Changes
On October 22, 2024, 5:12:22 PM UTC,
-
Added resource Supplementary material 1.pdf to Nitrogen cycling dynamics under altering redox conditions during sapropels S1 and the ambiguous S2 in the Eastern Mediterranean Sea
| f | 1 | { | f | 1 | { |
| 2 | "author": null, | 2 | "author": null, | ||
| 3 | "author_email": null, | 3 | "author_email": null, | ||
| 4 | "code": "7b.b.fd", | 4 | "code": "7b.b.fd", | ||
| 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | ||
| 6 | "creator_user_id": "63e7592d-9651-4127-b7e7-e2d4a62f88a5", | 6 | "creator_user_id": "63e7592d-9651-4127-b7e7-e2d4a62f88a5", | ||
| 7 | "creators": "[{\"firstname\":\"Zo\u00eb\",\"lastname\":\"van | 7 | "creators": "[{\"firstname\":\"Zo\u00eb\",\"lastname\":\"van | ||
| 8 | Kemenade\",\"orcid\":null,\"affiliation\":\"Royal Netherlands | 8 | Kemenade\",\"orcid\":null,\"affiliation\":\"Royal Netherlands | ||
| 9 | Institute for Sea | 9 | Institute for Sea | ||
| 10 | ctemailaddress\":\"zoe.van.kemenade@nioz.nl\",\"formatted\":\"Zo\u00eb | 10 | ctemailaddress\":\"zoe.van.kemenade@nioz.nl\",\"formatted\":\"Zo\u00eb | ||
| 11 | van Kemenade - Royal Netherlands Institute for Sea Research - ORCID: | 11 | van Kemenade - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 12 | - Corresponding Author - | 12 | - Corresponding Author - | ||
| 13 | Anna\",\"lastname\":\"Cutmore\",\"orcid\":null,\"affiliation\":\"Royal | 13 | Anna\",\"lastname\":\"Cutmore\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 14 | Netherlands Institute for Sea | 14 | Netherlands Institute for Sea | ||
| 15 | pondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Anna | 15 | pondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Anna | ||
| 16 | Cutmore - Royal Netherlands Institute for Sea Research - ORCID: | 16 | Cutmore - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 17 | ick\",\"lastname\":\"Hennekam\",\"orcid\":null,\"affiliation\":\"Royal | 17 | ick\",\"lastname\":\"Hennekam\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 18 | Netherlands Institute for Sea | 18 | Netherlands Institute for Sea | ||
| 19 | pondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Rick | 19 | pondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Rick | ||
| 20 | Hennekam - Royal Netherlands Institute for Sea Research - ORCID: | 20 | Hennekam - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 21 | llen\",\"lastname\":\"Hopmans\",\"orcid\":null,\"affiliation\":\"Royal | 21 | llen\",\"lastname\":\"Hopmans\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 22 | Netherlands Institute for Sea | 22 | Netherlands Institute for Sea | ||
| 23 | ondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Ellen | 23 | ondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Ellen | ||
| 24 | Hopmans - Royal Netherlands Institute for Sea Research - ORCID: | 24 | Hopmans - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 25 | \"},{\"firstname\":\"Marcel\",\"lastname\":\"van der | 25 | \"},{\"firstname\":\"Marcel\",\"lastname\":\"van der | ||
| 26 | Meer\",\"orcid\":null,\"affiliation\":\"Royal Netherlands Institute | 26 | Meer\",\"orcid\":null,\"affiliation\":\"Royal Netherlands Institute | ||
| 27 | for Sea | 27 | for Sea | ||
| 28 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Marcel | 28 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Marcel | ||
| 29 | van der Meer - Royal Netherlands Institute for Sea Research - ORCID: | 29 | van der Meer - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 30 | \"lastname\":\"Moijtahid\",\"orcid\":null,\"affiliation\":\"University | 30 | \"lastname\":\"Moijtahid\",\"orcid\":null,\"affiliation\":\"University | ||
| 31 | of | 31 | of | ||
| 32 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Meryem | 32 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Meryem | ||
| 33 | Moijtahid - University of Angers - ORCID: | 33 | Moijtahid - University of Angers - ORCID: | ||
| 34 | ,\"lastname\":\"Jorissen\",\"orcid\":null,\"affiliation\":\"University | 34 | ,\"lastname\":\"Jorissen\",\"orcid\":null,\"affiliation\":\"University | ||
| 35 | of | 35 | of | ||
| 36 | ondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Frans | 36 | ondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Frans | ||
| 37 | Jorissen - University of Angers - ORCID: | 37 | Jorissen - University of Angers - ORCID: | ||
| 38 | "Nicole\",\"lastname\":\"Bale\",\"orcid\":null,\"affiliation\":\"Royal | 38 | "Nicole\",\"lastname\":\"Bale\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 39 | Netherlands Institute for Sea | 39 | Netherlands Institute for Sea | ||
| 40 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Nicole | 40 | ndingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Nicole | ||
| 41 | Bale - Royal Netherlands Institute for Sea Research - ORCID: | 41 | Bale - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 42 | Jan\",\"lastname\":\"Reichart\",\"orcid\":null,\"affiliation\":\"Royal | 42 | Jan\",\"lastname\":\"Reichart\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 43 | Netherlands Institute for Sea | 43 | Netherlands Institute for Sea | ||
| 44 | ingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Gert-Jan | 44 | ingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Gert-Jan | ||
| 45 | Reichart - Royal Netherlands Institute for Sea Research - ORCID: | 45 | Reichart - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 46 | \"},{\"firstname\":\"Jaap\",\"lastname\":\"Sinninghe | 46 | \"},{\"firstname\":\"Jaap\",\"lastname\":\"Sinninghe | ||
| 47 | Damst\u00e9\",\"orcid\":null,\"affiliation\":\"Royal Netherlands | 47 | Damst\u00e9\",\"orcid\":null,\"affiliation\":\"Royal Netherlands | ||
| 48 | Institute for Sea | 48 | Institute for Sea | ||
| 49 | pondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Jaap | 49 | pondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Jaap | ||
| 50 | Sinninghe Damst\u00e9 - Royal Netherlands Institute for Sea Research - | 50 | Sinninghe Damst\u00e9 - Royal Netherlands Institute for Sea Research - | ||
| 51 | ORCID: | 51 | ORCID: | ||
| 52 | \"Darci\",\"lastname\":\"Rush\",\"orcid\":null,\"affiliation\":\"Royal | 52 | \"Darci\",\"lastname\":\"Rush\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 53 | Netherlands Institute for Sea | 53 | Netherlands Institute for Sea | ||
| 54 | arch\",\"iscorrespondingauthor\":null,\"contactemailaddress\":null}]", | 54 | arch\",\"iscorrespondingauthor\":null,\"contactemailaddress\":null}]", | ||
| 55 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.fd", | 55 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.fd", | ||
| 56 | "deposit_date": "2022-09-14", | 56 | "deposit_date": "2022-09-14", | ||
| 57 | "depositor": "Zoe van Kemenade", | 57 | "depositor": "Zoe van Kemenade", | ||
| 58 | "distribution_date": "2022-09-14", | 58 | "distribution_date": "2022-09-14", | ||
| 59 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 59 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 60 | Institute for Sea Research)", | 60 | Institute for Sea Research)", | ||
| 61 | "doi_date_published": "2023-03-15", | 61 | "doi_date_published": "2023-03-15", | ||
| 62 | "funding_references": "[{\"name\":\"Soehngen Institute of Anaerobic | 62 | "funding_references": "[{\"name\":\"Soehngen Institute of Anaerobic | ||
| 63 | Microbiology | 63 | Microbiology | ||
| 64 | \",\"awardnumber\":\"024.002.002\",\"awardtitle\":\"Gravitation | 64 | \",\"awardnumber\":\"024.002.002\",\"awardtitle\":\"Gravitation | ||
| 65 | Grant\"}]", | 65 | Grant\"}]", | ||
| 66 | "groups": [], | 66 | "groups": [], | ||
| 67 | "id": "1afab812-5d8f-445e-85d0-002ab17ba28e", | 67 | "id": "1afab812-5d8f-445e-85d0-002ab17ba28e", | ||
| 68 | "isopen": false, | 68 | "isopen": false, | ||
| 69 | "license_title": null, | 69 | "license_title": null, | ||
| 70 | "maintainer": null, | 70 | "maintainer": null, | ||
| 71 | "maintainer_email": null, | 71 | "maintainer_email": null, | ||
| 72 | "metadata_created": "2024-10-22T11:47:11.843489", | 72 | "metadata_created": "2024-10-22T11:47:11.843489", | ||
| n | 73 | "metadata_modified": "2024-10-22T17:12:21.113698", | n | 73 | "metadata_modified": "2024-10-22T17:12:22.283710", |
| 74 | "name": "7bbfd", | 74 | "name": "7bbfd", | ||
| 75 | "notes": "In the eastern Mediterranean Sea (EMS), the organic-poor | 75 | "notes": "In the eastern Mediterranean Sea (EMS), the organic-poor | ||
| 76 | sedimentary record is periodically interspersed with organic-rich | 76 | sedimentary record is periodically interspersed with organic-rich | ||
| 77 | layers, known as sapropels. Sapropels are characteristic of basin-wide | 77 | layers, known as sapropels. Sapropels are characteristic of basin-wide | ||
| 78 | anoxic events, triggered by precession-forced insolation maxima. In | 78 | anoxic events, triggered by precession-forced insolation maxima. In | ||
| 79 | the late Quaternary, relatively subdued insolation maxima are not | 79 | the late Quaternary, relatively subdued insolation maxima are not | ||
| 80 | always expressed as distinct sapropels. Late Quaternary EMS | 80 | always expressed as distinct sapropels. Late Quaternary EMS | ||
| 81 | sedimentary records hereby offer the opportunity to investigate | 81 | sedimentary records hereby offer the opportunity to investigate | ||
| 82 | tipping points of anoxia and associated nitrogen (N) cycling dynamics. | 82 | tipping points of anoxia and associated nitrogen (N) cycling dynamics. | ||
| 83 | To this extent, we have investigated a ~68 kyr sediment record from | 83 | To this extent, we have investigated a ~68 kyr sediment record from | ||
| 84 | the EMS (64PE406-E1), which contains the well-established Holocene | 84 | the EMS (64PE406-E1), which contains the well-established Holocene | ||
| 85 | sapropel S1 (deposited in two parts: S1a [~10.5\u25008.5 kyr BP] and | 85 | sapropel S1 (deposited in two parts: S1a [~10.5\u25008.5 kyr BP] and | ||
| 86 | S1b [~7.8\u25006.1 kyr BP]) and the sediments timed to the ambiguous | 86 | S1b [~7.8\u25006.1 kyr BP]) and the sediments timed to the ambiguous | ||
| 87 | S2 sapropel of the late Pleistocene (~53 kyr BP). We focus on lipid | 87 | S2 sapropel of the late Pleistocene (~53 kyr BP). We focus on lipid | ||
| 88 | biomarkers of microorganisms to reconstruct changes in key components | 88 | biomarkers of microorganisms to reconstruct changes in key components | ||
| 89 | of the N cycle: (1) anaerobic ammonium oxidation (anammox) using | 89 | of the N cycle: (1) anaerobic ammonium oxidation (anammox) using | ||
| 90 | ladderanes and a stereoisomer of bacteriohopanetetrol (BHT-x), (2) | 90 | ladderanes and a stereoisomer of bacteriohopanetetrol (BHT-x), (2) | ||
| 91 | dinitrogen gas (N2) fixation using heterocyte glycolipids (HGs), and | 91 | dinitrogen gas (N2) fixation using heterocyte glycolipids (HGs), and | ||
| 92 | (3) nitrification by Thaumarchaeota using crenarchaeol. Elevated | 92 | (3) nitrification by Thaumarchaeota using crenarchaeol. Elevated | ||
| 93 | crenarchaeol at the start of S1a indicates enhanced nitrification by | 93 | crenarchaeol at the start of S1a indicates enhanced nitrification by | ||
| 94 | Thaumarchaeota, likely promoted by an influx of nutrients via enhanced | 94 | Thaumarchaeota, likely promoted by an influx of nutrients via enhanced | ||
| 95 | river discharge. Anammox occurred throughout S1, but was most intense | 95 | river discharge. Anammox occurred throughout S1, but was most intense | ||
| 96 | ~1.5 kyr after the onset of anoxia (at ~10.5 cal. kyr BP; as | 96 | ~1.5 kyr after the onset of anoxia (at ~10.5 cal. kyr BP; as | ||
| 97 | indicated by redox-sensitive trace elements and benthic foraminifer | 97 | indicated by redox-sensitive trace elements and benthic foraminifer | ||
| 98 | assemblages). High organic carbon levels in S1a likely resulted in | 98 | assemblages). High organic carbon levels in S1a likely resulted in | ||
| 99 | anammox being initially outcompeted by heterotrophic denitrification. | 99 | anammox being initially outcompeted by heterotrophic denitrification. | ||
| 100 | N2-fixation by heterocytous cyanobacteria appeared predominantly at | 100 | N2-fixation by heterocytous cyanobacteria appeared predominantly at | ||
| 101 | the S1a termination and in the S1 interruption. Ladderanes suggest | 101 | the S1a termination and in the S1 interruption. Ladderanes suggest | ||
| 102 | additional episodes of bioavailable N removal between ~69 to 39 cal. | 102 | additional episodes of bioavailable N removal between ~69 to 39 cal. | ||
| 103 | kyr BP. These episodes correspond to brief periods of anoxia at the | 103 | kyr BP. These episodes correspond to brief periods of anoxia at the | ||
| 104 | sediment-water interface, with maximum deoxygenation occurring in | 104 | sediment-water interface, with maximum deoxygenation occurring in | ||
| 105 | sediments timed to S2 (53\u250053 cal. kyr BP; as indicated by Mn/Al | 105 | sediments timed to S2 (53\u250053 cal. kyr BP; as indicated by Mn/Al | ||
| 106 | and benthic foraminifera). During these episodes, BHT-x is absent, | 106 | and benthic foraminifera). During these episodes, BHT-x is absent, | ||
| 107 | but, ladderanes co-occur with a later eluting BHT stereoisomer | 107 | but, ladderanes co-occur with a later eluting BHT stereoisomer | ||
| 108 | (BHT-34R). BHT-34R compound-specific \u03b413C values indicate an | 108 | (BHT-34R). BHT-34R compound-specific \u03b413C values indicate an | ||
| 109 | anammox source, potentially synthesized by relatively poorly studied | 109 | anammox source, potentially synthesized by relatively poorly studied | ||
| 110 | marine sedimentary anammox bacteria. Taken all together, our results | 110 | marine sedimentary anammox bacteria. Taken all together, our results | ||
| 111 | highlight various modes of operation of the N cycle during the | 111 | highlight various modes of operation of the N cycle during the | ||
| 112 | different deoxygenation events. During S1a, a combination of anammox, | 112 | different deoxygenation events. During S1a, a combination of anammox, | ||
| 113 | denitrification and an excess supply of P may have been a reinforcing | 113 | denitrification and an excess supply of P may have been a reinforcing | ||
| 114 | feedback for anoxia, by favoring the appearance of diatom-diazotroph | 114 | feedback for anoxia, by favoring the appearance of diatom-diazotroph | ||
| 115 | symbiotic consortia. While during S1b and S2, a temporal coupling | 115 | symbiotic consortia. While during S1b and S2, a temporal coupling | ||
| 116 | between anammox and N2-fixation was not observed, either because loss | 116 | between anammox and N2-fixation was not observed, either because loss | ||
| 117 | of bioavailable N was not sufficiently extensive or diazotrophs were | 117 | of bioavailable N was not sufficiently extensive or diazotrophs were | ||
| 118 | nutrient limited. During these periods, anammox may have acted as a | 118 | nutrient limited. During these periods, anammox may have acted as a | ||
| 119 | negative feedback on anoxia by quenching primary production.", | 119 | negative feedback on anoxia by quenching primary production.", | ||
| n | 120 | "num_resources": 1, | n | 120 | "num_resources": 2, |
| 121 | "num_tags": 1, | 121 | "num_tags": 1, | ||
| 122 | "organization": { | 122 | "organization": { | ||
| 123 | "approval_status": "approved", | 123 | "approval_status": "approved", | ||
| 124 | "created": "2024-10-22T06:06:56.074257", | 124 | "created": "2024-10-22T06:06:56.074257", | ||
| 125 | "description": "", | 125 | "description": "", | ||
| 126 | "id": "bed2a893-3895-450b-bf4b-c74318003b1b", | 126 | "id": "bed2a893-3895-450b-bf4b-c74318003b1b", | ||
| 127 | "image_url": | 127 | "image_url": | ||
| 128 | z.nl/application/files/1216/8924/5333/NIOZ-logo_witte_randi-2023.svg", | 128 | z.nl/application/files/1216/8924/5333/NIOZ-logo_witte_randi-2023.svg", | ||
| 129 | "is_organization": true, | 129 | "is_organization": true, | ||
| 130 | "name": "nioz", | 130 | "name": "nioz", | ||
| 131 | "state": "active", | 131 | "state": "active", | ||
| 132 | "title": "Royal Netherlands Institute for Sea Research", | 132 | "title": "Royal Netherlands Institute for Sea Research", | ||
| 133 | "type": "organization" | 133 | "type": "organization" | ||
| 134 | }, | 134 | }, | ||
| 135 | "owner_org": "bed2a893-3895-450b-bf4b-c74318003b1b", | 135 | "owner_org": "bed2a893-3895-450b-bf4b-c74318003b1b", | ||
| 136 | "private": false, | 136 | "private": false, | ||
| 137 | "production_date": "2023-03-15", | 137 | "production_date": "2023-03-15", | ||
| 138 | "relationships_as_object": [], | 138 | "relationships_as_object": [], | ||
| 139 | "relationships_as_subject": [], | 139 | "relationships_as_subject": [], | ||
| 140 | "resources": [ | 140 | "resources": [ | ||
| 141 | { | 141 | { | ||
| 142 | "cache_last_updated": null, | 142 | "cache_last_updated": null, | ||
| 143 | "cache_url": null, | 143 | "cache_url": null, | ||
| 144 | "created": "2024-10-22T11:47:12.424822", | 144 | "created": "2024-10-22T11:47:12.424822", | ||
| 145 | "datastore_active": false, | 145 | "datastore_active": false, | ||
| 146 | "format": "XLSX", | 146 | "format": "XLSX", | ||
| 147 | "hash": "ad2bca96f3aedcf4715dff990892b59a", | 147 | "hash": "ad2bca96f3aedcf4715dff990892b59a", | ||
| 148 | "id": "c380ccc0-6198-4158-94f3-ffc9afbf1a79", | 148 | "id": "c380ccc0-6198-4158-94f3-ffc9afbf1a79", | ||
| 149 | "last_modified": "2024-10-22T11:47:12.405670", | 149 | "last_modified": "2024-10-22T11:47:12.405670", | ||
| 150 | "metadata_modified": "2024-10-22T11:47:12.862899", | 150 | "metadata_modified": "2024-10-22T11:47:12.862899", | ||
| 151 | "mimetype": | 151 | "mimetype": | ||
| 152 | "application/vnd.openxmlformats-officedocument.spreadsheetml.sheet", | 152 | "application/vnd.openxmlformats-officedocument.spreadsheetml.sheet", | ||
| 153 | "mimetype_inner": null, | 153 | "mimetype_inner": null, | ||
| 154 | "name": "Supplementary Material 2.xlsx", | 154 | "name": "Supplementary Material 2.xlsx", | ||
| 155 | "package_id": "1afab812-5d8f-445e-85d0-002ab17ba28e", | 155 | "package_id": "1afab812-5d8f-445e-85d0-002ab17ba28e", | ||
| 156 | "position": 0, | 156 | "position": 0, | ||
| 157 | "resource_type": null, | 157 | "resource_type": null, | ||
| 158 | "size": 35435, | 158 | "size": 35435, | ||
| 159 | "state": "active", | 159 | "state": "active", | ||
| 160 | "url": | 160 | "url": | ||
| 161 | 0-6198-4158-94f3-ffc9afbf1a79/download/supplementary-material-2.xlsx", | 161 | 0-6198-4158-94f3-ffc9afbf1a79/download/supplementary-material-2.xlsx", | ||
| 162 | "url_type": "upload" | 162 | "url_type": "upload" | ||
| t | t | 163 | }, | ||
| 164 | { | ||||
| 165 | "cache_last_updated": null, | ||||
| 166 | "cache_url": null, | ||||
| 167 | "created": "2024-10-22T17:12:22.295256", | ||||
| 168 | "datastore_active": false, | ||||
| 169 | "format": "PDF", | ||||
| 170 | "hash": "dcff0e97aaf41eeb4d1864c3bd39ca66", | ||||
| 171 | "id": "8e1d8249-9917-4d2d-ab3c-d639d206630d", | ||||
| 172 | "last_modified": "2024-10-22T17:12:22.274482", | ||||
| 173 | "metadata_modified": "2024-10-22T17:12:22.290240", | ||||
| 174 | "mimetype": "application/pdf", | ||||
| 175 | "mimetype_inner": null, | ||||
| 176 | "name": "Supplementary material 1.pdf", | ||||
| 177 | "package_id": "1afab812-5d8f-445e-85d0-002ab17ba28e", | ||||
| 178 | "position": 1, | ||||
| 179 | "resource_type": null, | ||||
| 180 | "size": 1933044, | ||||
| 181 | "state": "active", | ||||
| 182 | "url": | ||||
| 183 | 49-9917-4d2d-ab3c-d639d206630d/download/supplementary-material-1.pdf", | ||||
| 184 | "url_type": "upload" | ||||
| 163 | } | 185 | } | ||
| 164 | ], | 186 | ], | ||
| 165 | "state": "active", | 187 | "state": "active", | ||
| 166 | "subject": "Earth and Environmental Sciences", | 188 | "subject": "Earth and Environmental Sciences", | ||
| 167 | "tags": [ | 189 | "tags": [ | ||
| 168 | { | 190 | { | ||
| 169 | "display_name": "Marine nitrogen cycle Sapropel Eastern | 191 | "display_name": "Marine nitrogen cycle Sapropel Eastern | ||
| 170 | Mediterranean Sea Lipid biomarkers Anoxic events", | 192 | Mediterranean Sea Lipid biomarkers Anoxic events", | ||
| 171 | "id": "51ff3a04-a5f0-4927-9a9c-5f77aafcfe0a", | 193 | "id": "51ff3a04-a5f0-4927-9a9c-5f77aafcfe0a", | ||
| 172 | "name": "Marine nitrogen cycle Sapropel Eastern Mediterranean | 194 | "name": "Marine nitrogen cycle Sapropel Eastern Mediterranean | ||
| 173 | Sea Lipid biomarkers Anoxic events", | 195 | Sea Lipid biomarkers Anoxic events", | ||
| 174 | "state": "active", | 196 | "state": "active", | ||
| 175 | "vocabulary_id": null | 197 | "vocabulary_id": null | ||
| 176 | } | 198 | } | ||
| 177 | ], | 199 | ], | ||
| 178 | "title": "Nitrogen cycling dynamics under altering redox conditions | 200 | "title": "Nitrogen cycling dynamics under altering redox conditions | ||
| 179 | during sapropels S1 and the ambiguous S2 in the Eastern Mediterranean | 201 | during sapropels S1 and the ambiguous S2 in the Eastern Mediterranean | ||
| 180 | Sea", | 202 | Sea", | ||
| 181 | "type": "dataset", | 203 | "type": "dataset", | ||
| 182 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.fd", | 204 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.fd", | ||
| 183 | "version": "1" | 205 | "version": "1" | ||
| 184 | } | 206 | } |