Geoenergogenerated dynamic cataclysms as the launch mechanism of the origin and evolution of the terrestrial life
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| Published in: | Геофизический журнал |
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| Date: | 2010 |
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| Format: | Article |
| Language: | English |
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Інститут геофізики ім. С.I. Субботіна НАН України
2010
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| Online Access: | https://nasplib.isofts.kiev.ua/handle/123456789/101319 |
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| Cite this: | Geoenergogenerated dynamic cataclysms as the launch mechanism of the origin and evolution of the terrestrial life / A. Drozdovskaya // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 39-40. — Бібліогр.: 2 назв. — англ. |
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Digital Library of Periodicals of National Academy of Sciences of Ukraine| _version_ | 1860258825340190720 |
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| author | Drozdovskaya, A. |
| author_facet | Drozdovskaya, A. |
| citation_txt | Geoenergogenerated dynamic cataclysms as the launch mechanism of the origin and evolution of the terrestrial life / A. Drozdovskaya // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 39-40. — Бібліогр.: 2 назв. — англ. |
| collection | DSpace DC |
| container_title | Геофизический журнал |
| first_indexed | 2025-12-07T18:52:57Z |
| format | Article |
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Geoenergogenerated dynamic cataclysms as the launch
mechanism of the origin and evolution of the terrestrial life
A. Drozdovskaya, 2010
Department of Marine Geology and Sedimentary Ore Genesis,
National Academy of Sciences of Ukraine, Kiev, Ukraine
dakaktotak@mail.ru
The author proposes a new conception for the
mechanism of the origin and evolution of the terres-
trial life in the energetic Earth-Space interactions
[Drozdovskaya, 2009]. This conception (named
geoenergetic) has been developed in the process of
the analysis of the Earth's biological and dynamical
history from the viewpoint of the author-made stu-
dies of the geochemical evolution history
[Drozdovskaya, 1990] that was carried out using
geological, physical-chemical, geoecological and
eniological methods.
The problem of the mechanism and time of the
terrestrial life origin was solved in connection to the
physical-chemical and geostructural specifics of the
Early Proterozoic Krivoy Rog-type Jaspilite Forma-
tion (JFKT) termed in English as the Banded Iron
Formation (BIF). BIF is considered as the unique
geological phenomenon due to a number of specific
features peculiar only to it. The main ones amongst
them are the single-act and geologically short time
of the BIF's global origination in the range by isoto-
pic data 24—2,2 billion years with accumulation in
it about 90 % of iron ore reserves of the Earth's
crust in simplified elemental form, predominantly
iron-silicon-oxygen.
The computer physical-chemical experiments
demonstrated [Drozdovska
chemogenic-sedimentary
evolution which origination is themodynamically limi-
ted by redox-barrier parameters of chemical inter-
actions between three external shells of the Earth
— water (hydrosphere), gas (atmosphere) and so-
lid (lithosphere) composing the planet exosphere.
It means that the temporal development of geochemi-
cal evolution was predicted by the steady-directed
transformation of the terrestrial exosphere from the
primary reduced state into recent oxidized one with
single-act overcoming of the redox-barrier at the
geological time interval of 2,4—2,2 Ga. Accounting
this statement, the author’s opinion is that BIF is a
geological reference point of geochemical evolution
that confirm that during the BIF genesis time co-
ming into the exosphere free oxygen completed the
oxidization of reduced polyvalent elements occur-
ring there. But, in the moment when BIF finished
its development, free oxygen for the first time be-
came able to remain in the exosphere in a thermo-
dynamically steady state pointing in this way the
moment of oxygen era dawn on the planet Earth.
Proceeding from this
Proceeding from this conclusion, an appearance
of one else distinguishing feature of BIF became
understand: a mass burial of blue-green algae ap-
peared in directly covering sediments for the very
first time in the history of the Earth crust. That bio-
logical phenomenon showed that, as the BIF ge-
neration stopped, the first in the Earth's history glo-
bal and mass origin of unicellular organisms took
place, which was initiated by the first occurrence
in the exosphere of the thermodynamically stable
free oxygen. It means that 2,2 Ga the structuration
of the pre-cellular organic matter finished also.
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In these links, an attempt was made to deter-
mine the time period where that structuration passed
— therefore, to recognize the moment of the First
Global Life Appearance. Solving those problems,
the original explanation of one more BIF's feature
was in hand: all its global ingredients were located
in morphologically uniform, fracture-like faults of the
coeval global tectonic structure.
Accounting the planet rotation, we may to pre-
suppose that before the start of the BIF origina-
tion, an surplus amount of geogenic energy (tor-
sion, most of all) was accumulated in the Earth
which, trying to leave this close space, provoked a
blast-like geodynamical cataclysm with lithosphere
splitting by a number of fracture-like faults, and
(geologically, in the one moment) penetrated trough
to the day surface. It was a very hard energetic strike
onto the exospherical matter world.
At this notion about geodynamical evolution, we
can see by "the morning eyes" that before the BIF
origination that the results of today biological ex-
periments have shown: some DNA fragments were
found after energetic impacts into a mixture of bio-
philic combinations (including hydrocarbonic). In this
connection, we can to assume a massive pulse
outburst of geogenic energy in the Early Proterozo-
ic exosphere was able to initiate forming of the pri-
mary living matter forms from existing chemical
combinations (their important parts were in that time
the combinations of reduced biophilic elements in-
cluding carbon, nitrogen, and sulfur). Therefore, the
time of global appearance of initial live matters forms
(i. e. the life appearance time) can be reasonably
dated with lower BIF’s age as 2,4 billion years.
From these positions, the author analyzed and
re-comprehended the history of step species com-
position transformations in the biosphere and com-
plication of its organisms’ matter organization that
is fixed in the Earth's crust at the lower boundaries
of geological epochs (Vendian, Cambrian, Ordovi-
cian, Silurian, Devonian, Carboniferous, Permian,
Triassic, Jurassic, Cretaceous, Paleogene, Neo-
gene) which are termed as transformation frontiers
of biological evolution. It is proved that at each the
frontier some organic species with more simple or-
ganization exited and new, more complicated ap-
peared. It means that the biosphere developed
through the time by the step complication of its or-
ganisms’ matter organization in the chain: Uni-
cellulars Multicellulars Corals Crustacea
Fishes Arthropoda Quadrupedantae Amphi-
bians Reptiles Mammalia Hominidae.
In the comparisons of the biological evolution and
geodynamic phenomena histories a mutual relation
in time became understood between the biospheri-
cal transformations at the frontiers mentioned and
formation of global tectonic structures of fluidoge-
nic type in those geological times. An idea appeared
that those structures also formed in the origin mo-
ments of blast-like dynamic cataclysms which at each
transformation frontier maintained the pulse outbursts
of geogenic energy to the surface. Its impacts lead to
jumps in the species composition and matter organi-
zation level of the organisms’ in the biosphere. Pro-
ceeding from those notions, we should to refer those
structures as geoenergogenic ones and to consider
them as a kind of fluidogenic structures.
So, we postulate a universal geoenergogenera-
ted mechanism both for the origination and evolu-
tion of the terrestrial life. Its action is maintained
due three casual-concession geoenergogenerated
phenomena (mutually subordinated, which periodi-
cally appeared through the geological time due the
rotational existence of the Earth and its energetic
interaction with the Space:
1) generation and accumulation of geogenic
energy surplus amounts in the Earth, which
provoke attempts of its liberation from the
closed space outward;
2) origination as a concession of it the blast-
like dynamic cataclysms with global origina-
tion of numerous fracture-like faults in the
lithosphere;
3) pulse breaks of geogenic energy surpluses onto
the surface through those faults and its power-
ful impacts into the matter world of the exo-
sphere. It is stated that through action of this
mechanism, 2,4 billion years ago the global
transformation of the exosphere’s organic com-
binations into primary forms of terrestrial live
matter took place in the first time at the Earth;
and jump-like changes of species composition
and organization complication of biosphere or-
ganisms’ matter were carried out at the trans-
formation frontiers of biological evolution.
References
Drozdovskaya A. A. Chemical Evolution of the Ocean
and Atmosphere in the Geological History of the Earth.
— Kiev: Nauk. dumka, 1990. — 208 p. (in Russian).
Drozdovskaya A. A. The Life: the Origin and evolu-
tion under Earth-Space energy interaction. — Kiev:
Simvol-T, 2009. — 334 p. (in Russian).
|
| id | nasplib_isofts_kiev_ua-123456789-101319 |
| institution | Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| issn | 0203-3100 |
| language | English |
| last_indexed | 2025-12-07T18:52:57Z |
| publishDate | 2010 |
| publisher | Інститут геофізики ім. С.I. Субботіна НАН України |
| record_format | dspace |
| spelling | Drozdovskaya, A. 2016-06-02T14:27:53Z 2016-06-02T14:27:53Z 2010 Geoenergogenerated dynamic cataclysms as the launch mechanism of the origin and evolution of the terrestrial life / A. Drozdovskaya // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 39-40. — Бібліогр.: 2 назв. — англ. 0203-3100 https://nasplib.isofts.kiev.ua/handle/123456789/101319 en Інститут геофізики ім. С.I. Субботіна НАН України Геофизический журнал Geoenergogenerated dynamic cataclysms as the launch mechanism of the origin and evolution of the terrestrial life Article published earlier |
| spellingShingle | Geoenergogenerated dynamic cataclysms as the launch mechanism of the origin and evolution of the terrestrial life Drozdovskaya, A. |
| title | Geoenergogenerated dynamic cataclysms as the launch mechanism of the origin and evolution of the terrestrial life |
| title_full | Geoenergogenerated dynamic cataclysms as the launch mechanism of the origin and evolution of the terrestrial life |
| title_fullStr | Geoenergogenerated dynamic cataclysms as the launch mechanism of the origin and evolution of the terrestrial life |
| title_full_unstemmed | Geoenergogenerated dynamic cataclysms as the launch mechanism of the origin and evolution of the terrestrial life |
| title_short | Geoenergogenerated dynamic cataclysms as the launch mechanism of the origin and evolution of the terrestrial life |
| title_sort | geoenergogenerated dynamic cataclysms as the launch mechanism of the origin and evolution of the terrestrial life |
| url | https://nasplib.isofts.kiev.ua/handle/123456789/101319 |
| work_keys_str_mv | AT drozdovskayaa geoenergogenerateddynamiccataclysmsasthelaunchmechanismoftheoriginandevolutionoftheterrestriallife |