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DOI10.1111/gbi.12323
A small marine biosphere in the Proterozoic
Laakso T.A.; Schrag D.P.
发表日期2019
ISSN14724677
起始页码161
结束页码171
卷号17期号:2
英文摘要The riverine supply of the globally limiting nutrient, phosphorus, to the ocean accounts for only a few percent of nutrient supply to photosynthetic organisms in surface waters. Recycling of marine organic matter by heterotrophic organisms provides almost all of the phosphorus that drives net primary production in the modern ocean. In the low-oxygen environments of the Proterozoic, the lack of free oxygen would have limited rates of oxic respiration, slowing the recycling of nutrients and thus limiting global rates of photosynthesis. A series of steady-state mass balance calculations suggest that the rate of net primary production in the ocean was no more than 10% of its modern value during the Proterozoic eon, and possibly less than 1%. The supply of nutrients in such a world would be dominated by river input, rather than recycling within the water column, leading to a small marine biosphere found primarily within estuarine environments. © 2018 John Wiley & Sons Ltd
关键词biosphereestuarine environmentmarine environmentnet primary productionnutrient cyclingnutrient limitationorganic matterprimary productionProterozoicrecyclingsurface waterwater columnoxygenphosphorussea wateraquatic speciesbiotachemistryestuaryphotosynthesisphysiologyriverAquatic OrganismsBiotaEstuariesOxygenPhosphorusPhotosynthesisRiversSeawater
语种英语
来源机构Geobiology
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/133241
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GB/T 7714
Laakso T.A.,Schrag D.P.. A small marine biosphere in the Proterozoic[J]. Geobiology,2019,17(2).
APA Laakso T.A.,&Schrag D.P..(2019).A small marine biosphere in the Proterozoic.,17(2).
MLA Laakso T.A.,et al."A small marine biosphere in the Proterozoic".17.2(2019).
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