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Record W1966432379 · doi:10.1890/03-5047

OXYGEN ISOTOPE RATIOS OF WATERS AND RESPIRED CO <sub>2</sub> IN AMAZONIAN FOREST AND PASTURE ECOSYSTEMS

2005· article· en· W1966432379 on OpenAlexaff
Jean Pierre Ometto, Lawrence B. Flanagan, Luiz Antônio Martinelli, James R. Ehleringer

Bibliographic record

VenueEcological Applications · 2005
Typearticle
Languageen
FieldEnvironmental Science
TopicPlant Water Relations and Carbon Dynamics
Canadian institutionsUniversity of Lethbridge
Fundersnot available
Keywordsδ18OVapour Pressure DeficitEnvironmental sciencePastureEcosystemVegetation (pathology)Dry seasonIsotopes of oxygenEcologyAtmospheric sciencesHydrology (agriculture)Stable isotope ratioBiologyChemistryBotanyPhotosynthesisTranspirationGeology

Abstract

fetched live from OpenAlex

The oxygen isotope ratio (δ18O, SMOW) of atmospheric CO2 is a powerful indicator of large-scale CO2 exchange on land. Oxygen isotopic exchange between CO2 and water in leaves and soils controls the δ18O of atmospheric CO2. Currently there is little empirical information on the spatial and temporal variation in the δ18O of leaf and stem water in tropical ecosystems. We measured the seasonal dynamics of δ18O in atmospheric CO2 and water in different ecosystem compartments in both primary forest and pasture ecosystems in three different regions of the Amazonian Basin of Brazil (Ji-Paraná, Manaus, and Santarém). Within regions, the source (stem) water δ18O values for primary forests and pastures were similar; neither vegetation type exhibited distinct wet–dry season patterns. Daytime leaf water isotope ratios were strongly correlated with predictions of the Craig-Gordon model. The δ18O value of leaf water was positively correlated with leaf height above ground because of associated variation in vapor pressure deficit and the δ18O of atmospheric water vapor within forest canopies. Consistent with these observations, the δ18O value of leaf cellulose was positively correlated with forest height. Leaf water from pasture grasses was more 18O enriched than leaf water from forest vegetation. There was a tendency for daytime leaf water to be more enriched in 18O during the dry season, reflecting generally lower humidity conditions during the dry season. Nighttime measurements of the oxygen isotope ratio of ecosystem respired CO2 in both forest and pasture vegetation were not consistent with values expected for CO2 in equilibrium with stem (soil) water, despite nighttime vapor pressure deficits close to zero. Apparently, the δ18O of leaf water lagged and did not attain isotopic equilibrium at night. Thus, the deviation of nighttime δ18O values of ecosystem respiration from that expected from a CO2 efflux in equilibrium with soil (stem) water increased as δ18O values of ecosystem respiration became 18O enriched. Discrimination against CO2 containing 18O (ΔC18OO) during photosynthesis was calculated based on measured leaf water δ18O values. Forests had consistently higher modeled ΔC18OO values than pastures. The daytime isotope effects we calculate for photosynthesis and respiration were consistent with previous model predictions of a strong depletion of 18O in atmospheric CO2 over the Amazon Basin of Brazil.

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 score0.047
Threshold uncertainty score0.259

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)0.0000.000

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 head0.006
GPT teacher head0.195
Teacher spread0.190 · 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

Citations39
Published2005
Admission routes1
Has abstractyes

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