Trace elements in New Zealand ferromanganese nodules: implications for deep sea environments
Ferromanganese nodules are authigenic marine sediments that form over millions of years from the precipitation of Fe oxyhydroxides and Mn oxides from seawater (hydrogenetic-type growth) and sediment pore-water (diagenetic-type growth). Fe-Mn (oxyhydr)oxides grow in layers about nuclei, effectively s...
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ftvictoriauwfig:oai:figshare.com:article/17131868 2023-10-25T01:44:06+02:00 Trace elements in New Zealand ferromanganese nodules: implications for deep sea environments Davies, Andrea 2018-01-01T00:00:00Z https://doi.org/10.26686/wgtn.17131868 https://figshare.com/articles/thesis/Trace_elements_in_New_Zealand_ferromanganese_nodules_implications_for_deep_sea_environments/17131868 unknown doi:10.26686/wgtn.17131868 https://figshare.com/articles/thesis/Trace_elements_in_New_Zealand_ferromanganese_nodules_implications_for_deep_sea_environments/17131868 CC BY-NC-SA 4.0 Inorganic geochemistry Marine geoscience Chemical oceanography Geochemistry Ferromanganese Oceanography School: School of Geography Environment and Earth Sciences 040202 Inorganic Geochemistry 040502 Chemical Oceanography 040305 Marine Geoscience 970104 Expanding Knowledge in the Earth Sciences Degree Discipline: Geology Degree Level: Masters Degree Name: Master of Science Text Thesis 2018 ftvictoriauwfig https://doi.org/10.26686/wgtn.17131868 2023-09-27T23:16:39Z Ferromanganese nodules are authigenic marine sediments that form over millions of years from the precipitation of Fe oxyhydroxides and Mn oxides from seawater (hydrogenetic-type growth) and sediment pore-water (diagenetic-type growth). Fe-Mn (oxyhydr)oxides grow in layers about nuclei, effectively scavenging minor metals such as Ni, Cu and Co from the waters they grow in. The uptake of different elements into the ferromanganese nodules reflects their environment and mechanism of growth, and these deposits are of interest both as a potential source of metals of economic interest, and as records of changing ocean conditions. This study investigates the composition of 77 ferromanganese nodules from the seafloor around New Zealand. Samples analysed come from locations several thousand kilometres apart under the same water mass (Lower Circumpolar Deep Water – LCDW), but with varying depth, current velocity, and sediment type. The outermost 1 mm rim of each nodule, representing near-modern growth, was sampled to compare with modern environmental parameters including substrate sediment composition and chemical and physical oceanography. Major, minor, and trace element analysis of nodule rims were undertaken, and the authigenic and detrital components examined via leaching experiments to evaluate their relative influence on growth mechanisms. Overall, New Zealand ferromanganese nodules are hydrogenetic in origin. However, there are systematic variations in composition that reflect variable diagenetic influence. Hydrogenetic endmember compositions are defined by samples from two localities in the Southern Ocean that have no evidence for diagenetic influence. Diagenetic influence on nodule composition is exemplified by samples from the two locations in the Tasman Sea, but also include nodules from the Campbell nodule field. Nodules from the Campbell nodule field come from two transects perpendicular to the Campbell Plateau, and the Deep Western Boundary Current (DWBC). Both sediment composition and nodule rim chemistry ... Thesis Southern Ocean Open Access Victoria University of Wellington / Te Herenga Waka Southern Ocean New Zealand Campbell Plateau ENVELOPE(171.000,171.000,-50.667,-50.667) |
institution |
Open Polar |
collection |
Open Access Victoria University of Wellington / Te Herenga Waka |
op_collection_id |
ftvictoriauwfig |
language |
unknown |
topic |
Inorganic geochemistry Marine geoscience Chemical oceanography Geochemistry Ferromanganese Oceanography School: School of Geography Environment and Earth Sciences 040202 Inorganic Geochemistry 040502 Chemical Oceanography 040305 Marine Geoscience 970104 Expanding Knowledge in the Earth Sciences Degree Discipline: Geology Degree Level: Masters Degree Name: Master of Science |
spellingShingle |
Inorganic geochemistry Marine geoscience Chemical oceanography Geochemistry Ferromanganese Oceanography School: School of Geography Environment and Earth Sciences 040202 Inorganic Geochemistry 040502 Chemical Oceanography 040305 Marine Geoscience 970104 Expanding Knowledge in the Earth Sciences Degree Discipline: Geology Degree Level: Masters Degree Name: Master of Science Davies, Andrea Trace elements in New Zealand ferromanganese nodules: implications for deep sea environments |
topic_facet |
Inorganic geochemistry Marine geoscience Chemical oceanography Geochemistry Ferromanganese Oceanography School: School of Geography Environment and Earth Sciences 040202 Inorganic Geochemistry 040502 Chemical Oceanography 040305 Marine Geoscience 970104 Expanding Knowledge in the Earth Sciences Degree Discipline: Geology Degree Level: Masters Degree Name: Master of Science |
description |
Ferromanganese nodules are authigenic marine sediments that form over millions of years from the precipitation of Fe oxyhydroxides and Mn oxides from seawater (hydrogenetic-type growth) and sediment pore-water (diagenetic-type growth). Fe-Mn (oxyhydr)oxides grow in layers about nuclei, effectively scavenging minor metals such as Ni, Cu and Co from the waters they grow in. The uptake of different elements into the ferromanganese nodules reflects their environment and mechanism of growth, and these deposits are of interest both as a potential source of metals of economic interest, and as records of changing ocean conditions. This study investigates the composition of 77 ferromanganese nodules from the seafloor around New Zealand. Samples analysed come from locations several thousand kilometres apart under the same water mass (Lower Circumpolar Deep Water – LCDW), but with varying depth, current velocity, and sediment type. The outermost 1 mm rim of each nodule, representing near-modern growth, was sampled to compare with modern environmental parameters including substrate sediment composition and chemical and physical oceanography. Major, minor, and trace element analysis of nodule rims were undertaken, and the authigenic and detrital components examined via leaching experiments to evaluate their relative influence on growth mechanisms. Overall, New Zealand ferromanganese nodules are hydrogenetic in origin. However, there are systematic variations in composition that reflect variable diagenetic influence. Hydrogenetic endmember compositions are defined by samples from two localities in the Southern Ocean that have no evidence for diagenetic influence. Diagenetic influence on nodule composition is exemplified by samples from the two locations in the Tasman Sea, but also include nodules from the Campbell nodule field. Nodules from the Campbell nodule field come from two transects perpendicular to the Campbell Plateau, and the Deep Western Boundary Current (DWBC). Both sediment composition and nodule rim chemistry ... |
format |
Thesis |
author |
Davies, Andrea |
author_facet |
Davies, Andrea |
author_sort |
Davies, Andrea |
title |
Trace elements in New Zealand ferromanganese nodules: implications for deep sea environments |
title_short |
Trace elements in New Zealand ferromanganese nodules: implications for deep sea environments |
title_full |
Trace elements in New Zealand ferromanganese nodules: implications for deep sea environments |
title_fullStr |
Trace elements in New Zealand ferromanganese nodules: implications for deep sea environments |
title_full_unstemmed |
Trace elements in New Zealand ferromanganese nodules: implications for deep sea environments |
title_sort |
trace elements in new zealand ferromanganese nodules: implications for deep sea environments |
publishDate |
2018 |
url |
https://doi.org/10.26686/wgtn.17131868 https://figshare.com/articles/thesis/Trace_elements_in_New_Zealand_ferromanganese_nodules_implications_for_deep_sea_environments/17131868 |
long_lat |
ENVELOPE(171.000,171.000,-50.667,-50.667) |
geographic |
Southern Ocean New Zealand Campbell Plateau |
geographic_facet |
Southern Ocean New Zealand Campbell Plateau |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_relation |
doi:10.26686/wgtn.17131868 https://figshare.com/articles/thesis/Trace_elements_in_New_Zealand_ferromanganese_nodules_implications_for_deep_sea_environments/17131868 |
op_rights |
CC BY-NC-SA 4.0 |
op_doi |
https://doi.org/10.26686/wgtn.17131868 |
_version_ |
1780741427828883456 |