https://fossilsketch.org/_next/static/chunks/pages/games/ostracod_assemblage-63e1729f42427661.js

1(self.webpackChunk_N_E=self.webpackChunk_N_E||[]).push([[8478],{5911:function(e,a,r){(window.__NEXT_P=window.__NEXT_P||[]).push(["/games/ostracod_assemblage",function(){return r(5129)}])},5129:function(e,a,r){"use strict";r.r(a);var n=r(2322),s=r(2784),t=r(356),i=r.n(t),o=r(1783),l=r(8621),c=r(7577),h=r(7841),d=r(5632),m=r(7973),u=[[{Name:"sample1.jpg",Limnocythere:9,"Cythere lutea":6,Leptocythere:5,"Roundstonia globulifera":0,"Cytheropteron montrosiense":0,Elofsonella:0}],[{Name:"sample2.jpg",Leptocythere:6,"Sarsicytheridea punctillata":6,"Sarsicytheridea bradii":6,Heterocyprideis:3,"Roundstonia globulifera":0,Elofsonella:4}],[{Name:"sample3.jpg","Cythere lutea":0,"Sarsicytheridea punctillata":0,"Sarsicytheridea bradii":0,"Roundstonia globulifera":6,"Cytheropteron montrosiense":6,Elofsonella:2,Acanthocythereis:3}]],p=[{instructions:["Having identified species type and count, use the drop-down menus below to select the environment for each sample."],header:["Sample 1","Sample 2","Sample 3"],rowValues:[{"Sample 1":"Limnocythere: 9 (freshwater)","Sample 2":"Leptocythere: 6 (brackish water)","Sample 3":"Roundstonia: 6 (marine)"},{"Sample 1":"Cythere: 6 (brackish water)","Sample 2":"Sarsicytheridea p.: 6 (brackish to marine)","Sample 3":"Cytheropteron: 6 (marine)"},{"Sample 1":"Leptocythere: 5 (brackish water)","Sample 2":"Sarsicytheridea br.: 6 (brackish to marine)","Sample 3":"Elofsonella: 2 (marine)"},{"Sample 1":"","Sample 2":"Heterocyprideis: 3 (brackish to marine)","Sample 3":"Acanthocythereis: 3 (marine)"},{"Sample 1":"","Sample 2":"Elofsonella: 4 (marine)","Sample 3":""}],sampleOptions:[["Freshwater","Brackishwater","Marine"]],placeholderOption:["Environment?"]}],g=[["Brackishwater","Brackishwater","Marine"]];function f(e){var a=new Array(e.length).fill(!1).map((function(){return new Array(e[0].length).fill(!1)}));return"Brackishwater"!==e[0][0]&&"Freshwater"!==e[0][0]&&(a[0][0]=!0),"Brackishwater"!==e[0][1]&&(a[0][1]=!0),"Marine"!==e[0][2]&&(a[0][2]=!0),a}var y={sections:[],overallRatingQuestionId:"none",commentQuestionId:"none"};a.default=function(e){var a=e.handleLogout,r=(0,s.useState)(!0),t=r[0],b=r[1],w=(0,d.useRouter)(),v=(0,s.useContext)(m.Z),S=(0,s.useState)(!1),k=S[0],_=S[1];return(0,s.useEffect)((function(){if(w.isReady)if("1"===w.query.skipEnd||Array.isArray(w.query.skipEnd)&&w.query.skipEnd.includes("1")){var e=(v.userEmail||localStorage.getItem("userEmail")||"").toLowerCase();_("[email protected]"===e)}else _(!1)}),[w.isReady,w.query.skipEnd,v.userEmail]),(0,n.jsxs)("div",{className:i().background,children:[(0,n.jsx)(o.Z,{handleLogout:a}),(0,n.jsx)(l.Z,{assemblagePool:u,initialRoundImgs:"sample",assemblageFolder:"ostracodaAssemblageGame",imageFolder:"ostracoda",gameName:"ostracod_assemblage",endQuestions:p,checkAnswer:f,endQuestion:!0,multiLevel:!1,answerRange:0,answers:g,surveyConfig:y,forceOpenEndModal:k}),t&&(0,n.jsx)(c.a,{opacity:1,color:"rgba(0, 0, 0, 1)",zIndex:5,style:{overflow:"hidden"},children:(0,n.jsxs)("div",{className:i().overlay_intro_container,children:[(0,n.jsx)("div",{className:i().overlay_intro_title,children:"Backgroun

1d"}),(0,n.jsxs)("div",{className:i().overlay_intro_middle,children:[(0,n.jsx)("img",{className:i().overlay_intro_img,src:"/overlays/maps.png"}),(0,n.jsx)("div",{className:i().overlay_intro_text,children:(0,n.jsxs)("p",{children:["The Baltic Sea region has experienced several climate-driven hydrological changes during the Holocene. Its history is highly dynamic and governed by the regional isostatic rebound (the rise of land masses that were depressed by the huge weight of ice sheets during the last ice age) and global sea level changes, allowing more or less saline water to enter the basin through more or less broad and deep straits, resulting in alternating freshwater and brackish phases and complex shoreline development.",(0,n.jsx)("br",{}),(0,n.jsx)("br",{}),"High-resolution studies of salinity and temperature changes in the past contribute to a better understanding of how environmental parameters change in continental shelf seas and enclosed basins. These data improve our understanding of the impact and magnitude of future environmental changes in the Baltic Sea region.",(0,n.jsx)("br",{}),(0,n.jsx)("br",{}),"We can look at changes in the abundance of microfossils, such as ostracods (crustaceans) that prefer different range of water salinity. When species that prefer freshwater environments make up all or the majority of individuals in the assemblage, we infer that the environment was freshwater. The same is true for brackish-water or marine ecologic groups."]})})]}),(0,n.jsx)(h.z,{radius:"xl",size:"lg",onClick:function(){return b(!1)},children:"Begin"})]})})]})}}},function(e){e.O(0,[6577,443,7301,1858,6943,6870,8621,9774,2888,179],(function(){return a=5911,e(e.s=a);var a}));var a=e.O();_N_E=a}]);