ANCIENT INQUIRY
AT-1178

Formation of Holocene limestone sequences by progradation, cementation, and erosion; two examples from the Bahamas

DOI · Academic research

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Source record

This is one canonical bibliographic record with topic-scoped research-use entries. It does not reproduce the paper, book, text, dataset, image, or manuscript and does not imply that full text was reviewed.
Canonical source ID
AT-1178
Accepted usage IDs
AT-1178
Types
DOI
Roles
Academic research
Verification
verified
Archive state
unavailable-through-registered-public-or-tdm-routes
Access
unavailable-through-registered-public-or-tdm-routes
Rights
not identified; not cleared
Public reproduction
Not cleared; citation and link only.
Correction / retraction
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Recorded research uses

AT-1178

Bimini Road

Why Ancient Inquiry uses this citation here

André Strasser and Eric Davaud's peer-reviewed Bahamian carbonate study; use as regional process context for Holocene cementation and erosion, not as a Bimini Road artifact report unless the relevant locality is verified in the full text.

What this usage does not establish

Bibliographic verification does not by itself establish that the full text was read.
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Topics citing it and claims using it

Supporting citation for public claim

The strongest cataloged geological interpretation treats Bimini Road as naturally formed and fractured beachrock.

Answer / theory: The strongest evidence says it is natural beachrock. What supports it: Carbonate beachrock formation and natural fracture patterns. What is weak or disputed: Visual regularity keeps the artificial claim alive. Evidence level: Strong Evidence for natural formation; Weak Evidence for construction.
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Limiting / critical citation for public claim

The claim that Bimini Road is an ancient built road, harbor feature, or Atlantis ruin is unsupported by the cataloged beachrock and corrective literature.

The evidence does not automatically support broader causal, technological, transmission, or literalizing claims beyond the cited record.
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Formation of Holocene limestone sequences by progradation, cementation, and erosion; two examples from the Bahamas

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