PARADOX IN STRATIGRAPHY
PARADOX IN STRATIGRAPHY:
WHERE ARE THE ANCIENT ROCKY LANDSCAPES AND SEASHORES?
When researching ancient rocky landscapes, we face a serious paradox. Ancient rocky seashores and true rocky landscapes are missing from the Paleozoic and Mesozoic eras. The ancient erosions surfaces are at odds with what we see today. They are mostly flat and lacking the normal erosion and alteration as we see in the present Earth. To tease your curiosity, we invited our readers to have a first look at these odd surfaces recorded along what we call the unconformities. An unconformity marks the limit between a younger sedimentary rock laid above an older eroded rock.
Early Jurassic layers overlaying vertical Paleozoic rocks. Roche Blain quarry, Normandy Credit: Geodoxa
Upper Jurassic overlaying Middle Jurassic, Utah. Credit: Copyright Thomas McGuire
Upper Permian overlaying Lower Carboniferous Kamsdorf, Saxony. Credit: Geodoxa
Early Jurassic layers overlaying vertical Paleozoic rocks. Roche Blain quarry, Normandy Credit: Geodoxa
Geologists with notions of geomorphology (the study of landforms) are baffled by the flatness of these rocky surfaces. These ancient unconformities should be adorned with
typical features of differential erosion whatever the climate conditions:
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Ribs shapes reliefs
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Stairsteps reliefs
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Etching effect on folded rocks
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Ribs shape accentuated by boring marine organisms in shallow water.
Ribs shape differential erosion on tipping strata. Bude, South of Wales. Credit Geodoxa
Ribs shape differential erosion on tipping strata. Bude, South of Wales. Credit Geodoxa
Differential erosion on Silurian rock with bioerosion by barnacles. Anticosti island, Quebec, Credit Geodoxa
Ribs shape differential erosion on tipping strata. Bude, South of Wales. Credit Geodoxa
Each stratum of layered rocks has its own resistance to alteration, waves abrasion, frost, and bioerosion. This effect, named differential erosion, affects all types of rock in any climatic conditions on earth today. Moreover, erosion of low reliefs would never evenly level rock strata. Even powerful waves abrasion is unable to sweep away the effect of differential erosion. Storm waves and torrents abrasion might blunt small reliefs, but differential erosion will always amplify its effect.
Blunt differential erosion on bedrock and slabs. Kimmeridge, UK. Credit Geodoxa
Blunt differential erosion. Millok Haven, UK. Credit Geodoxa
Blunt strata felted with algae. Anticosti Island, Quebec. Credit Geodoxa
Blunt differential erosion on bedrock and slabs. Kimmeridge, UK. Credit Geodoxa
The richness and beauty of our landscapes today are the result of differential erosion on a wide variety of strata. Nature is like an artist who needs time to sculpt his masterpiece of forms and colors. Rock surfaces exposed to an “aging” process give the best result.
The Paleozoic and Mesozoic unconformities are rather flat and dull with no traces of aging, depleted of differential erosion features. Instead, nature was generating super razing/bulldozing events, unlike anything we see today. In the end, we would have to doubt seriously about the uniformitarian doctrine.
In Ice or Water? 1905, Sir Henry Howorth raised the question by the following statement:
"The absence of the erosive agency of water, as manifested in cutting valleys and gorges in the under strata of the earth, is fatal to the theory that each formation has successively emerged from the sea and become the surface of the habitable world . . . What we want to see is a plain instance of valleys excavated and mountains formed in the ancient strata of the earth as we find them existing in the present day . . . "
Surprisingly, when geologists are exposed to this controversy, they admit the reality of a paradox. Unfortunately, this debate was ignored in the arena of earth science.
Many geology students have been taught that flat unconformities are simply the result of long periods of erosion into peneplains by a process named peneplanation.
Some geomorphologists might insist that long periods of regression and erosion would turn our continents into a vast “peneplane-unconformity”. As we will see this is just a desperate hypothesis that does not fit with the daily processes occurring on our modern continents.
Principles in geomorphology and stratigraphy
The following slideshow presents how a continent should be eroded according to the processes observed today. At any moment of this long process, our nature artist would always produce differential erosion masterpiece on any rock surface.
To illustrate this concept, we use 6 artistic licenses:
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The vertical scale is exaggerated.
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The continent is a cake built of ancient horizontal rock strata.
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The sea level is fixed with no fluctuation.
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No continent rebounds from the unloading erosion.
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No sinking of the continental margin under the overload of sediment.
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Orogeny or epeirogeny are omitted for this example.
Through time, erosion warns down the relief into detritus which are transported and laid down as sediment deposits at the margin. It is well established that the continent would be flattened if no uplifting tectonic force came into play.
Some geomorphologists might insist that a total flattening would transform a continent into what we call a peneplain. As we will see this is just a desperate hypothesis that does not fit with the nature of our continental crust. Meanwhile, the peneplanation process was prized by some stratigraphers to explain the odd aspect of the ancient unconformities. This concept is just an escape door to ignore the paradox concerning this webpage.
For some, a peneplain occurs when a continent is warned out to its base level (≈ sea level) then, erosion stops. At any moment up to the end, the continent's surface will bear the stairsteps aspect produced by differential erosion.
Today, flat lands are fluvial plains that are formed by sediment deposition, not by bedrock erosion. The only eroded flat bedrock on earth is Hudson Bay. Even there, the ice age abrasion left reliefs adorned with differential erosion. So, we find no modern examples of the “so-called” peneplains.
Folded Precambrian dolomites eroded differentially. Belcher (Sanikiluaq) islands, Hudson Bay. Credit: Mike Beauregard
Folded Precambrian dolomites eroded differentially. Belcher (Sanikiluaq) islands, Hudson Bay. Credit: Mike Beauregard
Seashores processes
The next slideshow presents a cross-section at one stage of this process. Erosion of the continent was omitted. The new sediment deposits cover a rocky seashore already sculpted with differential erosion. This sort of landscape burial occurs often during a sea rise, called a transgression. This surface will become a future unconformity. Strange enough, such an example belongs almost exclusively to our modern time (Pleistocene, Pliocene). We emphasize that such modern unconformity should have been ubiquitous throughout Earth's history.
The red dash line indicates a future unconformity.
In the above example, we insist on a sort of stairsteps seashore. This is not just due to the stratified aspect of the rocks. Because of the hydrodynamics of waves, even a very gradual rise of the sea level will always produce a series of ramps or terraces. This is well-known by coastal geomorphologists and geographers.
UBIQUITOUS COSTAL TERRACES
In the following example, you see a theoretical continent made of a homogeneous rock, like a granite dome. With the freedom of an artistic license:
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Continental fluvial erosion was omitted
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Sediment deposits were omitted except for the beach deposits.
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The last slide shows the relief without seawater.
Notice the fractal aspect of the shoreline carved with caps, bays, and terraces.
Following the Ice Age melt, a worldwide sea transgression had drowned innumerable “stairsteps” seashores. Buried under new sediments, these submarine rocky seashores become modern unconformities. All geologists should be astounded by the absence of stairsteps topography along Paleozoic and Mesozoic unconformities.
Mechanical rock abrasion does not occur under the sea level at a depth unreached by the waves’ amplitude. The chemical alteration has almost no effect on deeply drowning rock surface. The hydrothermal alteration would be efficient around the volcanic areas like the ocean ridge or the guyots. Bioerosion is efficient mainly above 200 m of depth where light sustain an ecosystem. To resume, landscapes are shaped when a regressing sea (a regression) exposes the rocky surface. The usual sequence is:
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During a regression, atmospheric agents produce a rocky landscape.
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During a transgression, the sea drowns and preserve the rocky landscape.
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New marine sediments deposits seal the rocky landscape as a future unconformity.
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The erosion of a new regression will expose the unconformity in the present time.
Keep in mind that the sea might transgress over 3 types of surface:
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A hard-rocky surface which will produce a true unconformity.
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Soft sediment deposits like a fluvial plain which will produce a paraconformity or a hiatus or a blended unconformity.
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A poorly lithified sedimentary rock like the one of badlands topography which will produce paraconformity or blended unconformity.
Many, not all, Paleozoic and Mesozoic unconformities are clearly of the first type.
The following example illustrates a sea regression exposing 2 types of rock followed by a transgression. The underlayers are a well-lithified limestone. The layers above are poorly lithified sediment typical of many badlands. Differential erosion is less defined. The topography is round and scourged by ravines and gullies.
The layers above are poorly lithified sediment. The underlayers are a well-lithified limestone.
Regression of the sea, a new landscape is expose to weathering.
The Painted Desert is a typical badland landscape. Petrified Forest National Park, Arizona. Credit: Adbar
The layers above are poorly lithified sediment. The underlayers are a well-lithified limestone.
Around the world, badlands are mostly carved in sedimentary rocks deposited at the end of the Mesozoic era (Cretaceous) and during the Cenozoic era. Remember that this is not an exclusive rule for that many well lithified sedimentary rocks are of the same ages. The degree of lithification depends on the chemistry of the sediments and their burial pressure.
The following slideshow helps to visualize how a transgressing shoreline would carve and dissolve a badland like Bryce Canyon. It is likely that the resulting unconformity would be a sort of paraconformity or a blended unconformity.
Credit: Jean-Christophe BENOIST
Credit: Jean-Christophe BENOIST
Since the work of Laurence Sloss on sequential stratigraphy, we know that our continents were deeply eroded many times during the Phanerozoic Eon (Paleozoic, Mesozoic, and Cenozoic eras).
Geologists are aware that the stratal expression and time of earth history had far more gaps than the fossils and rock records:
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90% in unconformities: gaps of the vanished records.
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10% in precious fossils and sedimentary records.
The erosion is so deep that the Paleozoic and Mesozoic seas were transgressing mostly over hard-rocky surfaces. Because of this, we expect that most of these unconformities should be sculpted with stairsteps series of terraces capped with shingle beaches. Rocky shores should be more predominant than terrestrial rocky landscapes.
The next slideshow presents the reality of our present nature AND NOT AN EXPRESSION OF THE ENIGMATIC PAST.
1- Platform carved by wave abrasion
2- Shore deposits: sand or/and shingle beach
9- Blue dotted line indicates the vanished terrestrial topography
1- Platform carved by wave abrasion
Uniformitarianism faces a serious appraisal:
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Rocky seashores are inexistent.
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Shingle beaches are inexistent.
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True rocky landscapes are none.
We must admit that our present nature is mocking our uniformitarian paradigms.
Many earth scientists are unaware that the actual uniformitarian tendency is a misleading path. Whoever enters this debate, he better be a well-known champion with decades of publications with a long emeritus professorate.
Derek Ager had such a solid authority when he published The nature of the stratigraphical record in 1973 (first edition). All stratigraphy geologists remember how his book was a challenge to uniformitarianism. Following his 3rd editions, antagonists were still unable to counterattack his view and, Ager decided to publish his new book with a more provocative title: The New Catastrophism — The importance of the rare event in geological history, 1993.
His publications had surely contributed to the recognition of great mass extinctions by the new generation of paleontologists. Curiously and understandably, Ager never treated the topics of the missing paleo landscapes, a discipline for geomorphologists. Meanwhile, he reminds his reader of an unsolved mystery related to ancient unconformity when he cited the work of Markes Johnson: Why Are Ancient Rocky Shores so Uncommon? 1988.
We might ask why geomorphologists are not so involved in studying the rocky surfaces along the ancient unconformities? The answer is simple: These surfaces are simply not rocky landscapes. This study is out of the competence of geomorphologists. There is a need for a new discipline; “cataclysmic erosiology”. Unfortunately for erosiologists, and fortunately for the inhabitants of our planets, there are not too many modern catastrophic erosional events to study.
The Geodoxa’s pages on the Ice Age outbursts are very relevant to the lack of interests in the topic. This is pure erosiology. While hydrodynamic engineers and physicists are very supportive of the subglacial water theory, many Ice Age geoscientists keep a bias attitude.
Coming next... Under construction
The shortcoming of karstic caves
During a transgression, lime deposit became limestone.
Regression. The limestone is expose to weathering.
A "fossilized karst" is a paleokarst.
During a transgression, lime deposit became limestone.
No rocky landscapes with dinosaurs
Dinosaurs standing on a flood plain
The sea regresses. Occasionally, dinosaurs stand on dry land. These islands are still soft ground not lithified yet.
Dinosaurs standing on a flood plain
The odd aspect of the Siccar Point unconformity
Synsedimentary tectonics
Carboniferous coal deposits:
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So many transgressions and regressions
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So many eroded channels in soft banks
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No differentially eroded rock surface!
Uniformitarianism
Many unconscious ad hoc