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iron manganese bioturbation
Regional patterns of bioturbation and iron and manganese
2013.10.1 Benthos Iron oxide reduction Bioturbation 1. Introduction The shelf region of the Bering Sea is productive, with iron (Fe)-replete surface waters, whereas the off
Charlar en LíneaIntegrated effects of bioturbation, warming and sea-level rise on ...
2023.4.15 Mangroves play a key role in maintaining and protecting (sub)tropical marine biodiversity and crucial ecosystem services, including regulating key global
Charlar en LíneaRegional patterns of bioturbation and iron and manganese
2013.10.1 Regional patterns of iron (Fe) and manganese (Mn) reduction rates across the shelf and slope of the southeastern Bering Sea, as well as the relative
Charlar en LíneaBiological rejuvenation of iron oxides in bioturbated
2018.1.17 Zetaproteobacteria were estimated to be a global total of 10 26 cells in coastal, bioturbated sediments, and predicted to annually produce 8 × 10 15 g of Fe in
Charlar en LíneaMillennial scale persistence of organic carbon bound to
2021.1.12 Iron and manganese (oxyhydroxide) reduction play an important role in organic matter degradation in this region 28,29 and it is therefore a suitable location to
Charlar en Línea(PDF) Bioturbation and Manganese Cycling in Hemipelagic
1990.6.19 PDF The activities of infaunal macrobenthos have major influences on the types, rates and distributions of diagenetic reactions involving manganese in... Find,
Charlar en LíneaBioturbation and the δ56Fe signature of dissolved iron
2023.1.25 1. Introduction Iron plays a central role in marine biogeochemical cycles. Over the last 100 000 years, iron has been a limiting micronutrient for marine primary productivity in large parts of the ocean
Charlar en LíneaRegional patterns of bioturbation and iron and manganese
2013.10.1 Esch et al. (2013) investigated broader questions of carbon remineralization in sediments, in particular the role of iron and manganese reduction in
Charlar en LíneaIron and manganese cycling in different sedimentary
1997.8.1 The quality and quantity of the organic matter deposited in each sedimentary environment are shown to determine whether sediments become sufficiently
Charlar en LíneaBioturbation and manganese cycling in hemipelagic
1990.6.19 In some non-sulphidic hemipelagic deposits of the eastern equatorial Pacific (Panama Basin) biogenic reworking drives internal cycles of manganese, which
Charlar en Línea