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Record W2131220869 · doi:10.2110/jsr.2007.089

Recognition of the Sedimentary Architecture of Dryland Anabranching (Anastomosing) Rivers

2007· article· en· W2131220869 on OpenAlexaboutno aff
Colin P. North, Gerald C. Nanson, Simon D. Fagan

Bibliographic record

VenueJournal of Sedimentary Research · 2007
Typearticle
Languageen
FieldEnvironmental Science
TopicHydrology and Sediment Transport Processes
Canadian institutionsnot available
Fundersnot available
KeywordsGeologySedimentary rockArchitecturePaleontologyGeochemistryGeomorphologyArchaeologyGeography

Abstract

fetched live from OpenAlex

Abstract The application of rigorous criteria for identifying fluvial style from sedimentary deposits is crucial if environmental reconstructions from stratigraphy are to be reliable. From modern observations, it appears that anabranching (anastomosing) rivers can be divided into separate humid and dryland classes. Each class has dissimilar characteristics to the other, necessitating different criteria for their recognition in the rock record. The criteria being used by sedimentologists to recognize deposits of anabranching rivers are derived solely from modern examples in humid regions, heavily biased to a few specific cases in Canada. These criteria are dominated by the concept of ribbon sandstone bodies encased in fine-grained floodplain sediment, with an overall low sand-to-mud ratio in the succession. There has been a general failure to appreciate that dryland anabranching rivers have characteristics significantly different from these and almost certainly leave a sedimentary record quite dissimilar to that previously expected. Avulsion or obtrusion (the gradual formation of an alternative channel) are the characteristic dynamic of anabranching rivers, forming and maintaining coexisting multiple anabranch channels. Avulsion or obtrusion require stream banks to have a high resistance to erosion, usually achieved by cohesive bank sediments or the reinforcement of banks by vegetative root mats. In some drylands, riparian vegetation can be sparse and bank resistance may depend in large part on a high clay content. Here, channel fills are mud dominated and floodplains have a uniform fine-grained character which is usually structureless because of intense pedoturbation and some bioturbation. The evidence from such present-day dryland anabranching rivers suggests that their sedimentary record is likely to be one of laterally extensive mud-rich beds with weak or enigmatic fluvial indicators. Elsewhere, dryland anabranching systems are sand-dominated, their banks reinforced with riparian gallery forests sustained by infrequent flow and a shallow water table. Though the stratigraphy of these has barely been investigated, they are clearly different from humid-region anabranching systems, for their channels and islands are predominantly sandy. Anabranching rivers with prominent channel sandbodies separated by muddy islands have never been described from contemporary drylands. The interpretation of a dryland origin for ancient stratigraphic successions with this form is made, therefore, without evidence that they can actually exist. In the light of this, such interpretations should be reevaluated.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.004
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Bench or experimental · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.444
Threshold uncertainty score0.999

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0040.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.001
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0020.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.027
GPT teacher head0.293
Teacher spread0.267 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

Study designBench or experimental
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations60
Published2007
Admission routes1
Has abstractyes

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