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Global Spatial and Temporal Variation of Cd:P in Euphotic Zone Particulates

机译：CD的全局空间和时间变异：P在Euphotic区颗粒中的P.

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Abstract >Concentrations of Cd and P were determined in particle samples collected using the multiple unit large volume in situ filtration system (MULVFS) from 50 profiles at 34 different locations throughout the Atlantic, Pacific, and Southern Oceans since 1991. Consistent methodology has been used. This data set of Cd:P in size fractionated particles gives insight into the processes that lead to differences in regional Cd:P particle values as well as how the formation and remineralization of these particles lead to dissolved deep water ratios that increase from the North Atlantic to the North Pacific. With large spatial and temporal variation, this data set allows us to study the effects of an El Ni?o, upwelling, large‐scale in situ Fe fertilization, low‐oxygen conditions, and seasonal variation on the Cd:P in particles. Overall, Cd:P tends to be higher (~1–2?mmol/mol) in particles gathered in biologically dynamic waters and is much lower (typically ~0.1?mmol/mol) in oligotrophic regions. Using multiple linear regression analysis, we investigate how euphotic zone parameters important to photosynthesis including nitrate, phosphate, silicate, temperature, and euphotic zone depth affect the Cd:P ratio in particles. Using the results of the analysis, we create global seasonal maps of predicted particulate Cd:P distributions. We find that three factors—local dissolved nitrate, silicate concentrations, and euphotic zone depth—can predict 59% of the variation in particulate Cd:P. We verified our projections using in situ filtration samples collected during GEOTRACES expeditions GA03 (North Atlantic) and GP16 (South Pacific). </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract Type =“Main”XML：Lang =“en”> <标题类型=“main”>抽象</ title> >在使用多个单元的原位收集的粒子样本中测定CD和P的浓度自1991年以来，从整个大西洋，太平洋和南部海洋的34个不同地点的50个曲线的过滤系统（Mulvfs）。已经使用了一致的方法。该数据组CD：P尺寸分级颗粒介绍了导致区域CD：P粒子值差异的过程的洞察力以及这些颗粒的形成和再矿化如何导致溶解的深水比率从北大西洋增加到北太平洋。随着空间和时间变化的大量变化，这种数据集允许我们研究EL NIα的效果，升上的升高，大规模的原位施肥，低氧气条件和CD颗粒中的季节性变化。总体而言，CD：P在生物动态水域聚集的颗粒中倾向于更高（〜1-2？mmol / mol），并且在寡噬细胞区域中的颗粒较低（通常为0.1×mmol / mol）。使用多元线性回归分析，我们研究了Euphotic区参数对光合作用的重要性如何对包括硝酸盐，磷酸盐，硅酸盐，温度和Euphy区深度的光合作用影响CD：P比在颗粒中的CD：P比。使用分析结果，我们创建了预测微粒CD：P分布的全局季节性地图。我们发现三个因素 - 局部溶解的硝酸盐，硅酸盐浓度和Euphotic区深度可以预测颗粒CD中的59％的变化：p。我们通过在地理条目探险GA03（北大西洋）和GP16（南太平洋）收集的原位过滤样品中使用原位过滤样品进行了验证。</ p> </ abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-23728/'>《Global Biogeochemical Cycles》</a> <b style="margin: 0 2px;">|</b><span>2018年第7期</span><b style="margin: 0 2px;">|</b><span>共19页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bourne H. L.&option=202" target="_blank" rel="nofollow">Bourne H. L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bishop J. K. B.&option=202" target="_blank" rel="nofollow">Bishop J. K. B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lam P. J.&option=202" target="_blank" rel="nofollow">Lam P. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ohnemus D. C.&option=202" target="_blank" rel="nofollow">Ohnemus D. C.;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Department of Earth and Planetary ScienceUniversity of CaliforniaBerkeley CA USA;</p> <p>Department of Earth and Planetary ScienceUniversity of CaliforniaBerkeley CA USA;</p> <p>Ocean Sciences DepartmentUniversity of CaliforniaBerkeley CA USA;</p> <p>Bigelow Laboratory for Ocean SciencesEast Boothbay ME USA;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/165.html" title="地质学">地质学;</a><a href="https://www.zhangqiaokeyan.com/clc/5109.html" title="生物地球化学、气体地球化学">生物地球化学、气体地球化学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=cadmium in marine particles&option=203" rel="nofollow">cadmium in marine particles;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=particle Cd:P variation in modern surface waters&option=203" rel="nofollow">particle Cd:P variation in modern surface waters;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=remineralization differences between Cd and P&option=203" rel="nofollow">remineralization differences between Cd and P;</a> </p> <div class="translation"> 机译：海洋颗粒中的镉;粒子CD：现代表面水域的P变异;CD和P之间的再矿化差异; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023423962.html">Global Spatial and Temporal Variation of Cd:P in Euphotic Zone Particulates</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bourne H. 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