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Record W339188483

Sedimentary Records of Mercury and Organic Matter in Canadian Lakes; Relationship between Climate Change and Contaminants

2010· article· en· W339188483 on OpenAlexaboutno aff
Hamed Sanei, P.M. Outridge, Gary A. Stern, Fei Wang, Fariborz Goodarzi

Bibliographic record

VenueEGUGA · 2010
Typearticle
Languageen
FieldEnvironmental Science
TopicMercury impact and mitigation studies
Canadian institutionsnot available
Fundersnot available
KeywordsSedimentary depositional environmentSedimentary rockArcticSedimentary organic matterClimate changeMercury (programming language)Organic matterBiogenic silicaGeologyGeologic recordSedimentKerogenEnvironmental scienceOceanographyPhysical geographyGeochemistryEcologySource rockPaleontologyGeographyStructural basin
DOInot available

Abstract

fetched live from OpenAlex

Recent studies in the remote pristine lakes in the Canadian High Arctic has shown that historical trends of mercury (Hg) are often paralleled with those of mainly algal-derived organic matter (OM) over past decades and centuries. This correlation is especially important during the latter half of the 20th Century when phytoplankton productivity increased by several orders of magnitude from historically low levels; suggesting that the dynamics and fate of Hg in High Arctic lakes may have been seriously confounded by increased algal productivity as the result of recent climate change. The important questions facing this hypothesis are (1) the degree that climate change and resulting algal productivity influence the Hg flux into the aquatic systems (2) whether or not this phenomena is limited to Arctic region and what is the role of depositional environment in the observed pattern (3) how atmospheric flux of Hg as related to the local/regional anthropogenic source(s) may influence the Hg-OM correlation observed in the sedimentary records. This study aims to answer some of these questions by examining the historical records of Hg and OM from 40 high-resolution lacustine/marine sediment cores representing a wide range of depositional environment, climatic, and geographical conditions across Canada. Organic geochemistry in conjunction with organic petrography provide unique information on the composition of sedimentary OM as defined by the source and type of kerogen. The results show that the nature of the relationship between sedimentary Hg and algal-derived OM may significantly change depending on the degree of Hg influx, and quantity and composition of the OM content of the sediments. It appears that OM, in particular, labile algal-derived OM primarily controls the Hg distribution in the sediments when the Hg influx (atmospheric deposition, runoff, etc) is within or close to background levels (e.g., as in Arctic lakes). When the Hg influx exhausts the capacity of OM scavenging (in the case of high anthropogenic input), excess Hg can be found in sediments, showing a clearly different temporal pattern to its organic counterpart. Only in these cases will sedimentary Hg profiles follow the history of anthropogenic Hg deposition. Given the relative homogeneity and paucity of OM in many Arctic and Sub-arctic lakes, small changes in climate may induce dramatic shifts in the rate of suspended OM scavenging of Hg, which is reflected in the sedimentary record of Hg.

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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.383
Threshold uncertainty score0.999

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 communication0.0000.000
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 head0.029
GPT teacher head0.259
Teacher spread0.230 · 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 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

Citations0
Published2010
Admission routes1
Has abstractyes

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