GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Bay of Bengal  (2)
  • 13.1; 15.1; 15.2; 15.3; 16.1; Angola Basin; Cerium, dissolved; Congo_River_12-1; Congo_River_12-2; Congo_River_12-3; Congo River; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; Dysprosium, dissolved; Erbium, dissolved; Europium, dissolved; Event label; GA08; Gadolinium, dissolved; GEOTRACES; Global marine biogeochemical cycles of trace elements and their isotopes; hafnium; Hafnium, dissolved; Hafnium-176/Hafnium-177; Holmium, dissolved; ICP-MS, Elemental Scientific, seaFAST; IFISH; Iron fish; Isotope dilution; Lanthanum, dissolved; LATITUDE; LONGITUDE; Lutetium, dissolved; M121; M121_1200-1; M121_1202-1; M121_1202-1_fish65; M121_1206-1; M121_1210-1; M121_1210-1_fish69-15.1; M121_1210-1_fish69-15.2; M121_1210-1_fish69-15.3; M121_1212-1; M121_1214-1; M121_1214-1_fish77; M121_1218-1; M121_1222-1; M121_1224-1; M121_1226-1; M121_1228-1; M121_1230-1; M121_1232-1; M121_1234-1; M121_1236-1; M121_1238-1; M121_1240-1; M121_1243-1; M121_1247-1; M121_1248-1; M121_1250-1; Meteor (1986); Neodymium; Neodymium, dissolved; Neodymium-143/Neodymium-144 ratio; Praseodymium, dissolved; RIVER; Salinity; Samarium, dissolved; Sampling river; Southeast Atlantic; South East Atlantic Ocean; Station label; Temperature, water; Terbium, dissolved; Thulium, dissolved; Ytterbium, dissolved; ε-Hafnium; ε-Hafnium, standard deviation; ε-Neodymium; ε-Neodymium, standard deviation  (1)
  • 165-999; AGE; Aluminium/Calcium ratio; Aluminium/Neodymium ratio; Caribbean Sea; COMPCORE; Composite Core; Depth, composite; Iron; Iron/Calcium ratio; Iron/Manganese ratio; Joides Resolution; Leg165; Manganese; Manganese/Calcium ratio; Sample ID  (1)
Document type
Keywords
Publisher
Years
  • 1
    Publication Date: 2023-12-09
    Keywords: 165-999; AGE; Aluminium/Calcium ratio; Aluminium/Neodymium ratio; Caribbean Sea; COMPCORE; Composite Core; Depth, composite; Iron; Iron/Calcium ratio; Iron/Manganese ratio; Joides Resolution; Leg165; Manganese; Manganese/Calcium ratio; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 333 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2024-02-02
    Description: To better understand the inputs of riverine REEs and Hf to the ocean and their impact on the open ocean we collected filtered seawater samples from 16 full water column profiles along the Congo River plume at the coast of Congo and Gabon and along an offshore section at 3°S, complemented by three freshwater samples collected directly from the Congo River. The water samples from the Congo River plume were collected during GEOTRACES cruise GA08 with German RV Meteor (M121) in November and December 2015 with a stainless steel CTD rosette and a towed fish for surface waters. River water end-member samples from the Congo River at zero salinity were taken upstream by boat in May, July and October 2017 near the center of the river at ~6°S and ~12.5°E (stations 12.1–12.3). We determine for the first time REE and Hf concentrations and isotope compositions within the Congo River plume and quantify Nd and Hf fluxes. Based on these data we evaluate how far the Congo River plume is traceable by these geochemical parameters, how it contributes to their budgets in the South East Atlantic Ocean, and to which degree the Nd and Hf isotope and REE distributions can be used as water mass tracers in areas of high continental inputs.
    Keywords: 13.1; 15.1; 15.2; 15.3; 16.1; Angola Basin; Cerium, dissolved; Congo_River_12-1; Congo_River_12-2; Congo_River_12-3; Congo River; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; Dysprosium, dissolved; Erbium, dissolved; Europium, dissolved; Event label; GA08; Gadolinium, dissolved; GEOTRACES; Global marine biogeochemical cycles of trace elements and their isotopes; hafnium; Hafnium, dissolved; Hafnium-176/Hafnium-177; Holmium, dissolved; ICP-MS, Elemental Scientific, seaFAST; IFISH; Iron fish; Isotope dilution; Lanthanum, dissolved; LATITUDE; LONGITUDE; Lutetium, dissolved; M121; M121_1200-1; M121_1202-1; M121_1202-1_fish65; M121_1206-1; M121_1210-1; M121_1210-1_fish69-15.1; M121_1210-1_fish69-15.2; M121_1210-1_fish69-15.3; M121_1212-1; M121_1214-1; M121_1214-1_fish77; M121_1218-1; M121_1222-1; M121_1224-1; M121_1226-1; M121_1228-1; M121_1230-1; M121_1232-1; M121_1234-1; M121_1236-1; M121_1238-1; M121_1240-1; M121_1243-1; M121_1247-1; M121_1248-1; M121_1250-1; Meteor (1986); Neodymium; Neodymium, dissolved; Neodymium-143/Neodymium-144 ratio; Praseodymium, dissolved; RIVER; Salinity; Samarium, dissolved; Sampling river; Southeast Atlantic; South East Atlantic Ocean; Station label; Temperature, water; Terbium, dissolved; Thulium, dissolved; Ytterbium, dissolved; ε-Hafnium; ε-Hafnium, standard deviation; ε-Neodymium; ε-Neodymium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 1257 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2021-07-21
    Description: The development of the South Asian monsoon (SAM) and Himalaya‐Tibetan Plateau uplift were closely intertwined with some studies suggesting that uplift initiated the monsoon whereas others link tectonics with monsoon‐controlled exhumation. Silicate weathering controls atmospheric CO2 on geological timescales resulting in a large potential for monsoon strength and the Himalayan orogeny to influence global climate but detailed records of SAM‐induced weathering on million year (Myr) timescales are lacking. Here, we present radiogenic Sr, Nd, and Pb isotope compositions of clay minerals produced by silicate weathering and transported to the central Bay of Bengal. The radiogenic isotope data exhibit a relatively small range and demonstrate a remarkably consistent mixture of sources dominated by Himalayan rocks and the Indo‐Burman ranges, which consist of sediments derived from the Himalayas. This suggests that the spatial pattern of regional weathering, which today is highest in the regions of strongest monsoon rains, has persisted in a similar form for the last 27 Myrs. A pronounced increase in primary clay mineral abundance (from 9% to 22%) coincident with global cooling 13.9 Myrs ago points to a shift in the weathering regime given that the clay provenance did not change dramatically. Relatively weaker chemical weathering intensity during the mid and late Miocene cooling suggests increased aridity and changes in the large scale atmospheric circulation in the SAM domain. The establishment of the dry winter monsoon season during the mid and late Miocene may have caused this shift in the weathering regime and can reconcile much of the contrasting evidence for SAM initiation.
    Description: Key Points: Relatively stable mixture of source rocks weathered to clays over the past 27 Myrs Pronounced increase in primary clay minerals occurred 13.9 Myrs ago Shift in weathering regime possibly result of winter monsoon dry season development
    Keywords: 551.3 ; Bay of Bengal ; clay minerals ; radiogenic Sr, Nd, Pb isotopes ; Silicate silicate weathering ; South Asian monsoon
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2021-07-21
    Description: Tectonics and regional monsoon strength control weathering and erosion regimes of the watersheds feeding into the Bay of Bengal, which are important contributors to global climate evolution via carbon cycle feedbacks. The detailed mechanisms controlling the input of terrigenous clay to the Bay of Bengal on tectonic to orbital timescales are, however, not yet well understood. We produced orbital‐scale resolution geochemical records for International Ocean Discovery Program Site U1443 (southern Bay of Bengal) across five key climatic intervals of the middle to late Miocene (15.8–9.5 Ma). Our new radiogenic Sr, Nd, and Pb isotope time series of clays transported to the Ninetyeast Ridge suggest that the individual contributions from different erosional sources overall remained remarkably consistent during the Miocene despite major tectonic reorganizations in the Himalayas. On orbital timescales, however, high‐resolution data from the five investigated intervals show marked fluctuations of all three isotope systems. Interestingly, the variability was much higher within the Miocene Climatic Optimum (around 16–15 Ma) and across the major global cooling (~13.9–13.8 Ma) until ~13.5 Ma, than during younger time intervals. This change is attributed to a major restriction on the supply of High Himalayan erosion products due to migration of the peak precipitation area toward the frontal domains of the Himalayas and the Indo‐Burman Ranges. The transient excursions of the radiogenic isotope signals on orbital timescales most likely reflect climatically driven shifts in monsoon strength.
    Description: Key Points: A consistent mix of clay sources contributed to the Bay of Bengal throughout the middle to late Miocene A marked change in detrital Sr, Nd, and Pb isotope variability at 13.5 Ma was related to Miocene global cooling Transient orbital‐scale fluctuations in clay source most likely reflect changes in monsoon intensity
    Description: Deutsche Forschungsgemeinschaft (DFG) http://dx.doi.org/10.13039/501100001659
    Keywords: 551 ; Bay of Bengal ; IODP Site U1443 ; Miocene ; sediment provenance ; Himalayas ; weathering ; erosion
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...