{"id":4743,"date":"2018-09-06T21:04:51","date_gmt":"2018-09-06T19:04:51","guid":{"rendered":"https:\/\/sites.uclouvain.be\/slim\/testwordpress\/?page_id=4743"},"modified":"2023-03-05T16:10:13","modified_gmt":"2023-03-05T15:10:13","slug":"bahamas","status":"publish","type":"page","link":"https:\/\/www.slim-ocean.be\/index.php\/bahamas\/","title":{"rendered":"Modelling whitings formation on the Great Bahama Bank"},"content":{"rendered":"<p>The Great Bahama Bank (GBB) is one of the largest sites of shallow-water carbonate production on Earth. It is currently thought that between 50 and 70% of the carbonate muds produced on the platform originate from inorganic and\/or bio-induced drifting patches of fine-grained aragonite (CaCO3), the so-called whitings. However, whitings have remained a sedimentological enigma for the last 80 years and explanation of their formation mechanism is still controversial. Nonetheless, the underlying process is assumed to result from an intricate bio-physico-chemical coupling between microbial communities, water circulation and chemistry.<\/p>\n<p>SLIM2D has been used to simulate currents on the shallow platform and study bottom-sediments resuspension, as the resuspended material is thought to be used as nucleation points for carbonate precipitation. The resulting current velocities are shown below. One may observe large-scale circulations features such as the Gulf Stream along Florida coastlines as well as small-scale features on the Great Bahama Bank.<\/p>\n<p><iframe loading=\"lazy\" width=\"843\" height=\"474\" src=\"https:\/\/www.youtube.com\/embed\/Mvnuysnj-C0?feature=oembed\" frameborder=\"0\" allow=\"accelerometer; autoplay; encrypted-media; gyroscope; picture-in-picture\" allowfullscreen><\/iframe><\/p>\n<p>Moreover, interactions between platform-top and off-platform waters are studied as they have an influence on the aragonite saturation state of waters on the GBB. These interactions are studied by the mean of three tools: the computation of water fluxes through the platform margin, the use of a Lagrangian particle tracker and the computation of the age of waters using the Eulerian transport module of the model.<\/p>\n<h4>External collaborators<\/h4>\n<p>Dr Matthieu Le H\u00e9naff (NOAA and University of Miami), Dr Amanda Oehlert (University of Miami) and Prof. Sam Purkis (University of Miami),<\/p>\n<h4>To learn more&#8230;<\/h4>\n<div id=\"zotpress-bf90e1115917a8e8af5de35f3b994ce2\" class=\"zp-Zotpress zp-Zotpress-Bib wp-block-group\">\n\n\t\t<span class=\"ZP_API_USER_ID ZP_ATTR\">778265<\/span>\n\t\t<span class=\"ZP_ITEM_KEY ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_COLLECTION_ID ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_TAG_ID ZP_ATTR\">bahamas<\/span>\n\t\t<span class=\"ZP_AUTHOR ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_YEAR ZP_ATTR\"><\/span>\n        <span class=\"ZP_ITEMTYPE ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_INCLUSIVE ZP_ATTR\">1<\/span>\n\t\t<span class=\"ZP_STYLE ZP_ATTR\">apa<\/span>\n\t\t<span class=\"ZP_LIMIT ZP_ATTR\">50<\/span>\n\t\t<span class=\"ZP_SORTBY ZP_ATTR\">date<\/span>\n\t\t<span class=\"ZP_ORDER ZP_ATTR\">desc<\/span>\n\t\t<span class=\"ZP_TITLE ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_SHOWIMAGE ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_SHOWTAGS ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_DOWNLOADABLE ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_NOTES ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_ABSTRACT ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_CITEABLE ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_TARGET ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_URLWRAP ZP_ATTR\"><\/span>\n\t\t<span class=\"ZP_FORCENUM ZP_ATTR\"><\/span>\n        <span class=\"ZP_HIGHLIGHT ZP_ATTR\"><\/span>\n        <span class=\"ZP_POSTID ZP_ATTR\">4743<\/span>\n\t\t<span class=\"ZOTPRESS_PLUGIN_URL ZP_ATTR\">https:\/\/www.slim-ocean.be\/wp-content\/plugins\/zotpress\/<\/span>\n\n\t\t<div class=\"zp-List loading\">\n\t\t\t<div class=\"zp-SEO-Content\">\n\t\t\t\t<span class=\"ZP_JSON ZP_ATTR\">%7B%22status%22%3A%22success%22%2C%22updateneeded%22%3Afalse%2C%22instance%22%3Afalse%2C%22meta%22%3A%7B%22request_last%22%3A0%2C%22request_next%22%3A0%2C%22used_cache%22%3Atrue%7D%2C%22data%22%3A%5B%7B%22key%22%3A%22V6TLSQ66%22%2C%22library%22%3A%7B%22id%22%3A778265%7D%2C%22meta%22%3A%7B%22lastModifiedByUser%22%3A%7B%22id%22%3A6462585%2C%22username%22%3A%22MiguelDLC%22%2C%22name%22%3A%22%22%2C%22links%22%3A%7B%22alternate%22%3A%7B%22href%22%3A%22https%3A%5C%2F%5C%2Fwww.zotero.org%5C%2Fmigueldlc%22%2C%22type%22%3A%22text%5C%2Fhtml%22%7D%7D%7D%2C%22creatorSummary%22%3A%22Purkis%20et%20al.%22%2C%22parsedDate%22%3A%222023-03-31%22%2C%22numChildren%22%3A1%7D%2C%22bib%22%3A%22%26lt%3Bdiv%20class%3D%26quot%3Bcsl-bib-body%26quot%3B%20style%3D%26quot%3Bline-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%26quot%3B%26gt%3B%5Cn%20%20%26lt%3Bdiv%20class%3D%26quot%3Bcsl-entry%26quot%3B%26gt%3BPurkis%2C%20S.%20J.%2C%20Oehlert%2C%20A.%20M.%2C%20Dobbelaere%2C%20T.%2C%20Hanert%2C%20E.%2C%20%26amp%3B%20Harris%2C%20P.%20%28Mitch%29.%20%282023%29.%20Always%20a%20White%20Christmas%20in%20the%20Bahamas%3A%20temperature%20and%20hydrodynamics%20localize%20winter%20mud%20production%20on%20Great%20Bahama%20Bank.%20%26lt%3Bi%26gt%3BJournal%20of%20Sedimentary%20Research%26lt%3B%5C%2Fi%26gt%3B%2C%20%26lt%3Bi%26gt%3B93%26lt%3B%5C%2Fi%26gt%3B%283%29%2C%20145%26%23x2013%3B160.%20%26lt%3Ba%20class%3D%26%23039%3Bzp-DOIURL%26%23039%3B%20href%3D%26%23039%3Bhttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.2110%5C%2Fjsr.2022.066%26%23039%3B%26gt%3Bhttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.2110%5C%2Fjsr.2022.066%26lt%3B%5C%2Fa%26gt%3B%26lt%3B%5C%2Fdiv%26gt%3B%5Cn%26lt%3B%5C%2Fdiv%26gt%3B%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Always%20a%20White%20Christmas%20in%20the%20Bahamas%3A%20temperature%20and%20hydrodynamics%20localize%20winter%20mud%20production%20on%20Great%20Bahama%20Bank%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Sam%20J.%22%2C%22lastName%22%3A%22Purkis%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Amanda%20M.%22%2C%22lastName%22%3A%22Oehlert%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Thomas%22%2C%22lastName%22%3A%22Dobbelaere%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Emmanuel%22%2C%22lastName%22%3A%22Hanert%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Paul%20%28Mitch%29%22%2C%22lastName%22%3A%22Harris%22%7D%5D%2C%22abstractNote%22%3A%22Whitings%2C%20or%20occurrences%20of%20%5Cufb01ne-grained%20carbonate%20in%20the%20water%20column%2C%20have%20been%20observed%20in%20modern%20environments%20with%20salinities%20ranging%20from%20fresh%20to%20marine%20conditions%2C%20and%20thick%20deposits%20of%20lime%20mud%20are%20described%20throughout%20the%20geological%20record.%20Despite%20their%20ubiquity%2C%20the%20trigger%20for%20whitings%20has%20been%20debated%20for%20more%20than%20eighty%20years.%20Satellite%20data%20reveal%20that%20most%20whitings%20are%20restricted%20to%20the%20northwestern%20part%20of%20Great%20Bahama%20Bank%20%28GBB%29%20which%20occupies%20%2C%2010%25%20of%20the%20platform%20area.%20Even%20here%2C%20whitings%20are%20further%20focused.%20More%20than%2035%25%20of%20them%20occur%20in%20a%20zone%20which%20occupies%20just%201%25%20of%20the%20platform.%20We%20propose%20a%20three-step%20process%20for%20the%20existence%20of%20this%20zone%20of%20peak%20whitings%20and%20why%20the%20whitings%20in%20it%20are%20both%20more%20frequent%20and%20larger%20in%20winter%20than%20summer.%20First%2C%20the%20temperature%20differential%20between%20on-%20and%20off-platform%20waters%20is%20highest%20in%20the%20winter%2C%20setting%20up%20a%20disparity%20between%20dissolved%20CO2%20concentrations%20in%20the%20two%20water%20masses.%20Second%2C%20hydrodynamic%20mixing%20of%20these%20two%20water%20masses%20increases%20the%20degree%20of%20aragonite%20saturation%20of%20the%20platform-top%20waters%2C%20as%20colder%20on-platform%20waters%20with%20theoretically%20higher%20concentrations%20of%20dissolved%20gases%20are%20warmed%20via%20mixing%20with%20the%20warmer%20off-platform%20waters.%20Finally%2C%20spatial%20heterogeneity%20in%20the%20degree%20of%20aragonite%20saturation%20is%20higher%20in%20the%20winter%2C%20and%20the%20zone%20of%20peak%20whitings%20is%20situated%20in%20an%20area%20of%20locally%20enhanced%20saturation%20state.%20Hydrodynamic%20simulation%20suggests%20that%20the%20whitings%20zone%20is%20located%20by%20tidal%20in%5Cufb02ow%20of%20off-platform%20waters%20across%20the%20western%20margin%20of%20GBB%2C%20as%20well%20as%20in%5Cufb02ow%20from%20the%20Tongue%20of%20the%20Ocean%20to%20the%20north%20of%20Andros%20Island.%20Despite%20thermodynamic%20forcing%20mechanisms%20that%20predict%20higher%20frequency%20of%20whitings%20in%20the%20summer%2C%20the%20environmental%2C%20hydrodynamic%2C%20geochemical%2C%20and%20kinetic%20conditions%20in%20the%20whitings%20zone%20appear%20to%20support%20the%20Goldilocks%20con%5Cufb01guration%20that%20enhances%20the%20formation%20of%20wintertime%20whitings%20on%20Great%20Bahama%20Bank.%20This%20phenomenon%20has%20implications%20for%20the%20interpretation%20of%20whitings%20mud%20in%20the%20geological%20record%2C%20including%20the%20geochemical%20signatures%20within%20it.%22%2C%22date%22%3A%222023-03-31%22%2C%22section%22%3A%22%22%2C%22partNumber%22%3A%22%22%2C%22partTitle%22%3A%22%22%2C%22DOI%22%3A%2210.2110%5C%2Fjsr.2022.066%22%2C%22citationKey%22%3A%22purkisAlwaysWhiteChristmas2023%22%2C%22url%22%3A%22https%3A%5C%2F%5C%2Fpubs.geoscienceworld.org%5C%2Fjsedres%5C%2Farticle%5C%2F93%5C%2F3%5C%2F145%5C%2F620896%5C%2FAlways-a-White-Christmas-in-the-Bahamas%22%2C%22PMID%22%3A%22%22%2C%22PMCID%22%3A%22%22%2C%22ISSN%22%3A%221938-3681%2C%201527-1404%22%2C%22language%22%3A%22en%22%2C%22collections%22%3A%5B%22GJSQZPDC%22%5D%2C%22dateModified%22%3A%222026-02-16T13%3A06%3A05Z%22%7D%7D%2C%7B%22key%22%3A%22PFFJ4E5Q%22%2C%22library%22%3A%7B%22id%22%3A778265%7D%2C%22meta%22%3A%7B%22lastModifiedByUser%22%3A%7B%22id%22%3A6462585%2C%22username%22%3A%22MiguelDLC%22%2C%22name%22%3A%22%22%2C%22links%22%3A%7B%22alternate%22%3A%7B%22href%22%3A%22https%3A%5C%2F%5C%2Fwww.zotero.org%5C%2Fmigueldlc%22%2C%22type%22%3A%22text%5C%2Fhtml%22%7D%7D%7D%2C%22creatorSummary%22%3A%22Lopez%5Cu2010Gamundi%20et%20al.%22%2C%22parsedDate%22%3A%222022%22%2C%22numChildren%22%3A1%7D%2C%22bib%22%3A%22%26lt%3Bdiv%20class%3D%26quot%3Bcsl-bib-body%26quot%3B%20style%3D%26quot%3Bline-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%26quot%3B%26gt%3B%5Cn%20%20%26lt%3Bdiv%20class%3D%26quot%3Bcsl-entry%26quot%3B%26gt%3BLopez%26%23x2010%3BGamundi%2C%20C.%2C%20Dobbelaere%2C%20T.%2C%20Hanert%2C%20E.%2C%20Harris%2C%20P.%20M.%2C%20Eberli%2C%20G.%2C%20%26amp%3B%20Purkis%2C%20S.%20J.%20%282022%29.%20Simulating%20sedimentation%20on%20the%20Great%20Bahama%20Bank%20%26%23x2013%3B%20Sources%2C%20sinks%20and%20storms.%20%26lt%3Bi%26gt%3BSedimentology%26lt%3B%5C%2Fi%26gt%3B%2C%20%26lt%3Bi%26gt%3B69%26lt%3B%5C%2Fi%26gt%3B%287%29%2C%202693%26%23x2013%3B2714.%20%26lt%3Ba%20class%3D%26%23039%3Bzp-DOIURL%26%23039%3B%20href%3D%26%23039%3Bhttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1111%5C%2Fsed.13020%26%23039%3B%26gt%3Bhttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1111%5C%2Fsed.13020%26lt%3B%5C%2Fa%26gt%3B%26lt%3B%5C%2Fdiv%26gt%3B%5Cn%26lt%3B%5C%2Fdiv%26gt%3B%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Simulating%20sedimentation%20on%20the%20Great%20Bahama%20Bank%20%5Cu2013%20Sources%2C%20sinks%20and%20storms%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Cecilia%22%2C%22lastName%22%3A%22Lopez%5Cu2010Gamundi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Thomas%22%2C%22lastName%22%3A%22Dobbelaere%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Emmanuel%22%2C%22lastName%22%3A%22Hanert%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Paul%20M.%22%2C%22lastName%22%3A%22Harris%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Gregor%22%2C%22lastName%22%3A%22Eberli%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Sam%20J.%22%2C%22lastName%22%3A%22Purkis%22%7D%2C%7B%22creatorType%22%3A%22editor%22%2C%22firstName%22%3A%22Tracy%22%2C%22lastName%22%3A%22Frank%22%7D%5D%2C%22abstractNote%22%3A%22This%20study%20developed%20a%20high-%5Cufb01delity%20hydrodynamic%20simulation%20of%20sediment%20production%2C%20transport%20and%20deposition%20for%20the%20Great%20Bahama%20Bank.%20This%20model%20was%20run%20with%20a%20time-step%20of%2015%20min%20for%20the%20entirety%20of%202016%2C%20forced%20by%20tides%2C%20off-platform%20circulation%20and%20wind.%20Encompassed%20in%20this%20run%20are%20364%20days%20of%20fair-weather%20conditions%20and%20two%20days%20when%20the%20passage%20of%20Category%204%20Matthew%20brought%20hurricane-force%20winds%20to%20the%20platform.%20This%20simulation%20therefore%20offers%20an%20excellent%20opportunity%20to%20contrast%20the%20sway%20of%20fair-weather%20and%20storm-weather%20conditions%20on%20sculpting%20the%20facies%20arrangement%20atop%20this%20100%20000%20km2%20shallow-water%20carbonate%20platform.%20The%20work%20suggests%20that%20fairweather%20conditions%20are%20suf%5Cufb01cient%20to%20deliver%20the%20platform%5Cu2019s%20broad-scale%20facies%20patterns.%20Even%20the%20lethargic%20currents%20of%20the%20platform%20interior%20can%20move%20mud%20%28%26lt%3B63%20%5Cu03bcm%29%20over%20200%20km%20from%20its%20source%20over%20the%20course%20of%20one%20year.%20Intense%20focusing%20of%20tidal%20currents%20between%20islands%20and%20close%20to%20the%20platform%20margin%20are%20ample%20to%20move%20coarse%20grains%20%28%26gt%3B450%20%5Cu03bcm%29%2C%20at%20least%20locally%2C%20as%20is%20necessary%20to%20produce%20the%20vast%20ooid%20fairways%20for%20which%20the%20Great%20Bahama%20Bank%20is%20famed.%20Even%20at%20the%20height%20of%20Hurricane%20Matthew%2C%20average%20current%20speeds%20in%20these%20tidally-dominated%20areas%20do%20not%20exceed%20the%20speeds%20simulated%20for%20fairweather%20conditions.%20Hence%2C%20the%20hurricane%20has%20negligible%20effect%20in%20these%20highenergy%20areas.%20The%20hurricane%20does%20not%20have%20zero%20impact%2C%20though.%20For%20up%20to%20110%20km%20either%20side%20of%20the%20storm%5Cu2019s%20track%2C%20winds%20exceeding%2026%20m%5C%2Fs%20induce%20currents%20that%20winnow%20mud%20over%20longer%20distances%20than%20delivered%20by%20fair-weather%20conditions.%20Hence%2C%20the%20storm%20has%20a%20sedimentological%20signature%20which%2C%20albeit%20minor%2C%20might%20propagate%20into%20the%20depositional%20architecture%20of%20the%20platform%20when%20scaled%20over%20many%20storms%20through%20geological%20time.%20This%20work%20informs%20on%20the%20role%20of%20uniformitarianism%20versus%20catastrophism%20on%20carbonate%20sedimentation%20and%20casts%20doubt%20on%20geological%20interpretations%20of%20coarse-grained%20storm%20deposits%20%28tempestites%29%20atop%20shallow-water%20platforms.%22%2C%22date%22%3A%2212%5C%2F2022%22%2C%22section%22%3A%22%22%2C%22partNumber%22%3A%22%22%2C%22partTitle%22%3A%22%22%2C%22DOI%22%3A%2210.1111%5C%2Fsed.13020%22%2C%22citationKey%22%3A%22lopez-gamundiSimulatingSedimentationGreat2022%22%2C%22url%22%3A%22https%3A%5C%2F%5C%2Fonlinelibrary.wiley.com%5C%2Fdoi%5C%2F10.1111%5C%2Fsed.13020%22%2C%22PMID%22%3A%22%22%2C%22PMCID%22%3A%22%22%2C%22ISSN%22%3A%220037-0746%2C%201365-3091%22%2C%22language%22%3A%22en%22%2C%22collections%22%3A%5B%22GJSQZPDC%22%5D%2C%22dateModified%22%3A%222026-02-16T13%3A06%3A05Z%22%7D%7D%5D%7D<\/span>\n\n\t\t\t\t<div id=\"zp-ID-4743-778265-V6TLSQ66\" data-zp-author-date='Purkis-et-al.-2023-03-31' data-zp-date-author='2023-03-31-Purkis-et-al.' data-zp-date='2023-03-31' data-zp-year='2023' data-zp-itemtype='journalArticle' class=\"zp-Entry zpSearchResultsItem\">\n<div class=\"csl-bib-body\" style=\"line-height: 2; padding-left: 1em; text-indent:-1em;\">\n  <div class=\"csl-entry\">Purkis, S. J., Oehlert, A. M., Dobbelaere, T., Hanert, E., & Harris, P. (Mitch). (2023). Always a White Christmas in the Bahamas: temperature and hydrodynamics localize winter mud production on Great Bahama Bank. <i>Journal of Sedimentary Research<\/i>, <i>93<\/i>(3), 145\u2013160. <a class='zp-DOIURL' href='https:\/\/doi.org\/10.2110\/jsr.2022.066'>https:\/\/doi.org\/10.2110\/jsr.2022.066<\/a><\/div>\n<\/div>\n\t\t\t\t<\/div><!-- .zp-Entry .zpSearchResultsItem -->\t\t\t\t<div id=\"zp-ID-4743-778265-PFFJ4E5Q\" data-zp-author-date='Lopez\u2010Gamundi-et-al.-2022' data-zp-date-author='2022-Lopez\u2010Gamundi-et-al.' data-zp-date='2022' data-zp-year='2022' data-zp-itemtype='journalArticle' class=\"zp-Entry zpSearchResultsItem\">\n<div class=\"csl-bib-body\" style=\"line-height: 2; padding-left: 1em; text-indent:-1em;\">\n  <div class=\"csl-entry\">Lopez\u2010Gamundi, C., Dobbelaere, T., Hanert, E., Harris, P. M., Eberli, G., & Purkis, S. J. (2022). Simulating sedimentation on the Great Bahama Bank \u2013 Sources, sinks and storms. <i>Sedimentology<\/i>, <i>69<\/i>(7), 2693\u20132714. <a class='zp-DOIURL' href='https:\/\/doi.org\/10.1111\/sed.13020'>https:\/\/doi.org\/10.1111\/sed.13020<\/a><\/div>\n<\/div>\n\t\t\t\t<\/div><!-- .zp-Entry .zpSearchResultsItem -->\n\t\t\t<\/div><!-- .zp-zp-SEO-Content -->\n\t\t<\/div><!-- .zp-List -->\n\t<\/div><!--.zp-Zotpress-->\n\n\n","protected":false},"excerpt":{"rendered":"<p>The Great Bahama Bank (GBB) is one of the largest sites of shallow-water carbonate production on Earth. It is currently thought that between 50 and&hellip;<\/p>\n","protected":false},"author":13,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_bbp_topic_count":0,"_bbp_reply_count":0,"_bbp_total_topic_count":0,"_bbp_total_reply_count":0,"_bbp_voice_count":0,"_bbp_anonymous_reply_count":0,"_bbp_topic_count_hidden":0,"_bbp_reply_count_hidden":0,"_bbp_forum_subforum_count":0,"footnotes":""},"class_list":["post-4743","page","type-page","status-publish","hentry"],"jetpack_sharing_enabled":true,"_links":{"self":[{"href":"https:\/\/www.slim-ocean.be\/index.php\/wp-json\/wp\/v2\/pages\/4743","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.slim-ocean.be\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.slim-ocean.be\/index.php\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.slim-ocean.be\/index.php\/wp-json\/wp\/v2\/users\/13"}],"replies":[{"embeddable":true,"href":"https:\/\/www.slim-ocean.be\/index.php\/wp-json\/wp\/v2\/comments?post=4743"}],"version-history":[{"count":5,"href":"https:\/\/www.slim-ocean.be\/index.php\/wp-json\/wp\/v2\/pages\/4743\/revisions"}],"predecessor-version":[{"id":42623,"href":"https:\/\/www.slim-ocean.be\/index.php\/wp-json\/wp\/v2\/pages\/4743\/revisions\/42623"}],"wp:attachment":[{"href":"https:\/\/www.slim-ocean.be\/index.php\/wp-json\/wp\/v2\/media?parent=4743"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}