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Record W2347859162

Sequence Stratigraphic Correlation and Eustatic Events from Latest Cambrian to Early Early Ordovician between North China and Yangtze Platforms

2000· article· en· W2347859162 on OpenAlexaboutno aff
Wang Hai

Bibliographic record

VenueDicengxue zazhi · 2000
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsnot available
Fundersnot available
KeywordsOrdovicianGeologyPaleontologyMarine transgressionCoveBiostratigraphyStructural basinGeomorphology
DOInot available

Abstract

fetched live from OpenAlex

Four orthosequences have been recognized both from the Yeli Formation to the lower Liangjiashan Formation in northern and northeastern North China platform and from the upper Wuduhe Formation to the Fenxiang Formation in central Yangtze platform during the latest Cambrian to early Early Ordovician ( from the Fryxellodontus inornatus Subzone to Paltodus deltifer Zone ).δ 13 C value of carbonates from C.proavus Zone to C. angulatus Zone shows three rise and drop cyclic changes. Similar changes can be recognized during this interval in the δ 13 C profiles at Black Mountain, Australia, Lawson Cove , USA and Batyrbay , Kazakhstan .The simultaneous changes in carbon isotopes are useful in international correlation of the Cambrian Ordovician boundary strata . Based on the biostratigraphic data of conodonts and graptolites, and on the carbon isotopic stratigraphic data, four third order sequences could be well correlated on both platforms . During the latest Cambrian to early Early Ordovician ( from Fryxellodontus inornatus Subzone to Paltodus deltifer zone ), there existed 6 eustatic events : ( 1 ) the eustatic event ( equivalent to the Lange Ranch Eustatic Event in North America ) between the Fengshan Formation and the Yeli Formation, and in the upper part of the Wuduhe Formation (Lower C.proavus ; (2)the eustatic event between the First Member and the Second Member of the Yeli Formation and between the Wuduhe Formation and the Xilingxia Formation (between C. proavus Zone and C. intermedius Zone); (3) the regression event in the upper Xilingxia Formation on the Yangtzi platform (equivalent to the Aceroceras regression event in Australia);(4) the eustatic event between the Xilingxia Formation and the Nanjingguan Formation (between C. lindstromi Zone and C.angulatus Zone ), equivalent to the Black Mountain eustatic event in Australia; (5) the eustatic event between the Second Member and the Third Member of the Yeli Fomation, and between the Nanjingguan Formation and the Fenxiang Formation, the maximum transgression during Tremadocian occurred in the Psigraptus Zone to Adelograptus Zone; (6) the eustatic event between the lower and the middle Liangjiashan Formaion, and between the Fenxiang Formation and the Honghuayuan Formation (between Paltodus deltifer Zone and Serratognathus Zone) .At the Dayangcha section, in the lower C. lindstromi Zone which represents a maximum transgression period, there abundantly occurred the planktonic graptolite fauna of the Rhabdinopora flabelliformis parabola Zone which is significant for the global correlation. The maximum flood surface near this graptolite zone and below the FAD of C. prolindstromi could be taken as an important inference boundary for the Cambrian Or dovician Boundary. Iapeognathus fluctivagus in 23 bed of the Green Point section , Canada, has a limited distribution, and is not practical to be taken as an index fossil for the global correlation .

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)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.128
Threshold uncertainty score0.987

Codex and Gemma teacher scores by category

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

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 head0.014
GPT teacher head0.213
Teacher spread0.199 · 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.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
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

Citations4
Published2000
Admission routes1
Has abstractyes

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