MétaCan
Menu
Back to cohort
Record W58681602

Salt marsh sedimentation over the past c. 120 years along the west Cotentin coast of Normandy (France): Relationship to sea-level rise and sediment supply

2003· article· en· W58681602 on OpenAlexaboutno aff
Simon K. Haslett, Andrew B. Cundy, C.F.C. Davies, E.S. Powell, Ian W. Croudace

Bibliographic record

VenueePrints Soton (University of Southampton) · 2003
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsnot available
Fundersnot available
KeywordsSalt marshMarshEstuaryGeologyOceanographySedimentAccretion (finance)Sea levelSedimentationBrackish marshBayGeomorphologySalinityWetlandBrackish waterEcology
DOInot available

Abstract

fetched live from OpenAlex

Natural high sediment supply to a number of macrotidal estuaries along the western coast of the Cotentin Peninsula (Normandy, France) is resulting in estuarine infilling. A previously published aerial survey in one estuary shows salt marsh laterally expanding at a rate of $4400m^ {2}/y$. Five sediment cores collected from salt marshes in three estuaries (Havre de Carteret, Havre de Surville, and Havre de Lessay) are used to investigate the relationship between lateral and vertical salt marsh accretion, and sea level. The cores are chemostratigraphically correlated with reference to is established by 210Pb and 137Cs dating of one of the cores, providing a chronologyextending back to $1880\pm23$. Through this period, mean vertical accretion rates for single cores from interior planar salt marsh surface sites at Surville and Lessay are 7.7 and 6.3mm/y respectively. Three cores from Carteret were taken from a seaward sloping salt marsh, one each from low, middle and high marsh settings, yielding mean vertical accretion rates of 5.5, 4.4, and 4.1 mm/y respectively. These data are compared with a regional rise in relative mean sea level (msl) of 3.9mm/y determined from a tide gauge on the nearby island of Jersey from 1952-2001. The high marsh at Carteret appears to be accreting relative position to msl, as there is no significant upcore change in the faunas. A core from Surville, however, indicates salt marsh emergence, demonstrated by transitions from sandflat to salt marsh faunas. The low marsh core from Cateret reveals a recent acceleration in vertical accretion (8mm/y since $1975\pm5$) and may be related to an increase in sediment availability due to the cessation of intertidal sand mining. This study demonstrates the long-term emergence of the Cotentin salt marshes, but suggests no general increase in vertical accretion despite increased sediment supply from recent mining cessation. Rather, newly available sediments support enhanced accretion along the marsh edge and rapid development of new marsh surface through lateral accretion. This study is in close agreement with a previous study of stilt marsh deposition from the macrotidal Bay of Fundy (Canada) that states high marsh accretion reflects sea-level or hydrological changes, whilst low marsh accretion is greatly influenced by changes in sediment supply. For future studies, knowledge of these relationships enables the selection of sites according to the aims of the investigation.

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)0.001
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 score0.005
Threshold uncertainty score0.997

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
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)0.0040.000

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 head0.020
GPT teacher head0.218
Teacher spread0.198 · 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

Citations23
Published2003
Admission routes1
Has abstractyes

Explore more

Same venueePrints Soton (University of Southampton)Same topicGeology and Paleoclimatology ResearchFrench-language works237,207