海洋生物地球化学

天然放射性核素~（32）P和~（33）P在海洋生物地球化学中的示踪研究概况

A review of natural radionuclides ~ ( 32 ) p and ~ ( 33 ) p tracer studies for the biogeochemistry in the ocean

海洋生物地球化学与生态系统分析（OCEANS）&一个酝酿中的国际科学计划

Ocean Biogeochemistry and Ecosystem Analysis & A New Planning International Academic Program

海洋生物地球化学过程对Ca和Sr的地球化学特征有重要影响。

Also , the processes of marine geochemistry play an important role in the characteristics of Ca and Sr in the study area .

比较系统地介绍了国内外Al的海洋生物地球化学研究进展，内容包括Al在海洋中的来源及输送通量、不同海区的分布特点、水体中的溶解态Al的赋存形式及其迁移转化规律等。

The manuscript focused on the progresses of marine biogeochemistry study on aluminum at home and abroad , including the main study fields of aluminum , such as its source and transport flux , distribution , dissolved speciation in the water and transformation .

氯甲烷的海洋生物地球化学研究

Studying on Marine Biogeochemistry of Methyl Chloride

中国海洋生物地球化学过程研究的最新进展

Progress of marine biogeochemical processes in China

综述了1998年以来中国海洋生物地球化学研究的主要进展。

The advances in marine biogeochemistry studies in China since 1998 are reviewed in this paper .

海洋生物地球化学的产生与发展

Origination and Evolution of Marine Biogeochemistry

它有着特殊的物理-化学-生物性质，对海洋生物地球化学循环、物质的海-气界面通量、乃至气候等等都有着直接而重要的影响。

Because of its unique physical , chemical and biological properties , the SML have an important and direct effect on biogeochemical cycles in ocean , material fluxes in sea-air interface and global climates .

主要阐述了海洋碳循环生物地球化学过程研究的主要进展，包括海气界面CO2通量过程、溶解&颗粒碳的海洋转化过程、生物固碳与生物泵过程以及河口碳的生物地球化学过程。

This paper reviewed the progress in biogeochemistry processes of marine carbon cycle which include process of CO 2 fluxes across air-sea interface , process of dissolved-particle carbon transforming , biochemistry process of carbon cycle in estuary and function of biological pump .

中国海洋碳循环生物地球化学过程研究的主要进展（1998-2002）

Advances in Biogeochemical Process Research on Marine Carbon Cycles in China ( 1998-2002 )

这种构造发育的时间限制说明了臼齿的形成与海洋环境的生物地球化学演化具有潜在联系。

The temporal restriction of this fabric suggests a potential link between MT formation and the biogeochemical evolution of marine environments .

海洋溶解有机物质（DOM）在海洋碳的生物地球化学循环中占有重要地位。

Dissolved organic matter ( DOM ) in the ocean is the fundamental part of marine carbon biogeochemical cycles .

溶解氧是海洋生命活动不可缺少的物质，同时也是研究海洋生物地球化学循环的一个重要参数。

Dissolved oxygen ( DO ) is not only the indispensable substance of maintaining the metabolism of marine lives , but also an important parameter in the investigation of marine biogeochemistry cycles .

活性磷是海洋浮游植物生长所必需的物质基础，在磷的海洋生物地球化学过程中扮演着重要角色。

Orthophosphate is an essential nutrient element for phytoplankton in ocean environment , and plays an important role in the marine biogeochemical cycle of phosphorus .