Bibliografie tematiche / Bassin du Changjiang (Yangtze)

Letteratura scientifica selezionata sul tema "Bassin du Changjiang (Yangtze)"

Autore: Grafiati
Pubblicato: 25 maggio 2024

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  1. Articoli di riviste
  2. Tesi
  3. Libri
  4. Capitoli di libri
  5. Atti di convegni

Articoli di riviste sul tema "Bassin du Changjiang (Yangtze)":

1

Men, Ke-Pei, e Shu-Dan Zhu. "The Ordered Network Structure and its Prediction for the Big Floods of the Changjiang River Basins". Zeitschrift für Naturforschung A 68, n. 12 (1 dicembre 2013): 766–72. http://dx.doi.org/10.5560/zna.2013-0061.

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Abstract (sommario):
According to the latest statistical data of hydrology, a total of 21 floods took place over the Changjiang (Yangtze) River Basins from 1827 to 2012 and showed an obvious commensurable orderliness. In the guidance of the information forecasting theory of Wen-Bo Weng, based on previous research results, combining ordered analysis with complex network technology, we focus on the summary of the ordered network structure of the Changjiang floods, supplement new information, further optimize networks, construct the 2D- and 3D-ordered network structure and make prediction research. Predictions show that the future big deluges will probably occur over the Changjiang River Basin around 2013 - 2014, 2020 - 2021, 2030, 2036, 2051, and 2058.
2

Cheung, Richard Ching Wa, Moriaki Yasuhara, Hokuto Iwatani, Chih-Lin Wei e Yun-wei Dong. "Benthic community history in the Changjiang (Yangtze River) mega-delta: Damming, urbanization, and environmental control". Paleobiology 45, n. 3 (22 luglio 2019): 469–83. http://dx.doi.org/10.1017/pab.2019.21.

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AbstractThe coastal environment of the Changjiang delta has been influenced by recent anthropogenic activities such as dam construction and increased sewage and fertilizer inputs. Previous work examined the compositional shift of marine plankton to assess ecological impacts of these activities on marine ecosystems in the Changjiang discharge area. Here we used benthic marine ostracodes collected in the Changjiang estuary and the adjacent East China Sea in the 1980s and the 2010s, respectively, to investigate temporal changes of the benthic community and controlling factors for the benthic fauna. Our results revealed more shoreward distribution of some well-known offshore ostracode species in the 2010s compared with the 1980s and a relatively more important role for environmental processes (e.g., bottom-water temperature, bottom-water salinity, and eutrophic conditions of surface water) than spatial processes (e.g., the flow of ocean currents) in structuring ostracode compositions. The temporal changes in the ostracode community are likely attributable to the combined effects of reduced fresh water and sediment discharge and eutrophic conditions of the Changjiang due to the many dams constructed along the Changjiang and population expansion in the Changjiang Basin. Results of redundancy analysis and variation partitioning suggest that ocean currents facilitated environmental filtering of ostracode species such that they could disperse to preferred environmental conditions. These findings highlight the potential uses of marine microfossils to better understand ecological impacts on benthic ecosystems in vulnerable Asian mega-deltas and provide insights into the integration of metacommunity concepts in disentangling dynamics of marine benthic communities.
3

Shankman, David, Barry D. Keim, Tadanobu Nakayama, Rongfang Li, Dunyin Wu e W. Craig Remington. "Hydroclimate Analysis of Severe Floods in China’s Poyang Lake Region". Earth Interactions 16, n. 14 (1 dicembre 2012): 1–16. http://dx.doi.org/10.1175/2012ei000455.1.

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Abstract Poyang Lake in Jiangxi Province is the largest freshwater lake in China and is historically a region of significant floods. Maximum annual lake stage and the number of severe flood events have increased during the past few decades because of levee construction that reduced the area available for floodwater storage. The most severe floods since 1950 occurred during 1954, 1973, 1983, 1995, and 1998. Each of these floods followed El Niño events that influence the Asian monsoon and that are directly linked to rainfall in the Changjiang (Yangtze River) basin. The 1954 flood was the largest ever recorded until the 1990s. That year the peak Changjiang stage at Hukou was 21.6 m, which was 1.6 m above the previous record high. The last major flood on the Changjiang was during 1998, when the peak Changjiang stage reached 22.5 m, higher than during 1954, even though peak discharge was lower. The most severe floods, including those in 1954 and 1998, require both 1) high rainfall and tributary discharge into Poyang Lake and 2) high Changjiang discharge and stage at Hukou that backflows into the lake or slows Poyang Lake drainage. Since gauging stations were established on the Changjiang, these conditions always occurred following an El Niño.
4

Kubota, Y., R. Tada e K. Kimoto. "Changes in East Asian summer monsoon precipitation during the Holocene deduced from a freshwater flux reconstruction of the Changjiang (Yangtze River) based on the oxygen isotope mass balance in the northern East China Sea". Climate of the Past 11, n. 2 (17 febbraio 2015): 265–81. http://dx.doi.org/10.5194/cp-11-265-2015.

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Abstract. The δ18O of seawater (δ18Ow), an indirect indicator of sea surface salinity (SSS), in the northern East China Sea (ECS) is reconstructed for the Holocene using paired analyses of Mg / Ca ratio and δ18O of planktic foraminiferal tests. According to modern observation, interannual variations in SSS during summer in the northern ECS are mainly controlled by the Changjiang (Yangtze River) discharge, which reflects summer rainfall in its drainage basin. Thus, changes in the summer SSS in the northern ECS are interpreted as reflecting variations in the East Asian summer monsoon (EASM) precipitation in the Changjiang Basin. This interpretation is confirmed by a strong relationship between the SSS in the northern ECS and the Changjiang discharge during the wet season (May–October) based on instrumental salinity records from 1951 to 2000. However, it is difficult to estimate absolute salinity values in the past with high accuracy, because the past salinity–δ18Ow regression slope, end member salinity, and δ18Ow values are not well understood. Here, we conduct δ18Ow mass-balance calculation to estimate the freshwater contribution to the surface water of the northern ECS during the last 7 kyr by assuming a simple mixing between two end members – the seawater and the Changjiang freshwater. The result indicates that there has been no gradual decreasing secular trend in the Changjiang freshwater flux from the middle Holocene to the present day, suggesting that summer insolation in the Northern Hemisphere does not regulate the EASM precipitation in the Changjiang Basin. Instead, internal feedback appears to have been more important during the Holocene. The absence of a decreasing trend in regional summer precipitation over the Changjiang Basin since the middle Holocene is contradictory to Chinese speleothems' δ18O records, suggesting that it is not possible to explain orbital changes in Chinese speleothems' δ18O during the Holocene by changes in summer precipitation, but that such changes are related to other factors such as changes in the moisture source.
5

Huang, Y., W. F. Yang e L. Chen. "Water resources change in response to climate change in Changjiang River basin". Hydrology and Earth System Sciences Discussions 7, n. 3 (25 maggio 2010): 3159–88. http://dx.doi.org/10.5194/hessd-7-3159-2010.

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Abstract. Doubtlessly, global climate change and its impacts have caught increasing attention from all sectors of the society world-widely. Among all those affected aspects, hydrological circle has been found rather sensitive to climate change. Climate change, either as the result or as the driving-force, has intensified the uneven distribution of water resources in the Changjiang (Yangtze) River basin, China. In turn, drought and flooding problems have been aggravated which has brought new challenges to current hydraulic works such as dike or reservoirs which were designed and constructed based on the historical hydrological characteristics, yet has been significantly changed due to climate change impact. Thus, it is necessary to consider the climate change impacts in basin planning and water resources management, currently and in the future. To serve such purpose, research has been carried out on climate change impact on water resources (and hydrological circle) in Changjiang River. The paper presents the main findings of the research, including main findings from analysis of historical hydro-meteorological data in Changjiang River, and runoff change trends in the future using temperature and precipitation predictions calculated based on different emission scenarios of the 24 Global Climate Modes (GCMs) which has been used in the 4th IPCC assessment report. In this research, two types of macro-scope statistical and hydrological models were developed to simulate runoff prediction. Concerning the change trends obtained from the historical data and the projection from GCMs results, the trend of changes in water resources impacted by climate change was analyzed for Changjiang River. Uncertainty of using the models and data were as well analyzed.
6

Hu, Jingwen, Zhengxin Yang, Yuxin Yi, Zhaoqing Shu, Pan Yu, Qingmin You e Quanxi Wang. "Possible Origin and Distribution of an Invasive Diatom Species, Skeletonema potamos, in Yangtze River Basin (China)". Water 15, n. 16 (9 agosto 2023): 2875. http://dx.doi.org/10.3390/w15162875.

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Skeletonema potamos is a freshwater diatom that has been widely distributed in North America, Europe, and Australia since the 1980s. However, there have been few previous reports of S. potamos in China. Only recently has S. potamos been frequently found in our extensive ecological surveys in China, and it has sometimes even been the dominant species. This study clarified the morphology, distribution, and origin of S. potamos, as well as the underlying mechanism contributing to its dominance. We examined the samples collected from the Changjiang River (Yangtze River) Basin during 2016–2022 and determined their geographical distribution. Genetic distance analysis indicated that S. potamos strains in China might have been transported by ships and ballast water from the USA or Japan through the East Sea into the Yangtze River Estuary. Cargo ships possibly contribute to its dispersal. An analysis of the ecological factors affecting the occurrence and distribution of S. potamos in China indicated that many waterbodies provide environments suitable for S. potamos. The suitable environment, small size, and rapid reproduction of S. potamos are the reasons for its dominance in the Yangtze River Basin. We predict that S. potamos is likely to form “blooms” in China in the future.
7

Chen, Zhongyuan, e Yiwen Zhao. "Impact on the Yangtze (Changjiang) Estuary from its drainage basin: Sediment load and discharge". Chinese Science Bulletin 46, S1 (gennaio 2001): 73–80. http://dx.doi.org/10.1007/bf03187240.

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8

Tang, Xianqiang, Rui Li, Ding Han e Miklas Scholz. "Response of Eutrophication Development to Variations in Nutrients and Hydrological Regime: A Case Study in the Changjiang River (Yangtze) Basin". Water 12, n. 6 (7 giugno 2020): 1634. http://dx.doi.org/10.3390/w12061634.

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Data and literature related to water quality as well as nutrient loads were used to evaluate the Changjiang River (also Yangtze or Yangzi) Basin with respect to its hydrological regime, sediment transport, and eutrophication status. Waterbodies exhibited different eutrophic degrees following the ranking order of river < reservoir < lake. Most of the eutrophic lakes and reservoirs distributed in the upstream Sichuan Basin and Jianghan Plain are located in the middle main stream reaches. During the past decade, the water surface area proportion of moderately eutrophic lakes to total evaluated lakes continually increased from 31.3% in 2009 to 42.7% in 2018, and the trophic level of reservoirs rapidly developed from mesotrophic to slightly eutrophic. Construction and operation of numerous gates and dams changed the natural transportation rhythm of runoff, suspended solids (SS), and nutrients, and reduced flow velocity, resulting in decreased discharge runoff, slow water exchange, and decreased connectivity between rivers and lakes as well as accumulated nutrient and SS, which are the main driving forces of eutrophication. To mitigate eutrophication, jointly controlling and monitoring nutrient concentrations and flux at key sections, strengthening water quality management for irrigation backwater and aquaculture wastewater, and balancing transportation among runoff, SS, and nutrients is recommended.
9

SATO, Osamu, Takao NAKAGAWA e Tetsuo HASHIMOTO. "Recent tritium levels in environmental waters collected at the drainage basin of Changjiang (Yangtze river), China." RADIOISOTOPES 38, n. 12 (1989): 529–36. http://dx.doi.org/10.3769/radioisotopes.38.12_529.

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10

Li, Gen, Xingchen T. Wang, Zhongfang Yang, Changping Mao, A. Joshua West e Junfeng Ji. "Dam-triggered organic carbon sequestration makes the Changjiang (Yangtze) river basin (China) a significant carbon sink". Journal of Geophysical Research: Biogeosciences 120, n. 1 (gennaio 2015): 39–53. http://dx.doi.org/10.1002/2014jg002646.

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Ti possono interessare anche gli elenchi estesi di opere sul tema "Bassin du Changjiang (Yangtze)":
Articoli di riviste Libri

Tesi sul tema "Bassin du Changjiang (Yangtze)":

1

Morgan, Stephen Lloyd. "County-town enterprises in the lower Changjiang (Yangtze) River basin: implications of rural industrialization forurbanization in the Chinese countryside since the reform of 1978". Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1987. http://hub.hku.hk/bib/B31949162.

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2

Yang, Chengfan. "Li isotope study of Yangtze River sediments : new constraints on climate, weathering and carbon cycle relationships". Electronic Thesis or Diss., Sorbonne université, 2020. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2020SORUS433.pdf.

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Abstract (sommario):
Au cours de ce travail, j’ai réalisé une série d'études dans le bassin du Changjiang (Yangtze), afin de mieux comprendre l'influence de ces effets.Tout d'abord, l'exploitation du barrage des Trois Gorges (TGD) a modifié la composition géochimique des sédiments en aval. Depuis 2003, les sédiments venant des hauts bassins ont été en grande partie retenus en amont, tandis que les sédiments précédemment déposés dans le bassin moyen-inférieur ont été progressivement remis en suspension. Ces processus expliquent l’évolution géochimique des sédiments exportés vers la mer de Chine. En deuxième partie, une étude systématique démontre que les compositions isotopiques en lithium des phases dissoutes et particulaires se comportent de façon conservative dans la zone de mélange de l'estuaire du Changjiang. Cependant, les phases échangeables ne représentent qu'une faible quantité de Li, ce qui explique son impact négligeable dans cette zone. Troisièmement, Cette étude confirme que dans les grands bassins versants, l'altération chimique peut réagir rapidement à de grandes amplitudes climatiques. Ceci est particulièrement bien illustré, dans la carotte CM97, par la période du Younger Dryas. Depuis 2 000 ans, les δ7Li des argiles s’accentuent clairement par rapport à la période précédente, à cause de l'érosion des sols de plaines induite par l'homme. En résumé, ces résultats apportent de nouveaux éclairages sur l'interprétation des proxys et sur la réponse de l'altération chimique aux variations climatiques, ce qui est essentiel pour mieux quantifier l’impact du l’altération continentale sur les climats passés et futurs de notre planète
In order to better understand the weathering-climate feedback, a series of studies was carried out in the Changjiang (Yangtze) Basin. First, the operation of the Three Gorges Dam (TGD) changed downstream sediment geochemical compositions. Before 2003, large amounts of upstream-derived sediments deposited and experienced further weathering in the mid-lower basin. Since 2003, strong riverbed sediment resuspension changed the roles of the mid-lower reaches from important sinks to major sources of sediments delivered to the sea. As a consequence, an intensified weathering intensity of downstream sediment was observed.Second, dissolved δ7Li exhibit a conservative behavior in the Changjiang Estuary. During the process of SPM transported offshore, weathering product flocculated and deposited, while primary minerals resuspended. The combined effect resulted in the UCC-like SPM δ7Li values. There is a Li isotope fractionation between the dissolved load and exchangeable phase. However, this process shows negligible impact on δ7Li of dissolved load and particulates. Third, weathering response to climate is complex in large river basins. During the Younger Dryas, the positive excursion of clay δ7Li is consistent with enhanced incongruent weathering, in response to temperature cooling. The minor variation of clay δ7Li at 11 – 2 ka likely indicate stable weathering and mile climate variation. Over the last 2 kyr, the fluctuation of clay δ7Li is mostly caused by intensification of human activities. In summary, this thesis sheds new lights on the weathering-climate feedback over geologic past, and provides perspectives on how human activities affect natural processes

Libri sul tema "Bassin du Changjiang (Yangtze)":

1

Hayashi, Seiji. Modeling of daily runoff in the Changjiang (Yangtze) River basin and its application to evaluating the flood control effect of the Three Gorges project. Tsukuba-shi, Japan: National Institute for Environmental Studies, 2005.

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2

1916-, Xu Xiaobing, a cura di. Changjiang. 8a ed. Chongqing: Chongqing chu ban she, 1993.

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3

Peijin, Lan, e Cao Lei, a cura di. Changjiang Sanxia =: Three Gorges on Yangtze River. 8a ed. Beijing: Wai wen chu ban she, 1997.

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4

Zhang, Ren. Changjiang yu San xia gong cheng. Beijing: Qing hua da xue chu ban she, 1998.

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5

Yun, Caixing. Tu shuo Chang Jiang he kou yan bian: Tushuo Changjiang hekou yanbian. 8a ed. Beijing Shi: Hai yang chu ban she, 2010.

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6

Chung-kuo kʻo hsüeh yüan. Research Group on Impacts of the Three Gorges Project on Ecology and Environment. Atlas of ecology and environment in the Three Gorges area of the Changjiang River. Beijing, China: Science Press, 1990.

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7

Zhou, Ting. Changjiang shang you jing ji dai yu sheng tai ping zhang gong jian yan jiu. 8a ed. Beijing: Jing ji ke xue chu ban she, 2008.

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8

Zhang, Jing, a cura di. Ecological Continuum from the Changjiang (Yangtze River) Watersheds to the East China Sea Continental Margin. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16339-0.

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9

1950-, Hong Yinxing, e Liu Zhibiao 1959-, a cura di. Changjiang Sanjiaozhou Diqu jing ji fa zhan de mo shi he ji zhi. 8a ed. Beijing: Qing hua da xue chu ban she, 2003.

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10

Huang, Philip C. Changjiang san jiao zhou xiao nong jia ting yu xiang cun fa zhan. Hong Kong: Oxford University Press, 1994.

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Capitoli di libri sul tema "Bassin du Changjiang (Yangtze)":

1

He, Qing, Leicheng Guo, Hong Liu e Ya Wang. "Changjiang Estuary Sediment Transport Dynamics". In Ecological Continuum from the Changjiang (Yangtze River) Watersheds to the East China Sea Continental Margin, 47–69. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16339-0_3.

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2

Zhang, Liquan, Lin Yuan e Huamei Huang. "Coastal Wetlands in the Changjiang Estuary". In Ecological Continuum from the Changjiang (Yangtze River) Watersheds to the East China Sea Continental Margin, 137–59. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16339-0_7.

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3

Yanling, Liang. "Preliminary study of the aquatic Oligochaeta of the Changjiang (Yangtze) River". In Aquatic Oligochaeta, 195–98. Dordrecht: Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3091-9_26.

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4

Vezzoli, G., M. Limonta, E. Garzanti e S. Yang. "Quantitative Provenance Analysis of Sediments in the Changjiang (Yangtze) River (China)". In Geostatistical and Geospatial Approaches for the Characterization of Natural Resources in the Environment, 293–300. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-18663-4_45.

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5

Zhu, Jianrong, Hui Wu e Lu Li. "Hydrodynamics of the Changjiang Estuary and Adjacent Seas". In Ecological Continuum from the Changjiang (Yangtze River) Watersheds to the East China Sea Continental Margin, 19–45. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16339-0_2.

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6

Xu, Zhao Li, Xiao Min Shen e Qian Gao. "Marine Biology of the Changjiang (Yangtze River) Estuary and Adjacent East China Sea Shelf". In Ecological Continuum from the Changjiang (Yangtze River) Watersheds to the East China Sea Continental Margin, 161–80. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16339-0_8.

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7

Wu, Ying, Zhuoyi Zhu, Hongyan Bao, Shuchai Gan e Jing Zhang. "Organic Matter and Biomarkers of the Changjiang Estuary and East China Sea Shelf". In Ecological Continuum from the Changjiang (Yangtze River) Watersheds to the East China Sea Continental Margin, 119–35. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16339-0_6.

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8

Zhang, Jing, Ying Wu e Ying Ying Zhang. "Plant Nutrients and Trace Elements from the Changjiang Watersheds to the East China Sea". In Ecological Continuum from the Changjiang (Yangtze River) Watersheds to the East China Sea Continental Margin, 93–118. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16339-0_5.

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9

Zhang, Jing. "Land–Ocean Interactions Between the Changjiang (Yangtze River) Watersheds to the East China Sea Continental Margin". In Ecological Continuum from the Changjiang (Yangtze River) Watersheds to the East China Sea Continental Margin, 1–18. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16339-0_1.

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10

Yang, S. L., e H. F. Yang. "Temporal Variations in Water and Sediment Discharge from the Changjiang (Yangtze River) and Downstream Sedimentary Responses". In Ecological Continuum from the Changjiang (Yangtze River) Watersheds to the East China Sea Continental Margin, 71–91. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16339-0_4.

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Atti di convegni sul tema "Bassin du Changjiang (Yangtze)":

1

Duan, Zhifei, Chao Li, Shouye Yang, Yulong Guo, Juan Xu, Ergang Lian, Xiangtong Huang e Chenyang Jin. "Comminution ages constrain sediment residence time in the large Changjiang (Yangtze) river catchment". In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.5759.

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2

Vasquez Vargas, Ana, Shouye Yang, Simon Hohl, Zhiwei He, Junjie Guo e Qiang Hao. "Anthropogenic source identification and the naturally heavy Cu isotopic signatures in the Changjiang (Yangtze River)". In Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.16399.

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3

Chen, Jianyu, Xiaobo Ni, Zhihua Mao, Yifan Wang, Lijin Liang e Fang Gong. "Remote sensing and buoy based effect analysis of typhoon on hypoxia off the Changjiang (Yangtze) Estuary". In SPIE Remote Sensing, a cura di Charles R. Bostater, Stelios P. Mertikas, Xavier Neyt, Caroline Nichol, Dave Cowley e Jean-Paul Bruyant. SPIE, 2012. http://dx.doi.org/10.1117/12.974398.

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Li, Chao, Junfei Chen e Shouye Yang. "The Sediment Residence Times of Changjiang (Yangtze River) Catchment Response to Climate Change during last 14 kyrs". In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.10318.

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5

Cao, Fang, Shou-ye Yang, Cheng-fan Yang, Yu-long Guo, Lei Bi e Yu-ze Li. "Using lithium isotopes to quantitatively extract the silicate weathering signal registered in the Changjiang (Yangtze) estuarine sediments". In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.4666.

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Zhang, Xiaoyu. "Reduced Trace Metals in the Sediments of the Changjiang (Yangtze) Estuary：Evidence of Impacts from Three Gorges Dam Construction". In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.3134.

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7

Chen, Yang, Shilei Li, Jun Chen, Gen Li e Weiqiang Li. "Effects of secondary carbonate precipitation and dissolution on Changjiang (Yangtze) river chemistry and estimates of silicate weathering rates". In Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.15481.

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Vasquez Vargas, Ana Cristina, Junjie Guo, Zhiwei He, Shouye Yang, Ni Su e Qiang Hao. "Unusually heavy Cu isotope signatures of the Changjiang (Yangtze) River: The impact of chemical weathering and delivery to the oceans". In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.9313.

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Guo, Junjie, Ni Su, Ana Vasquez Vargas, Qiang Hao, Shouye Yang e Zhiwei He. "Geochemical characteristics of the Changjiang (Yangtze) River water during a large flood event and implications for enhanced chemical weathering and CO2 consumption". In Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.17363.

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