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dc.contributor.author신경훈-
dc.date.accessioned2020-01-28T04:19:33Z-
dc.date.available2020-01-28T04:19:33Z-
dc.date.issued2019-12-
dc.identifier.citationJOURNAL OF SOUTH AMERICAN EARTH SCIENCES, v. 96, Article no. 102349en_US
dc.identifier.issn0895-9811-
dc.identifier.urihttps://www.sciencedirect.com/science/article/pii/S0895981119303402-
dc.identifier.urihttps://repository.hanyang.ac.kr/handle/20.500.11754/122267-
dc.description.abstractIn this study, we evaluate sources of organic matter (OM) in two contrasting tropical coastal environments in Colombia, using a combination of glycerol dialkyl glycerol tetraethers (GDGTs) and n-alkane lipid biomarkers. A clear difference between the less productive Caribbean Sea and the more productive eastern Pacific is observed, with higher terrestrial contributions into the eastern Pacific strongly associated with riverine inputs. Although higher land plant-derived n-alkanes can be transported as eolian dust, our results suggest mainly riverine sources for our samples. When looking at the branched GDGT compositions, in situ production could be identified in most Caribbean stations and some of the more coastal sites in the Pacific with #rings(te)(tra) index values of above 0.7. The remaining stations in the eastern Pacific display soil-eroded GDGTs inputs associated with river discharges and deposited in the proximity of the coast. Marine production as measured by short chain n-alkanes and crenarchaeol are also higher in the eastern Pacific. It appears that the terrestrial inputs would bring nutrients as well as OM fueling both auto- and heterotrophs making the eastern Pacific overall more productive. We also observe OM of petrogenic origin, albeit in a low amount, especially in coastal Caribbean sites located near main harbors. This study helps improve the understanding of the complex mixture of OM inputs, origins and transport mechanisms into Colombian coastal areas. The present work emphasizes the need to integrate climate, geological setting and hydrology to fully understand the carbon cycle at a regional scale.en_US
dc.description.sponsorshipThis work was partially funded by FAPA project "Biomarcadores lipidicos para reconstrucciones paleoclimaticas" [R.3.2015.2423; Los Andes University] to CH. This work was also supported by the National Research Foundation of Korea (NRF) grant funded by the Ministry of Science and ICT [MSIT, No. NRF-2016R1A2B3015388, KOPRI-PN19100] to J-H. K. This project was conceived by CG and CH as part of the project "Distribucidn de palinomorfos marinos y terrestres en sedimentos marinos superficiales del Mar Caribe y el Pacifico tropical oriental en relacion con parametros ambientales" funded by COLCIENCIAS [project 1204-569-34184]. We are grateful to Centro de Innovacidn y Tecnologia from the Institute Colombiano de Petroleo (ICP), Laboratorio Biologia Marina Uniandes (BIOMAR), Lamont Doherty Earth Observatory (LDEO), Ocean Drilling Program (ODP, OIDP), and EAFIT University for providing samples.en_US
dc.language.isoen_USen_US
dc.publisherPERGAMON-ELSEVIER SCIENCE LTDen_US
dc.subjectGlycerol dialkyl glycerol tetraethers (GDGTs)en_US
dc.subjectn-alkanesen_US
dc.subjectTerrestrial inputen_US
dc.subjectCaribbeanen_US
dc.subjectEastern tropical pacificen_US
dc.titleSources of organic matter in two contrasting tropical coastal environments: The Caribbean Sea and the eastern Pacificen_US
dc.typeArticleen_US
dc.relation.no102349-
dc.relation.volume96-
dc.identifier.doi10.1016/j.jsames.2019.102349-
dc.relation.page1-10-
dc.relation.journalJOURNAL OF SOUTH AMERICAN EARTH SCIENCES-
dc.contributor.googleauthorHuguet, C.-
dc.contributor.googleauthorKim, J.-H.-
dc.contributor.googleauthorGonzález-Arango, C.-
dc.contributor.googleauthorRamírez-Valencia, V.-
dc.contributor.googleauthorKang, S.-
dc.contributor.googleauthorGal, J.-K.-
dc.contributor.googleauthorShin, K.-H.-
dc.relation.code2019000253-
dc.sector.campusE-
dc.sector.daehakCOLLEGE OF SCIENCE AND CONVERGENCE TECHNOLOGY[E]-
dc.sector.departmentDEPARTMENT OF MARINE SCIENCE AND CONVERGENCE ENGINEERING-
dc.identifier.pidshinkh-


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