eds.):
Phanerozoic Reef Patterns. - SEPM, Special Publication,
72
, 691-733
Grotzinger, J.P., James, N.P. (eds., 2000): Precambrian car-
bonates: evolution of understanding - SEPM, Special
Publication,
67
, 3-20
Hay, W.W. (1999): Carbonate sedimentation through the late
Precambrian and Phanerozoic. - Zentralblatt für Geologie
und Paläontologie, Teil I,
1998
, 435-445
Kiessling, W. (2001): Paleoclimatic significance of Phanero-
zoic reefs. - Geology,
29
, 751-754
Kiessling, W. (2002): Secular variations in the Phanerozoic
reef ecosystem. - In. Kiessling, W., Flügel, E., Golonka,
J. (eds., 2002): Phanerozoic Reef Patterns. - SEPM, Spe-
cial Publication,
72
, 625-690
Kiessling, W., Flügel, E., Golonka, J. (2000): Fluctuations in
the carbonate production of Phanerozoic reefs. - In:
Insalaco, E., Skelton, P.W., Palmer, T.J. (eds.): Carbonate
platform systems; components and interactions. - Geo-
logical Soc. London, Special Publication,
178
, 191-215
Kiessling, W., Flügel, E., Golonka, J. (2003): Patterns of car-
bonate platform sedimentation. - Lethaia,
36
, 195-225
