Changes
On August 4, 2023 at 9:32:40 AM UTC, admin:
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Moved Soil and sediment analyses of Lake La Thuile (Bauges, France) from organization PANGEA (Agriculture) to organization PANGAEA (Agriculture)
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Changed value of field
repository_name
toPANGAEA (Data Publisher for Earth & Environmental Science)
in Soil and sediment analyses of Lake La Thuile (Bauges, France)
f | 1 | { | f | 1 | { |
2 | "author": "Bajard Manon", | 2 | "author": "Bajard Manon", | ||
3 | "author_email": "", | 3 | "author_email": "", | ||
4 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | 4 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | ||
5 | "doi": "10.1594/PANGAEA.867313", | 5 | "doi": "10.1594/PANGAEA.867313", | ||
6 | "doi_date_published": "2016", | 6 | "doi_date_published": "2016", | ||
7 | "doi_publisher": "", | 7 | "doi_publisher": "", | ||
8 | "doi_status": "True", | 8 | "doi_status": "True", | ||
9 | "extra_authors": [ | 9 | "extra_authors": [ | ||
10 | { | 10 | { | ||
11 | "extra_author": "Poulenard J\u00e9r\u00f4me", | 11 | "extra_author": "Poulenard J\u00e9r\u00f4me", | ||
12 | "orcid": "0000-0003-0810-0308" | 12 | "orcid": "0000-0003-0810-0308" | ||
13 | }, | 13 | }, | ||
14 | { | 14 | { | ||
15 | "extra_author": "Sabatier Pierre", | 15 | "extra_author": "Sabatier Pierre", | ||
16 | "orcid": "0000-0002-9620-1514" | 16 | "orcid": "0000-0002-9620-1514" | ||
17 | }, | 17 | }, | ||
18 | { | 18 | { | ||
19 | "extra_author": "Develle Anne-Lise", | 19 | "extra_author": "Develle Anne-Lise", | ||
20 | "orcid": "0000-0003-2824-4106" | 20 | "orcid": "0000-0003-2824-4106" | ||
21 | }, | 21 | }, | ||
22 | { | 22 | { | ||
23 | "extra_author": "Jacob J\u00e9r\u00e9my", | 23 | "extra_author": "Jacob J\u00e9r\u00e9my", | ||
24 | "orcid": "0000-0002-3921-9566" | 24 | "orcid": "0000-0002-3921-9566" | ||
25 | }, | 25 | }, | ||
26 | { | 26 | { | ||
27 | "extra_author": "Giguet-Covex Charline", | 27 | "extra_author": "Giguet-Covex Charline", | ||
28 | "orcid": "0000-0002-5141-4815" | 28 | "orcid": "0000-0002-5141-4815" | ||
29 | }, | 29 | }, | ||
30 | { | 30 | { | ||
31 | "extra_author": "Crouzet Christian", | 31 | "extra_author": "Crouzet Christian", | ||
32 | "orcid": "0000-0002-4138-5213" | 32 | "orcid": "0000-0002-4138-5213" | ||
33 | }, | 33 | }, | ||
34 | { | 34 | { | ||
35 | "extra_author": "David Fernand", | 35 | "extra_author": "David Fernand", | ||
36 | "orcid": "" | 36 | "orcid": "" | ||
37 | }, | 37 | }, | ||
38 | { | 38 | { | ||
39 | "extra_author": "Pignol C\u00e9cile", | 39 | "extra_author": "Pignol C\u00e9cile", | ||
40 | "orcid": "" | 40 | "orcid": "" | ||
41 | }, | 41 | }, | ||
42 | { | 42 | { | ||
43 | "extra_author": "Arnaud Fabien", | 43 | "extra_author": "Arnaud Fabien", | ||
44 | "orcid": "0000-0002-8706-9902" | 44 | "orcid": "0000-0002-8706-9902" | ||
45 | } | 45 | } | ||
46 | ], | 46 | ], | ||
47 | "groups": [], | 47 | "groups": [], | ||
48 | "id": "426c6abb-123c-4852-828c-88f599ce02d9", | 48 | "id": "426c6abb-123c-4852-828c-88f599ce02d9", | ||
49 | "isopen": false, | 49 | "isopen": false, | ||
50 | "license_id": "CC-BY-3.0", | 50 | "license_id": "CC-BY-3.0", | ||
51 | "license_title": "CC-BY-3.0", | 51 | "license_title": "CC-BY-3.0", | ||
52 | "metadata_created": "2023-01-12T13:31:17.133341", | 52 | "metadata_created": "2023-01-12T13:31:17.133341", | ||
n | 53 | "metadata_modified": "2023-01-12T13:31:17.133347", | n | 53 | "metadata_modified": "2023-08-04T09:32:40.789590", |
54 | "name": "png-doi-10-1594-pangaea-867313", | 54 | "name": "png-doi-10-1594-pangaea-867313", | ||
55 | "notes": "Soils have a substantial role in the environment because | 55 | "notes": "Soils have a substantial role in the environment because | ||
56 | they provide several ecosystem services such as food supply or carbon | 56 | they provide several ecosystem services such as food supply or carbon | ||
57 | storage. Agricultural practices can modify soil properties and soil | 57 | storage. Agricultural practices can modify soil properties and soil | ||
58 | evolution processes, hence threatening these services. These | 58 | evolution processes, hence threatening these services. These | ||
59 | modifications are poorly studied, and the resilience/adaptation times | 59 | modifications are poorly studied, and the resilience/adaptation times | ||
60 | of soils to disruptions are unknown. Here, we study the evolution of | 60 | of soils to disruptions are unknown. Here, we study the evolution of | ||
61 | pedogenetic processes and soil evolution phases (progressive or | 61 | pedogenetic processes and soil evolution phases (progressive or | ||
62 | regressive) in response to human-induced erosion from a 4000-year lake | 62 | regressive) in response to human-induced erosion from a 4000-year lake | ||
63 | sediment sequence (Lake La Thuile, French Alps). Erosion in this small | 63 | sediment sequence (Lake La Thuile, French Alps). Erosion in this small | ||
64 | lake catchment in the montane area is quantified from the terrigenous | 64 | lake catchment in the montane area is quantified from the terrigenous | ||
65 | sediments that were trapped in the lake and compared to the soil | 65 | sediments that were trapped in the lake and compared to the soil | ||
66 | formation rate. To access this quantification, soil processes | 66 | formation rate. To access this quantification, soil processes | ||
67 | evolution are deciphered from soil and sediment geochemistry | 67 | evolution are deciphered from soil and sediment geochemistry | ||
68 | comparison. Over the last 4000 years, first impacts on soils are | 68 | comparison. Over the last 4000 years, first impacts on soils are | ||
69 | recorded at approximately 1600 yr cal. BP, with the erosion of surface | 69 | recorded at approximately 1600 yr cal. BP, with the erosion of surface | ||
70 | horizons exceeding 10 t/km**-2/yr. Increasingly deep horizons were | 70 | horizons exceeding 10 t/km**-2/yr. Increasingly deep horizons were | ||
71 | eroded with erosion accentuation during the Higher Middle Ages | 71 | eroded with erosion accentuation during the Higher Middle Ages | ||
72 | (1400-850 yr cal. BP), reaching 1000 t/km**-2/yr , and leading to the | 72 | (1400-850 yr cal. BP), reaching 1000 t/km**-2/yr , and leading to the | ||
73 | remobilization of carbonated and poorly weathered material, hence | 73 | remobilization of carbonated and poorly weathered material, hence | ||
74 | rejuvenating soil development. Erosion exceeded the soil formation | 74 | rejuvenating soil development. Erosion exceeded the soil formation | ||
75 | rate and constituted a regression in the development of soils. The | 75 | rate and constituted a regression in the development of soils. The | ||
76 | tolerable erosion limit is thus defined for erosion from 25 to 30 | 76 | tolerable erosion limit is thus defined for erosion from 25 to 30 | ||
77 | t/km**-2/yr. Beyond this limit, the sustainability of the | 77 | t/km**-2/yr. Beyond this limit, the sustainability of the | ||
78 | agroecosystem is limited and ecosystem services decrease. Afterwards, | 78 | agroecosystem is limited and ecosystem services decrease. Afterwards, | ||
79 | pedogenesis evolved again from progressive (700-300 yr cal. BP) to | 79 | pedogenesis evolved again from progressive (700-300 yr cal. BP) to | ||
80 | regressive (300 yr cal. BP-today) phases. Erosion was less important | 80 | regressive (300 yr cal. BP-today) phases. Erosion was less important | ||
81 | during the last 700 years than during the Middle Ages but with the | 81 | during the last 700 years than during the Middle Ages but with the | ||
82 | same weathering stages, indicating that soils were deeply affected | 82 | same weathering stages, indicating that soils were deeply affected | ||
83 | during the Middle-Age and have yet not recovered. Our results | 83 | during the Middle-Age and have yet not recovered. Our results | ||
84 | highlight the importance of the human factor in the pedogenesis over | 84 | highlight the importance of the human factor in the pedogenesis over | ||
85 | last millennia and suggest that the studied agro-ecosystem entered the | 85 | last millennia and suggest that the studied agro-ecosystem entered the | ||
86 | Anthropocene 1400 years ago.", | 86 | Anthropocene 1400 years ago.", | ||
87 | "num_resources": 0, | 87 | "num_resources": 0, | ||
88 | "num_tags": 0, | 88 | "num_tags": 0, | ||
89 | "orcid": "0000-0003-4622-0482", | 89 | "orcid": "0000-0003-4622-0482", | ||
90 | "organization": { | 90 | "organization": { | ||
91 | "approval_status": "approved", | 91 | "approval_status": "approved", | ||
n | 92 | "created": "2023-01-12T13:31:15.534211", | n | 92 | "created": "2023-08-04T09:32:38.098376", |
93 | "description": "PANGEA (Data Publisher for Earth & Environmental | 93 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
94 | Science): The information system PANGAEA is operated as an Open Access | 94 | Science): The information system PANGAEA is operated as an Open Access | ||
95 | library aimed at archiving, publishing and distributing georeferenced | 95 | library aimed at archiving, publishing and distributing georeferenced | ||
96 | data from earth system research. PANGAEA guarantees long-term | 96 | data from earth system research. PANGAEA guarantees long-term | ||
97 | availability (greater than 10 years) of its content. PANGAEA is open | 97 | availability (greater than 10 years) of its content. PANGAEA is open | ||
98 | to any project, institution, or individual scientist to use or to | 98 | to any project, institution, or individual scientist to use or to | ||
99 | archive and publish data. PANGAEA focuses on georeferenced | 99 | archive and publish data. PANGAEA focuses on georeferenced | ||
100 | observational data, experimental data, and models/simulations. | 100 | observational data, experimental data, and models/simulations. | ||
101 | Citability, comprehensive metadata descriptions, interoperability of | 101 | Citability, comprehensive metadata descriptions, interoperability of | ||
102 | data and metadata, a high degree of structural and semantic | 102 | data and metadata, a high degree of structural and semantic | ||
103 | harmonization of the data inventory as well as the commitment of the | 103 | harmonization of the data inventory as well as the commitment of the | ||
104 | hosting institutions ensures FAIRness of archived data.", | 104 | hosting institutions ensures FAIRness of archived data.", | ||
n | 105 | "id": "bde9e9b1-5746-46d6-809c-7515b699dbac", | n | 105 | "id": "93da141a-dc26-4ce9-bff3-b2b283505dcc", |
106 | "image_url": "pangea-logo.png", | 106 | "image_url": "pangea-logo.png", | ||
107 | "is_organization": true, | 107 | "is_organization": true, | ||
n | 108 | "name": "pangea", | n | 108 | "name": "pangaea", |
109 | "state": "active", | 109 | "state": "active", | ||
n | 110 | "title": "PANGEA (Agriculture)", | n | 110 | "title": "PANGAEA (Agriculture)", |
111 | "type": "organization" | 111 | "type": "organization" | ||
112 | }, | 112 | }, | ||
n | 113 | "owner_org": "bde9e9b1-5746-46d6-809c-7515b699dbac", | n | 113 | "owner_org": "93da141a-dc26-4ce9-bff3-b2b283505dcc", |
114 | "private": false, | 114 | "private": false, | ||
115 | "publication_year": "2016", | 115 | "publication_year": "2016", | ||
n | n | 116 | "related_identifiers": [ | ||
117 | { | ||||
118 | "authors": "Bajard Manon,Poulenard J\u00e9r\u00f4me,Sabatier | ||||
119 | Pierre,Develle Anne-Lise,Giguet-Covex Charline,Jacob | ||||
120 | J\u00e9r\u00e9my,Crouzet Christian,David Fernand,Pignol | ||||
121 | C\u00e9cile,Arnaud Fabien", | ||||
122 | "email_authors": | ||||
123 | niv-smb.fr,,,Fernand.David@LBHP.U-3mrs.fr,,fabien.arnaud@univ-smb.fr", | ||||
124 | "identifier": "https://doi.org/10.1016/j.catena.2016.11.001", | ||||
125 | "identifier_type": "DOI", | ||||
126 | "orcid_authors": | ||||
127 | 1-4815,0000-0002-3921-9566,0000-0002-4138-5213,,,0000-0002-8706-9902", | ||||
128 | "relation_type": "IsSupplementTo", | ||||
129 | "source": "CATENA", | ||||
130 | "title": "Progressive and regressive soil evolution phases in | ||||
131 | the Anthropocene", | ||||
132 | "year": "2017" | ||||
133 | } | ||||
134 | ], | ||||
116 | "relationships_as_object": [], | 135 | "relationships_as_object": [], | ||
117 | "relationships_as_subject": [], | 136 | "relationships_as_subject": [], | ||
n | 118 | "repository_name": "PANGEA (Data Publisher for Earth & Environmental | n | 137 | "repository_name": "PANGAEA (Data Publisher for Earth & |
119 | Science)", | 138 | Environmental Science)", | ||
120 | "resource_type": "application/zip - filename: Bajard_2016", | 139 | "resource_type": "application/zip - filename: Bajard_2016", | ||
121 | "resources": [], | 140 | "resources": [], | ||
t | t | 141 | "services_used_list": "", | ||
122 | "source_metadata_created": "2016", | 142 | "source_metadata_created": "2016", | ||
123 | "source_metadata_modified": "", | 143 | "source_metadata_modified": "", | ||
124 | "state": "active", | 144 | "state": "active", | ||
125 | "subject_areas": [ | 145 | "subject_areas": [ | ||
126 | { | 146 | { | ||
127 | "subject_area_additional": "", | 147 | "subject_area_additional": "", | ||
128 | "subject_area_name": "Agriculture" | 148 | "subject_area_name": "Agriculture" | ||
129 | }, | 149 | }, | ||
130 | { | 150 | { | ||
131 | "subject_area_additional": "", | 151 | "subject_area_additional": "", | ||
132 | "subject_area_name": "LakesRivers" | 152 | "subject_area_name": "LakesRivers" | ||
133 | }, | 153 | }, | ||
134 | { | 154 | { | ||
135 | "subject_area_additional": "", | 155 | "subject_area_additional": "", | ||
136 | "subject_area_name": "Lithosphere" | 156 | "subject_area_name": "Lithosphere" | ||
137 | } | 157 | } | ||
138 | ], | 158 | ], | ||
139 | "tags": [], | 159 | "tags": [], | ||
140 | "title": "Soil and sediment analyses of Lake La Thuile (Bauges, | 160 | "title": "Soil and sediment analyses of Lake La Thuile (Bauges, | ||
141 | France)", | 161 | France)", | ||
142 | "type": "vdataset", | 162 | "type": "vdataset", | ||
143 | "url": "https://doi.org/10.1594/PANGAEA.867313" | 163 | "url": "https://doi.org/10.1594/PANGAEA.867313" | ||
144 | } | 164 | } |