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| 1 | 中太平洋地区两个铁锰结壳的生长幕研究显示文摘通过对3块中太平洋铁锰结壳样品进行的生物地层学及其结构构造、元素地球化学剖面的综合研究发现,铁锰结壳的生长主要集中于两个形成环境存在差异分别由不同因素控制的形成阶段,一个是约25Ma以来其形成环境氧化程度由南极底层流(AABW)控制的对应于结壳新壳层的生长幕,另一个是渐新世之前其形成环境氧化程度由环赤道表中层洋流和高密度温盐表层水下沉控制的对应于结壳老壳层的生长幕,而在早、中渐新世处于两种环境的转换期,也正好是海退期、大洋低生产力期、低CCD和生物碳酸盐低产率期,形成结壳生长的主要生长间断。该研究成果对于进一步了解太平洋的古海洋、古环境演变有一定意义。 | 武光海 周怀阳 张海生 Irine PULYAEVA 凌洪飞 刘捷红 | 2006 | 地质学报2006，80，4： | 8 |
| 2 | Calcareous Nannofossils and Molecular Fossils in Cobalt-rich Crusts and their Response to the P/E Global Event显示文摘A biostratigraphic study on calcareous nannofossils from the CM3D06 Co-rich ferromanganese crust from the Magellan seamounts in the northwestern Pacific enabled estimation of depositional age.The bio-imprinting of calcareous nannofossils and other fossil species suggests six age ranges for the nannofossils: late Cretaceous,late Paleocene,(early,middle,late) Eocene,middle Miocene,late Pliocene,and Pleistocene.Gas chromatography(GC) and gas chromatography-mass spectrometry(GC-MS) were used to test the Co-rich crusts,and a variety of molecular fossils were detected,such as chloroform bituminous 'A',n-alkane,isoprenoid and sterol.Peak carbon and molecular indices(such as ΣC23 /ΣC24 +,CPI,Pr/Ph,Pr/nC17,Ph/nC18 and δ13C) indicate that the parent organic matter is dominated by marine phytoplankton and thallogen whereas there is little input of terrestrial organic matter.Researches on calcareous nannofossils,molecular fossils and molecular organic geochemistry data reveal that the Paleocene/Eocene(P/E) global event is recorded in the cobaltrich crusts from the northwestern Pacific Ocean.A succession of biomes can be observed near the 85 mm boundary(about 55 Ma),i.e.,the disappearance of the late Cretaceous Watznaueria barnesae and Zigodicus spiralis,and Broisonia parka microbiotas above the P/E boundary,and the bloom of Coccolithus formosus,Discoaster multiradiatus,Discoaster mohleri and Discoaster sp.below the boundary.Typical parameters of molecular fossils,such as saturated hydrocarbon components and carbon-number maxima,Pr/Ph,Pr/C17,Ph/C18,distribution types of sterols,Ts/Tm ratios and bacterial hopane,also exhibit dramatic changes near the P/E boundary.These integrated results illustrate that the biome succession of calcareous nannofossils,relative content of molecular fossils and molecular indices in the cobalt-rich crusts near the 85 mm boundary faithfully record the P/E global event. | ZHANG Haisheng ZHAO Jun HAN Zhengbing LU Bing WU Guanghai PULYAEVA I.A. | 2013 | Acta Geologica Sinica(English Edition)2013，87，5： | 6 |
| 3 | 中太平洋海山铁锰结壳生物地层学研究显示文摘用生物地层学方法对位于中太平洋同一座海山上的2块铁锰结壳样品进行了生物地层学详细研究,发现2块样品的生长层位对应,生物组合也相同。经鉴定,2块结壳的主要生长期都是晚古新世、中始新世至晚始新世、中中新世至上新世、上新世至更新世,2个主要的结壳生长间断分别在渐新世和早始新世。 | 武光海 PULYAEVA I A 刘捷红 李雪富 | 2011 | 海洋学报2011，33，4： | 3 |
| 4 | Biomineralization of organic matter in cobalt-rich crusts from the Marcus–Wake Seamounts of the western Pacific Ocean显示文摘Organic matter in cobalt-rich crust(CRC) from the Marcus–Wake Seamounts of the western Pacific Ocean, Sample CM1D03, has been analyzed to understand the source, geochemistry and mineralization of organic matter, and the mineralization environment. Biomarkers, including n-alkanes, isoprenoids, terpanes and sterols, have been detected in various layers of the CRC sample, using gas chromatography(GC) and gas chromatography–mass spectrometry(GC–MS). The content of organic carbon(OC) and its stable isotope(δ13C), and the combined features of the biomarkers show that the mineralized organic matter in CM1D03 CRC was mainly derived from microorganisms and lower plankton(e.g., bacteria and algae, respectively) from marine surface water, with some terrestrial higher plant components. The ratio of chloroform bitumen 'A': OC was high in the CRC, between 10.51 and 20.66, showing significant migration characteristics of n-alkanes. Four mineralization categories of organic matter were recognized based on GC chromatograms of n-alkane molecules:(1) primitive type(bacteria and algae), which is characterized by moderately mature of n-alkanes preserving the original characteristics of the organic matter from microorganisms and lower plankton;(2) microbial degradation type, which is characterized by low contents of n-alkanes and rising baseline in the chromatogram, with the 'bulge' being the products of organic matter by biodegradation;(3) organic matter migration type, which is characterized by low carbon number of n-alkanes with n C18 as the main peak carbon, without odd even predominance, and low concentrations of isoprenoids and hydrocarbons with high carbon number; and(4) organic matter hydrothermal type, which is characterized by relatively low concentration of small molecular weight n-alkanes, pristane, and phytane, accompanied by higher concentration of n-alkanes with carbon number greater than n C18. This study shows that biomarkers can record controlling factors of mineralization and their variation. | ZHAO Jun ZHANG Haisheng WU Guanghai LU Bing PULYAEVA Irina A ZHANG Haifeng PANG Xuehui | 2014 | Acta Oceanologica Sinica2014，33，12： | 3 |
| 5 | 西太平洋富钴结壳中钙质超微化石和分子化石研究显示文摘本文对西太平洋麦哲伦海山CM3D06富钴结壳进行了钙质超微化石生物地层学研究,发现结壳中有代表白垩纪(晚期)、古新世(晚期)、始新世(早、中、晚期)、中新世(中期)、上新世(晚期)和更新世等各时代的标准钙质超微化石,表明结壳的形成始于白垩纪(晚期);在富钴结壳中检出正构烷烃、类异戊二烯烃、甾烷类等众多分子化石,分子化石组合特征指数、主峰碳、ΣC-23/C+24、CPI、Pr/Ph、Pr/nC17、Ph/nC18和nC31/nC17显示有机质生物母源主要为海洋浮游植物、浮游动物和底栖非光合作用的菌类,而甾烷类的C29、C28和C27含量分布的变化则说明生物种群具有快速演变的特征。此外,还探讨了CM3D06结壳中Pr/Ph和有机碳同位素组成变化与结壳生长过程中的海洋环境演化的关联程度。 | 陈荣华 赵庆英 张海生 卢冰 Pulyaeva I A | 2015 | 海洋学报2015，37，7： | 2 |
| 6 | 西太平洋海山富钴结壳分子化石和超微化石记录:年代划分和古生态环境演变显示文摘分析了西太平洋海山CM1D03富钴结壳中超微化石生物地层学记录,结合钙质微浮游生物印痕,对结壳进行了地质年代的划分,其年代为晚古新世—早始新世(54~51Ma)、中始新世(45~40Ma)、中新世—上新世(22~2.4Ma)、上新世—更新世(3.6~1.2Ma)。利用气相色谱、气相色谱-质谱联用检测了结壳中的正构烷烃、类异戊二烯、甾烷等分子化石,探讨结壳生长过程中的生源构成、沉积环境以及古生态演替特征。结果表明,结壳中氯仿沥青'A'/有机碳(TOC)比值为10.51%~21.74%,具有明显的烃类运移特征。正构烷烃的轻/重烃比值(ΣC-23/ΣC+24)为0.74~1.47,碳优势指数(CPI)为0.80~1.45,碳稳定同位素(δ13 C)为-24.00‰^-25.48‰,指示有机质主要来源于海洋表层水体的浮游植物。研究还表明,有机质物源,C27、C28、C29甾烷的丰度变化,TOC保存及δ13 C等均与结壳生长所处海洋环境、全球气候和南极底流的结构变化有关。 | 赵军 张海生 于培松 武光海 卢冰 Pulyaeva I A | 2014 | 海洋地质与第四纪地质2014，34，2： | 2 |
| 7 | 西太平洋海山富钴结壳钙质超微化石变化与E/O界限的地质记录显示文摘选择马尔库斯-威克海山区和麦哲伦海山区的2块壳结纹层记录,进行生物地层学的精细研究,并利用钙质超微化石的生物印痕分出时代:马尔库斯-威克海山CM1D03年代为晚古新世到更新世,而麦哲伦海山CM3D06结壳年代则更久远些——白垩纪晚期(约大于70.0 Ma),这表明不同海山的富钴结壳最初形成年代和富集特征具有显著的时空差异性,而不同海山结壳层内部的古微体化石组合面貌、分布特征上的差别表明有关属种对大洋不同环境的适应性差异所致.本文还利用结壳纹层中所保存的钙质超微化石种群数进行生态学研究,寻找钙质超微化石变化与古新世末至渐新世初(E/O)界限地质事件的联系,研究发现在E/O界线之交(对应CM1D03结壳的25 mm和CM3D06结壳的58mm附近)生物群落发生明显演替和重组,这些生物群落在E/O界限上下的改变所形成独特的生态结构,无疑反映了西太平洋古生物群落对全球冷事件存在明显响应,也说明结壳生长过程与全球气候变化有着紧密联系. | 张海生 胡佶 赵军 韩正兵 于培松 武光海 雷吉江 卢冰 PULYAEVA Irina A | 2015 | 中国科学:地球科学2015，45，4： | 2 |
| 8 | SPARC/ osteonectin induces matrix metalloproteinase activation in human breast cancer cell lines显示文摘 | Gilles C Bassuk JA Pulyaeva H | 1998 | Cancer Res1998，58，23： | 1 |
| 9 | SPARC/osteonectin induces matrix metalloproteinase2activation in human breast cancer cell lines显示文摘 | GILLES C BASSUK J A PULYAEVA H | 1998 | Cancer Res1998，58，： | 1 |
| 10 | Thompson,SPARC/osteonectin induces matrix metalloproteinase 2 activation in human breast cancer cell lines显示文摘 | Gilles C Bassuk J A Pulyaeva H | 1998 | Cancer Res1998，58，11： | 1 |
| 11 | Membrane fusion mediated by baculovirus GP64 involves assembly of stable GP64 trimers into multiprotein aggregates显示文摘 | Pulyaeva H Sokoloff A | 1998 | J Cell Biol1998，143，： | 1 |
| 12 | SPARC/osteonectin induces matrix metalloproteinase 2 activation in human breast cancer cell lines显示文摘 | Gilles C Bassuk JA Pulyaeva H | 1998 | Cancer Res1998，58，23： | 1 |
| 13 | SPARC/osteonectin induces matrix metalloproteinase 2 activation in human breast cancer cell lines显示文摘 | Gilles C Bassuk JA Pulyaeva H | 1998 | Cancer Res1998，58，： | 1 |
| 14 | Fe-Mn and mineralization on the IOAN Guyot,Western Pacific: results of a detailed survey显示文摘 | Melnikov M L Shkolnik E L Pulyaeva I A | 1996 | Geol of Pac Ocean1996，12，： | 1 |
| 15 | SPARC/osteonectin induces matrix metalloproteinase 2 activation in human breast cancer cell lines显示文摘 | Gilles C Bassuk JA Pulyaeva H | 1998 | Cancer Res1998，58，23： | 1 |
| 16 | SPARC/osteonectin induces matrix metalloproteinase 2 activation in human breast cancer cell lines显示文摘 | Gilles C Bassuk JA Pulyaeva H | 1998 | Cancer Res1998，58，23： | 1 |
| 17 | Variations of calcareous nannofossils of cobalt-rich crusts and geological records at the Eocene-OIigocene transition in western Pacific seamounts显示文摘Two records of the crust laminae from the Marcus-Wake Seamounts and the Magellan Seamount were biostratigraphically studied. Based on biological imprints of the calcareous nannofossils, the geological ages of the two records were determined, with CM1D03 from the Marcus-Wake Seamounts being of late Paleocene to Pleistocene and CM3D06 from the Magellan Seamount of Late Cretaceous(more than 70.0 Ma). There are the obvious temporal-spatial differences in the initial formation period and enrichment characteristics of the cobalt-rich crusts of the two seamount chains and differences in the combination and distribution of microfossils in the inner crust layers between the seamounts. These differences are due to the adaptabilities of oceanic species in different environments. Ecological research was carried out in terms of population size of the calcareous nannofossils preserved in the crustal layers to discern the relation of the geological events at the Eocene-Oligocene(E/O) transition. The results show the transitions and recombination of species in the biotic community during the E/O transition obviously corresponded to 25 mm depth in the CM1D03 crust and 58 mm depth in the CM3D06 crust. The changes in biological species and the formation of particular ecological structures indicate the adaptive response of the paleo-biological community in the western Pacific Ocean to the global cold-climate events and the close correlation between the formation of the crust and the global climate change. | ZHANG HaiSheng HU Ji ZHAO Jun HAN ZhengBing YU PeiSong WU GuangHai LEI Ji Jiang LU Bing Irina A PULYAEVA | 2015 | Science China Earth Sciences2015，58，5： | 1 |
| 18 | SPARC/osteonectin induces matrix metalloproteinase 2 activation in human breast cancer cell lines显示文摘 | Gilles C Bassuk JA Pulyaeva H | 1998 | Cancer Res1998，58，23： | 1 |
| 19 | Membrane fusion mediated by baculovirus gp64 involves assembly of stable gp64 trimers into muhiprotein aggregates 显示文摘 | MARKOVIC I PULYAEVA H SOKOLOFF A | 1998 | J Cell Biol1998，143，5： | 1 |
| 20 | SPARC/osteonectin induces matrix metalloproteinase 2 activation in human breast cancer cell lines显示文摘 | Gilles C Bassuk JA Pulyaeva H | 1998 | Cancer Res1998，58，23： | 1 |
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