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克隆得到了合浦珠母贝(Pinctada fucata)PF-CREB3L2蛋白的c DNA序列,其c DNA全长1 983 bp,其中开放阅读框长度为1 728 bp,编码的蛋白含有575个氨基酸残基。组织表达分布实验发现,其在合浦珠母贝内脏囊中表达量最高,在外套膜和鳃中也有大量表达,推测其广泛参与合浦珠母贝的贝壳形成等生理活动。贝壳损伤修复实验中发现,在合浦珠母贝贝壳受到损伤后,PF-CREB3L2和基质蛋白的表达量会迅速上升,且PF-CREB3L2的峰值出现更早,推测其通过影响基质蛋白转录,参与合浦珠母贝生物矿化的调控过程。PF-CREB3L2与合浦珠母贝基质蛋白表达相关性的分析发现,PF-CREB3L2与Prisilkin39、KRMP的表达量呈现显著的正相关,说明其可能特异性地调控某些基质蛋白的转录。 相似文献
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三倍体和二倍体合浦珠母贝育珠比较初步研究 总被引：2，自引：0，他引：2
利用人工诱导培育的三倍体合浦珠母贝Pinctada martensii(D.)进行插核育珠试验,并同处理组内的二倍体同胞进行比较。结果表明:三倍体合浦珠母贝的留核率和正圆珠比率分别为81.0％和58.8％,而二倍体则为71.3％和37.8％;在非正圆珠中两者的污珠率差别不大,但三倍体的尾巴珠和素珠的比率明显低于二倍体;三倍体的正圆珠珍珠层平均厚度和平均重量分别为381μm和163mg,二倍体分别为265μm和105mg,两者差异极显著(P<0.01)。初步表明,利用三倍体合浦珠母贝培育珍珠,能缩短育珠期,提高珍珠的产量和质量。 相似文献
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国内外贝类学界都认为贝壳角质层仅由贝壳素构成.棱柱层由方解石构成.珍珠层通常为霰石构成.日本的小林新二郎提出棱柱珍珠是方解石结构,国内外许多论文对此都没有提出异议.本研究采用X-射线对贝壳和棱柱珍珠衍射结果证明:(1)贝壳珍珠层全是是霰石结构,只有牡蛎(Ostrea rivularis)壳例外,符合以上理论;(2)棱柱层几乎全是霰石结构,只有牡蛎壳和紫色裂江珧(Pinna atropurpurea)壳的棱柱层是方解石结构,基本否定了以上理论;(3)角质层由有机物—贝壳素和方解石或霰石组成的,有些还含二氧化硅等杂质,这不完全相符上面理论;(4)棱柱珍珠完全是霰石结构,证明小林新二郎的结论是错误的. 相似文献
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分别用地塞米松(Dexamethasone,DEX)和过氧化氢(H2O2)处理合浦珠母贝(Pinctada fucata),研究其对贝珍珠层和基质蛋白表达的影响。扫描电镜观察显示,DEX可促进珍珠层生长,H2O2则抑制珍珠层生长。体外碳酸钙结晶实验表明,DEX处理组间液蛋白调控文石生成的趋势加强,并加速碳酸钙结晶速率;H2O2处理组相反。实时定量PCR实验显示,DEX处理组TGFβ和NF-кB信号通路关键因子pf-smad3、pf-rel等和基质蛋白Nacrein等基因表达水平明显降低,H2O2作用组则显著上升。由上述结果推测,DEX和H2O2可通过抑制或激活合浦珠母贝的TGFβ和NF-кB信号通路,从而调控与珍珠层形成相关的基质蛋白的表达,并影响珍珠层的结构;同时暗示贝的免疫体系和矿化系统可能存在协同作用,该作用机制具有生物进化学意义,并对养殖珍珠的培育具有借鉴作用。 相似文献
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马氏珠母贝微卫星快速分离及遗传多样性分析 总被引：8，自引：0，他引：8
马氏珠母贝(Pinctada martensii Dunker)又称合浦珠母贝,是世界上用于生产海水珍珠的最主要贝类之一.自60年代我国成功地开展马氏珠母贝的人工育苗以来,海水珍珠养殖业发展迅速,至20世纪90年代,海水珍珠养殖已成为广东、广西和海南沿海部分地区的支柱产业,海水珍珠成为出口创汇的重要产品.海水珍珠产业的发展仅靠采捕天然野生的亲贝已不能满足生产的需要,越来越多地用人工养殖的亲贝进行人工繁殖.而采用少数亲贝(尤其是养殖亲贝)的育苗导致近亲繁殖,使马氏珠母贝种质资源出现了退化,在海水珍珠养殖上产生的直接后果是珍珠的质量和产量(单产)明显下降. 相似文献
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合浦珠母贝基质蛋白KRMP-3对二价金属离子选择性的研究 总被引：1，自引：0，他引：1
用大肠杆菌表达含有GST标签的基质蛋白KRMP-3。利用圆二色谱(Circular Dichroism, CD)研究不同浓度钙离子和镁离子对基质蛋白 KRMP-3二级结构的影响。结果表明,钙离子对其二级结构的变化远大于镁离子;同时,采用荧光淬灭法研究 KRMP-3对钙,镁,锶,钡等二价金属离子的选择性,结果表明, KRMP-3对钙离子有特异性选择性,钙离子与KRMP-3的结合常数K约为103 L/mol,结合位点数 n 近似为1,表明 KRMP-3与钙离子的结合能力适中,推测基质蛋白 KRMP-3对合浦珠母贝( Pinctada fucata)棱柱层形成起到促进作用。 相似文献
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Three colonies of the erect, robust branching, cheilostome bryozoan Adeonellopsis sp. were collected from Doubtful Sound, New Zealand, to investigate within‐colony variation in carbonate mineralogy. One‐hundred‐and‐twenty‐one sections from 9 branches were found to contain mostly aragonite, with calcite ranging from 1.1 to 7.3 wt% (mean ± SD = 2.4 ± 1.2 wt%, n = 120). The magnesium (Mg) content in calcite ranged from 5.3 to 13.1 wt% magnesium carbonate (8.8 ± 1.0 wt% MgCO3; n = 120). Calcite content decreased with increasing age proximally along the branch, indicating that secondary thickening is achieved with aragonite. In contrast, an oscillating trend in Mg content along branches suggests that seasonal or interannual environmental parameters may influence this geochemical parameter. Mineralogical variability highlights the need for multiple samples from the same colony to be measured when determining quantitative carbonate mineralogy in bryozoans. Bimineralic bryozoans such as Adeonellopsis sp. may have lower preservation potential than monomineralic bryozoans, and consequently may not survive diagenesis to become fossils. Bimineralic species may also be more vulnerable to dissolution pressure and possible ocean acidification than monomineralic calcitic taxa. 相似文献
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闭壳肌的疤痕部位（AMS）是闭壳肌和壳的固定点。它是一个重要的有机-无机界面和应力分布面。尽管有一些近期的研究进展,我们对AMS组成和结构的了解仍然是有限的。这里,我们研究比较了三种双壳类动物：厚壳贻贝、栉孔扇贝、菲律宾蛤仔的AMS。结果表明这三种动物的AMS明显不同。厚壳贻贝和栉孔扇贝在AMS的壳结构珍珠片层上部有一柱状层,该层在厚壳贻贝中的结构更有规律。菲律宾蛤仔缺乏此柱状层。原子力显微镜结果显示在三种软体动物中AMS的结构比珍珠层结构更光滑。傅立叶变换红外分析结果显示珍珠层和AMS层组成成分略有不同。聚丙烯酰胺凝胶电泳蛋白分离结果显示在厚壳贻贝界面柱状层存在一种约70 kDa的蛋白。对这种蛋白的进一步分析显示其还有较高摩尔比的Asx（Asp+Asn）,Glx（Glu+Gln）和Gly。AMS的特殊结构和组成对其稳定性、粘性以及在该应力分散部位的功能有重要作用。 相似文献
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用紫色蚌和非紫色蚌制取细胞小片,分别插入紫色蚌和非紫色蚌外套膜内,探究三角帆蚌(Hyriopsis cumingii)无核珍珠颜色与制片蚌、育珠蚌的关系;用不同类型制片蚌的不同部位制取细胞小片,分别插入育珠蚌外套膜内,进一步探究珍珠颜色与制片蚌珍珠质颜色的关系。结果表明,以紫色蚌为制片蚌,所产的珍珠为紫色系,珍珠紫色深浅与细胞小片所对应部位的制片蚌珍珠质紫色深浅呈正相关。以非紫色蚌为制片蚌,所产的珍珠有白色系和黄色系,珍珠黄色深浅与细胞小片所对应部位的制片蚌珍珠质黄色深浅呈正相关。三角帆蚌外套膜无核珍珠颜色是由提供细胞小片的制片蚌珍珠质颜色所决定,而与育珠蚌无关。该结论支持珍珠囊表皮细胞来自于移植细胞小片的观点。该结果表明,通过定向选育纯紫、纯白色贝壳珍珠质三角帆蚌新品系,即可培育出纯紫、纯白色无核珍珠。 相似文献
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激素敏感性脂肪酶（hormone sensitive lipase，HSL）和乙酰辅酶A羧化酶（acetyl-CoA carboxylase，ACC）是脂代谢的关键酶，肌肉和肝脏是鱼类脂代谢的主要场所。为研究饥饿过程中这两种酶的作用，本实验采用实时荧光定量PCR技术以及ELISA技术检测了在35 d饥饿过程中这两种酶在大黄鱼肌肉和肝组织中mRNA表达水平和酶活性的变化。结果显示，饥饿胁迫显著降低大黄鱼肌肉和肝组织中脂肪含量，以及脂肪合成关键酶ACC mRNA表达水平（P<0.05）；显著提高脂肪分解关键酶HSL mRNA表达水平（P<0.05）。饥饿胁迫对肌肉和肝组织中HSL和ACC酶活性均有显著影响（P<0.05），肌肉和肝组织HSL （相关系数r分别为0.598 2和0.539 6）以及肌肉组织ACC酶活性（r=0.677 7）与对应mRNA表达水平呈中度正相关（0.5 < r < 0.8），但ACC酶活性在肝组织与其对应的mRNA表达量呈负相关（r=-0.374 0），提示饥饿胁迫对大黄鱼HSL和ACC的表达存在翻译前和翻译后两种水平的调控。本研究结果可为研究饥饿胁迫对大黄鱼脂类代谢分子层面的影响机制提供依据。 相似文献
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The responses of atmospheric pCO2 and sediment calcite content to changes in the export rain ratio of calcium carbonate to organic carbon are examined using
a diffusion-advection ocean biogeochemical model coupled to a one-dimensional sediment geochemistry model. Our model shows
that a 25% reduction in rain ratio decreases atmospheric pCO2 by 59 ppm. This is caused by alkalinity redistribution by a weakened carbonate pump and an alkalinity increase in the whole
ocean via carbonate compensation with decreasing calcite burial. The steady state responses of sedimentary calcite content
and calcite preservation efficiency are rather insensitive to the deepening of the saturation horizon of 1.9 km. This insensitivity
is a result of the reduced deposition flux that decreases calcite burial, counteracting the saturation horizon deepening that
increases calcite burial. However, in the first 10,000 years the effect of reduced calcite deposition on the burial change
is more prominent; while after 10,000 years, the effect of saturation horizon deepening is more dominant. The lowering of
sediment calcite content for the first 10,000 years is effectively decoupled from the 1.9 km downward shift of the saturation
horizon. Our results are in part a consequence of the more dominant role that respiration CO2 plays in sediment calcite dissolution over bottom water chemistry in our control run and support the decoupling of calcite
lysocline depth and saturation horizon shifts, as suggested originally by Archer and Maier-Reimer (1994) and Archer et al. (2000). 相似文献
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R. Yu. Tarakanov 《Oceanology》2012,52(2):157-170
It is shown on the basis of the data of the Russian Academy of Sciences expeditions in 2003–2010, the historical CTD database,
the WOCE climatology, and the satellite altimetry that the area of the Scotia Sea and the Drake Passage is even a greater
significant orographic barrier for the eastward Antarctic Circumpolar Current (ACC) than was previously thought. It is the
current concept that this barrier is the most important for the ACC; it consists of three obstacles: the Hero Ridge with the
Phoenix Rift, the Shackleton Ridge, and the North Scotia Ridge with the relatively shallow eastern part of the Scotia Sea.
Despite the fact that all three obstacles are permeable for the layer of the Circumpolar Bottom Water (CBW; 28.16 < γ
n
< 28.26) being considered the lower part of the circumpolar water, the circulation in this layer throughout the Scotia Sea
and the Drake Passage quite substantially differs from the transfer by the surface-intensified ACC jets. Herewith, the upper
CBW boundary is the lower limit of the circumpolar coverage of the ACC jets. This result is confirmed by the near zero estimate
of the total CBW transport according to the three series of the LADCP measurements on the sections across the Drake Passage.
It is shown that the transformation (cooling and freshening) of the CBW layer, which occurs owing to the flow of the ACC over
the Shackleton Ridge, is associated with the shape and location of the ridge in the Drake Passage. The high southern part
of this ridge is a partially permeable screen for the eastward CBW transport behind which the colder and fresher waters of
the Weddell Sea and the Bransfield Strait of the same density range as the CBW penetrate into the ACC zone. The partial permeability
of the Shackleton Ridge for the CBW layer leads to the salinization of this layer on the eastern side of the ridge and to
the CBW’s freshening on the western side of this ridge, which is observed across the entire Drake Passage. 相似文献
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R. W. Gauldie 《新西兰海洋与淡水研究杂志》2013,47(2):267-274
Heating otoliths of the orange roughy (Hoplostethus atlanticus; Trachichthyidae) by the break‐and‐burn method causes a crystal transformation from aragonite to calcite. However, the change does not affect the legibility of the check rings. Orange roughy otolith check rings fall into two classes: a diffuse deposit (that is not visible in the break‐and‐burn method, but may have an annual periodicity) and structural check rings (which appear as fine lines on the surface, but as dark bands in the body of the otolith). Structural check ring deposition is irregular, but fortuitous aggregations of structural check rings might be mistaken for conventional annual check rings. 相似文献
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Akio Ishida 《Journal of Oceanography》1994,50(3):295-316
The transport and vertical structure of the Antarctic Circumpolar Current (ACC) are examined, especially the component of the current driven by buoyancy, by using a three-layer model. We investigate the effects of the South American peninsula, the island arc to the east, and the Macquarie ridge, which are modeled as partial meridional barriers overlapping meridionally each other. We found that the buoyancy-driven component is given as a function of the transport out of the Weddell Sea (S
W
) and the sum of the transports into the North Atlantic (S
A
) and the North Pacific (S
P
) out of the Southern Ocean. The buoyancy-driven current flows westward, ifS
W
andS
A
+S
P
are positive. The transport depends on the value ofS
W
more thanS
A
+S
P
by one order of magnitude within a realistic range of parameters. The most predominant term in the transport equation is inversely proportional to the difference between the Coriolis parameters at the tips of the partial meridional barriers. Thus, the magnitude of the transport strongly depends on the overlapping length of the meridional barriers. The eastward current of the ACC is driven by the predominant eastward wind stress in the Southern Ocean, although a part of the wind-driven component is canceled by the westward buoyancy-driven component. The vertical structure of the ACC is found to be attributed to the surface wind-driven circulation and the deep and bottom buoyancy-driven circulation. 相似文献