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Record W209239398

Paleoenvironmental analysis using thecamoebians and foraminifera in Mexican anchialine caves: a focus on Aktun Ha (Carwash) Mexico

2008· dissertation· en· W209239398 on OpenAlexfundno aff
Hengstum J. Peter Van

Bibliographic record

VenueMacSphere (McMaster University) · 2008
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsnot available
FundersNational Geographic SocietyNatural Sciences and Engineering Research Council of CanadaCushman Foundation for Foraminiferal Research
KeywordsForaminiferaCaveOceanographyGeologyFocus (optics)PaleontologyArchaeologyGeographyBenthic zone
DOInot available

Abstract

fetched live from OpenAlex

Thecamoebians (testate amoebae) and foraminifera have never been systematically investigated in a phreatic cave system. Foraminifera (marine to brackish water protists) and thecamoebians (brackish to freshwater protists) are cosmopolitan and have been studied in virtually all environments on Earth. Although foraminifera-bearing sediment has been observed from vadose cave environments in the last 20 years, there is no mention of their ecology - or mere existence - in flooded cave passages in any micropaleontology or microbiology textbooks. Only one published manuscript briefly mentions foraminifera in preliminary test samples from phreatic caves in Bermuda. The unprecedented ability of these organisms to colonize any environment on Earth led to the hypothesis that they are also exploiting global phreatic caves. The karst landscape of the Yucatan Peninsula, Mexico, is an ideal setting for the formation of anastomosing, anchialine, phreatic cave systems. The stratified aquifer contains passages in both the superior freshwater lens (thecamoebian habitat} and marine water (foraminifera habitat) intruding below, creating an ideal location to test the hypothesis. Several important contributions have resulted from investigating surface samples and cores in this region. (1) Using thirty-three surface samples from three different cenotes, thecamoebians and foraminifera were found living in the sinkhole (cenote) environment, which are the physical entrance into the caves. An ecological boundary of -3.5 ppt was determined for thecamoebians, with Centropyxis constricta "aerophilia" determined as the most euryhaline thecamoebian taxa. (2) Foraminifera and thecamoebians have been colonizing Carwash Cave since the Sangamon Interglacial (MIS 5e), based on seventy-five surface samples collected throughout the system. The recovered taxa have responded to changes in cave environment similarly to other coastal systems, thereby indicating their potential as paleoenvironmental proxies in phreatic caves. (3) In conjunction with stable isotopes (δ13Corg and δ15Norg), thecamoebians and foraminifera were successful recorders of mid-late Holocene paleoenvironmental evolution in Carwash Cave. An important salinity transition in the freshwater lens (from >2 ppt to 1.5 ppt) of the aquifer at ~2760 Cal yrs BP is coincident with changes in the local Maya populations, indicating a possible environmental linkage between ancient freshwater resources and Maya cultural genesis. This thesis demonstrates unequivocally that thecamoebians and foraminifera exist in phreatic cave systems and hold wider potential as paleoenvironmental proxies in other global phreatic caves.

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 machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Other · Consensus signal: none
Teacher disagreement score0.111
Threshold uncertainty score0.221

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.017
GPT teacher head0.218
Teacher spread0.201 · 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 source (direct Gemma or distilled Codex), not a consensus.

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

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
Published2008
Admission routes1
Has abstractyes

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