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Record W3037067285 · doi:10.31274/etd-20200624-25

Late Quaternary paleoecology of the North American midcontinent

2020· dissertation· en· W3037067285 on OpenAlexaboutno aff
Hannah M. Carroll

Bibliographic record

Venuenot available
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsnot available
Fundersnot available
KeywordsVegetation (pathology)PaleoecologyQuaternaryGeologyPrecipitationPhysical geographyClimatologyPaleoclimatologyClimate changeGeographyPaleontologyOceanographyMeteorology

Abstract

fetched live from OpenAlex

Vegetation dynamics at regional to subcontinental scales are complex, and our understanding of the critical factors which govern them is far from complete. Temperature operates on a roughly longitudinal gradient across North America, while precipitation gradients are roughly latitudinal. What results is a complex climate space which is then further subdivided by topography, underlying geology, surface and subsurface hydrology, and seasonality, to name but a few, into broad-scale vegetation zones, or ecoregions. I used a combination of approaches to investigate climate and vegetation dynamics at multiple spatiotemporal scales, and to develop new tools to study past climate. Defining and delineating past ecoregions has long presented a challenge. Fossil pollen distinguishes between major biome types, i.e., grassland versus forest, with great success. However, distinguishing between prairie types at regional to subcontinental scales using the pollen record has been impossible. The ratio of Ambrosia (ragweed) to Artemisia (sagebrush, wormwood, mugwort) pollen has been shown to differentiate between tallgrass, mixed grass, and shortgrass prairie over a small portion of the modern Great Plains of North America. I extended that technique, and showed that the log-transformed Ambrosia to Artemisia ratio can reliably distinguish between subregions within the Great Plains, as well as regions immediately adjacent. In addition, I found that the relationship between Ambrosia and Artemisia pollen is best explained by precipitation rather than temperature, and that it produces reliable precipitation estimates when used to create models. This will allow for better reconstructions of past climate and improve delineations of past ecoregion boundaries. Pollen data are routinely used in paleoenvironmental studies to understand past climate and vegetation. One existing limitation in working with pollen data is the need to write code in order to execute several of the routine analyses in paleoecological work. I developed GeoPollen, a Shiny Dashboard application, to be a streamlined, user-friendly GUI-based tool for performing these basic analyses. Users are able to utilize more than 3,000 publicly available pollen datasets from the Neotoma Paleoecology Database spanning the last 22,000 years from the United States and Canada. GeoPollen performs a suite of common tasks on demand and generates diagnostics necessary for evaluating results. I developed GeoPollen in order to increase the openness and accessibility of late Quaternary pollen data. Boundaries between vegetation types are often highly sensitive to perturbations in climate. For example, the tallgrass prairie-temperate forest ecotone in Minnesota shifted rapidly and repeatedly during the mid-Holocene climate optimum, a warm

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 score0.863
Threshold uncertainty score0.273

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.013
GPT teacher head0.244
Teacher spread0.231 · 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

Citations0
Published2020
Admission routes1
Has abstractyes

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