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# This CITATION.cff file was generated with cffinit.
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# Visit https://bit.ly/cffinit to generate yours today!
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cff-version: 1.2.0
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title: >-
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Preservation of Orbital Forcing in Incomplete Carbonate
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Successions
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message: >-
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If you use this software, please cite it using the
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metadata from this file.
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type: software
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authors:
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- given-names: Niklas
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family-names: Hohmann
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affiliation: Utrecht University
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orcid: 'https://orcid.org/0000-0003-1559-1838'
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- given-names: Peter
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family-names: Burgess
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affiliation: University of Liverpool
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- given-names: David
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family-names: De Vleeschouwer
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affiliation: Westfälische Wilhelms-Universität Münster
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orcid: 'https://orcid.org/0000-0002-3323-807X'
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- given-names: Emilia Jarochowska
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affiliation: Utrecht University
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orcid: 'https://orcid.org/0000-0001-8937-9405'
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identifiers:
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- type: doi
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value: 10.5281/zenodo.8312823
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description: Poster and associated code deposited on Zenodo
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repository-code: >-
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https://github.com/MindTheGap-ERC/preservation-orbital-forcing-carbonate-successions
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abstract: >-
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Cyclostratigraphy has the potential to establish relative
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ages in sedimentary records with a temporal resolution
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greater than that of absolute dating methods such as
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radiometric dating. Though, stratigraphic incompleteness
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complicates this process and is a source for uncertainty
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in cyclostratigraphic age-depth models. As a result,
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cyclostratigraphic studies on sedimentary archives from
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pelagic and hemi-pelagic environments are usually less
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contested than those on more shallow-water sections. To
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better quantify the impact of stratigraphic incompleteness
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on cyclostratigraphic results, we first quantify
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stratigraphic completeness throughout a carbonate
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platform, and then assess the impact on the recorded
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Milanković signal.
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Two-dimensional dip-sections generated by CarboCAT models
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of carbonate platform growth forced with insulation-driven
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eustatic sea-level oscillations generate synthetic
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stratigraphic columns and proxy records, and these are
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analyzed for presence of an insolation signal using the
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astrochron package.
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Our results show that if sea-level is driven by a
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Milanković signal, shallow water carbonate successions
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with moderate incompleteness are capable of recording said
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signal. This suggests that under accommodation-forcing by
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a Milanković signal, cyclostratigraphy can help establish
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relative time scales in shallow water environments.
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keywords:
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- Stratigraphy
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- Cyclostratigraphy
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- Carbonate Sedimentology
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- Geology
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- Basin simulation
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- Orbital forcing
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- Milanković cyclicity
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- Milankovitch cyclicity
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- Carbonate platform
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- Sedimentology
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license: Apache-2.0

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