tracts-100

动物作文

机器翻译,仅供参考~

(peach blossom tam)。

Below, we will see is "blessing word" on one place important conjoined landscape: "peach blossom changzhutan" and "wine pavilion". I believe you are familiar to the extreme of li bai WangLun "in" peach blossom pool, less than a thousand feet deep WangLun send my feeling "verse. In a peach blossom hometown, "peach blossom tam" symbol romantic, friendship and to the deep happiness. "Wine pavilion" is expressing natural and unrestrained next-best-thing, not drunk endlessly of friendship feeling carrier. Around a peach blossom, can say, this is surrounded in a natural and humanistic perfect blend.。

"Wine pavilion" and "peach blossom changzhutan" is a important part in the blessed path of conjoined twins landscape.。

"Wine" from the tang dynasty meng haoran makes:。

Wine penggui feeling contact, jean song wild xing idle.。

Mo sorrow path, recruit months with blind people.。

Nowadays in the bottom of the bottle will last a few drops of wine, says pot (f) wine.。

"Wine pavilion" is friends, relatives say goodbye place, it is expressed natural and unrestrained next-best-thing, not drunk endlessly of friendship feeling carrier, its carrying the feeling and mood just send WangLun LiBaiZhi matching with identical.。

(to wearers pavilion)。

Peach blossom hometown people's happiness life from peach to start. Scenic spot current planted peach tracts of nearly 5,000 mu, peach varieties nearly 100. Fruit annual gross amounts to 12.5million kilograms, production up to 45 million. The peach massive planting laid the foundation of the development of rural tourism, farmers from which is tasted sweets. In pollutants increasingly affluent today, farmers spiritual life is colorful.。

Previously in the visitor center for leaders mentioned the peach blossom poem village. The whole village of peach blossom native place, the peach blossom poem of life has more than 100 bits farmers poet. They usually besides farming kind of TaoZhi outside, still produce many small poem, every year, in March, peach blossom poem village will organize annual SaiShiHui, villagers would bring new creation short poems, here sing out, they express their for rich life satisfaction.。

Their poems not only included in a peach blossom poems selected peasants in peach blossom poem village, sanpo tenshoho shinan, some still boarded the People's Daily, let the people across the country have can feel happy life of peach blossom hometown.。

Walk on the path to the door of happiness on the road, we should be grateful for a person, that is deng xiaoping. May all the leaders, experts here still wondering why and longquan mountain, deng xiaoping, and peach blossom hometown has relations?。

In 1958, it is spring brilliant march, deng xiaoping came to longquan mountain. In th pointed out: "longquan mountain greening trees less, must promptly, longquan mountain become huaguo mountain". Deng xiaoping "longquan mountain become huaguo mountain" instructions, and the immediate land-saving county leaders at all levels of the recognition and implementation. Especially LongQuanYi danzhou-tunchang in 1959 after chengdu jurisdiction passels of province, city, district officers, employees, and came to the longquan mountain local people, a barren hills, build terraced, transforming, afforestation and plant trees, let the longquan mountain finally turned into "four seasons spent constantly, good fruit section of the famed huaguo mountain.。

Peach blossom hometown to create AAAA of high-quality curriculums to dig deeper into the peach culture, after the end of f word, feel a peach blossom hometown people's happiness, we're about to another swim trails "xi road" - that is, feeling way, arrived in sentiment path, a key scenic "heart-to-heart pavilion".。

谁帮我用英语简单介绍一下仙人掌

It was a fine day today and the sun was bright. I visited Beijing Zoo with my classmate, He Song. The animals were so interesting that all the people loved them. When a bear asked for some food by waving its ann, a visitor threw something to it. At once I went up to him and said without thinking, "Don’t do that. It’s bad for it. If you really love them, take good care of them." His face turned red and answered he wouldn’t do that again. 。

今天是个风和日丽的好天，我和同学贺松去了北京动物园。动物们是那么可爱，大家都非常喜欢它们。一只熊挥动着胳膊向人们要吃的，一个游客就投进去了什么东西。我想都没想就走过去说：“不要那样做。你的做法对它们没好处。如果真的喜欢它们，就应该爱护它们。”他的脸红了，并且回答说他不会再那么做了。

It was very fine today. It was neither too hot nor too cold.He Song and I went to Beijing Zoo in the morning. The animals were so interesting that everyone liked them very much. 。

We watched the bears for a long time. They were really lovely. One of them was standing and opening the mouth. Another of them was sitting on the ground and waving its arm like saying hello to us. The other two guys were boxing. We had a good laugh at it. But at that time I saw a visitor throwing food to them. I ran up to him and stopped him, because some of the animals had been hurt by the food given by visitors. 。

All the animals are our friends. Take good care of them if we really love them. 。

今天天气非常好，既不冷也不热。贺松和我去了北京动物园。动物们是那么可爱，大家都非常喜欢它们。

我们看了很长时间熊，它们太可爱了。其中一只站起采，张着大嘴；另一只正坐在地上挥动着它的胳膊，好像在对我们说你好。那边有两只正在练拳击，这让我们笑了个够。但是，那时我看见一个游客朝那些熊投喂食物，我马上跑过去制止他。因为以前就有一些动物被游客投喂的东西伤害过。

所有的动物都是我们的朋友，如果我们真正喜欢它们，就请好好保护它们。

英语日记

Cactuses

Cactuses are used to living in desert. The whole body of a cactus is green. The stalk is oval and there are thorns all over its body. Actually the thorns in their bodies are their leaves. The leaves are like this only because they can stop the water in their bodies from evaporating into the hot and dry air. The cactuses have long roots and they take their roots deep into the earth so that they can get the water from deeper,soil. Their flowers are always small and white. Although they are ignored in the desert, they never give up coming ont and alwaysdecorate the desert silently.。

仙人掌

仙人掌通常生长在沙漠里。它通身绿色。它的茎是椭圆形的，并且全身长满刺，实际上它们身上的刺是它们的叶子。叶于长成这种形状是为了阻止它们身体内的水分蒸发到热而干的空气里。仙人掌长着长长的根，它们把根深深地扎入地底下以便从更深层的土中吸收水分。

它们一般开小而白的花。尽管它们在沙漠里被忽视，但是它们从不放弃开花并且默默地点缀着沙漠。

日本中部房总半岛Shimosa群中上更新统浅海相沉积旋回和动物群旋回与轨道岁差或倾斜度的对应关系

第一篇：Today is the first day that we start our summer camp. Everybody is amazed at the foreign teacher. They have white skin, yellow hair, blue eyes……But no one is very beautiful or handsome. 。

Foreigners are very tall or fat. I don’t like them. White skin with them is a little ugly. All day around I found that two thirds of the day time I was sleepy. I think tomorrow will be better. 。

第2篇：Today is sunny day, the sunshine is very nice. I am very happy, because I meet some new classmates, chinese teachers and an Englsih teacher. They are really friendly to me. In the morning we go to meeting room to atten the opening ceremony of the summer camp. There are so many people in it. Then I have a test. In fact, I really can’t stand it. In the afternoon, we meet English teacher. He is really tall and thin. He is funny and friendly. The lesson is very interesting. We like him. Then we meet Maria Zhang. She can speak English very well. She teachs them about genesis and sing an English song. They are so great. 。

Ho, I’m free and I’m happy! 。

第三篇：Full of excitement 。

The English summer camp begins today.We were all excited today. 。

When we got on the bus in the morning,our guide miss Guo reminded us to take care of ourseues.She also asked us to introduce ourselves and after that,we got known with each other. 。

How time flies!After only on hour,we got to Zhejiang University.The university is pretty,beautiful and large.The Teaching buildings and student’s building are very new.I couldn’t wait to go into the student’s building.The condition of the flat is good.The air conditioner is prepared for us.The headteacher has a strong mind,no matter how hot it was,he still helped us to solve the problems. 。

In the afternoon,we had our first class.Mrs Zheng asked us 10 questions,and we answered them. 。

After having dinner,my friend and I went to the supermarket to buy some fruit. 。

How happy the day we had today! 。

第四篇：This holiday is my best busy holiday for I am learning English, computer and word and I fall in the weekend exam. Many times I want to take today off, but my mother said to me:“go on, you must belive that you can do it.” So I have to try. Now my English is better than 2months ago. I must thanks my mother, she is good for me. Practices makes perfect. 。

第五篇：How happy I am. Yesterday I finished all the work very quick, so I have a lot of time to do myself. Sometimes finish work early is a good thing, we can have more interests to do the next work. Because of this, I write English dairy eight in the morning. But I wrote it in the evening in the pass day. Everyone, if you can finish the work quickly, not lazy, just try your best. 。

第六篇：Today i took the bus to the park. Some people were waiting for the bus at the bus stop.When a young girl came,she spat a gum on the ground While she was waiting,she herself stepped on the gum.The gum stuck to one of her foot.When the bus came , she got on the bus. Then she discovered the gum stuck her foot all the time. 。

第7篇：Today,I"m going shopping with my mother, We buy some 。

apples bananas and a big watermelon.I"m buying some new books ,because I like reading interesting books very much.Then we get home.I"m very happy! 。

第8篇：Today i went to the museum.I met some robots. I think I am also be able to have a robot in many years.I think they can help me do some dishes .They also can help with my homework.A good robot can make me happy.When i am upset ,they can tell jokes for me.I will have more free time to have a relax. 。

第9篇：Happy family 。

I have happy family, it is my father, my mother and me. 。

My father is very fat, he is a civil servant, he works very hard.. Father is very funny, put my family very happy. I’m very happy. 。

My mother is very thin, she is civil servant, too. She is a good cooker, she cooks food for everybody. She is quiet, and she likes books and swimming. 。

I’m a little girl in the family, maybe I’ll be a writer. I like hamburger, chips, books, swim. 。

This is my happy family! 。

第10篇：My Eddweiss 。

Eddwiss, edelweiss, every morning you grate me, small and white , clean and bright. 。

You must have heard of this song. Do you look for edelweiss? I found it. In winter, I went to the mountain. I found a small edelweiss blossoming among grass. It had pure white. I endulged in the beautiful scenery. Edelweiss is like an angel, it is dancing and smiling to me. The next day I went to see it. I cannot forget that small edelwiess。

请张宪宝 英语学研究专家 帮忙

Takanobu Kamataki。

（Division of Earth and Planetary Sciences，Graduate School of Sciences，Kyoto，Kyoto 606-01，Japan）

Yasuo Kondo

（Department of Geology，Faculty of Sciences，Kochi University，Kochi 780，Japan）

摘要　从分布在房总（Boso）半岛西海岸、东京海湾东边的Anesaki地区的Shimosa群中的非海相至浅海相旋回层序中，共识别出9个与20ka或40ka旋回相对应的沉积层序。一个典型的旋回包括淡水泥、浅海相砂（海侵体系域）和浅海相砂（高水位体系域）。对沉积层序中的软体动物化石组合分析表明，沉积环境和海洋气候在冷水、淡水或半咸水环境或潮上带与温水潮下带下部间摆动。大约50～60m规模的水深变化和紧密相关的气候变化有力地说明了它的成因是冰川海平面变化。基于已发表的裂变径迹年代测定数据，韵律层序间距的同位素标尺跨度可从5到11。根据米兰科维奇理论，每个旋回的定时被推断为与20ka或40ka旋回相对应，后者由轨道岁差和倾斜度的周期性变化所引起。

关键词　沉积旋回　软体动物化石　岁差　倾斜度　米兰科维奇理论　中上更新统　Shimosa群。

1　引言

更新世期间由冰川性海平面升降引起的沉积旋回已从陆上的浅海相沉积层序中得到辨认，它包括新西兰旺阿努伊的Okehu群、Kai-iwi群和Shakespeare群[3,1]，日本神奈川的Omma组[9～11]和房总半岛的Kazusa群和Shimosa群[2，24，12，25，6，4，13，18，14，5，7，8]。其中，房总半岛位于冷亲潮（Oyashio）和暖黑潮（Kuroshio）的混合水域附近（图1），这些沉积物中的软体动物组合是气候变化的敏感指示物。而且，显示古气候区系的软体动物组合可能是海平面的指示标志。因此，这些沉积旋回的成因已被解释为是冰川海平面升降的结果（如文献[25，12，13，8]）。近来，Ito和O'Hara[7]声称他们通过对Jizodo组的层序地层分析，识别出了一个冰川海平面升降成因的沉积层序，对应于氧同位素地层的第12段至第10段。同样地，Yabu组相当于第10段至第8段，Kamiizumi组、Kiyokawa组和Yokata组相当于第8段至第6段[18，5，15]。然而，这些解释还未经富含在层序中的软体化石组合定量数据的检验。

我们对软体化石的定量分析表明，被认为对应于10万年旋回的Jizodo组和Yabu组可进一步分别划分为3个和2个不同的沉积层序。本文提出了穿过这些旋回的水深和气候变化的简况。

图1　研究区示意图

2　地质背景

中上更新统Shimosa群的旋回层序在日本中部房总半岛的北部有很好的露头（图1）。它沉积在一个称为古东京湾的浅海湾地区。以千叶县Anesaki区的沉积旋回层为基础，Shimosa群可划分为6个组，按层序向上依次为Jizodo组、Yabu组、Kamiizumi组、Kiyokawa组、Yokota组和Kioroshi组。这些沉积旋回为非海相泥岩和海相砂岩的交互沉积。

3　方法

在软体化石的定量分析中，每个点上采集体积约为7dm3的85个大样。每个样品经过2mm筛网的筛选分离出化石和沉积物。我们用近代软体动物的水深分布和地理分布两方面的数据作为古气候的指示物[19，20，17]。Shimosa群中大部分软体化石都为现存的种类。Oya-ma[20]对其水深分布范围规定如下：N0——现生活在潮间带的种；N1——从低潮面至20～30m深；N2——从20～30m至50～60m深；N3——从50～60m至100～120m深；N4——从100～120m至200～250m深。O'Hara[17]使用了下列的地理分布；K-1——现生活在北纬35°以南地区的种；K-2——北纬39°以南地区；J——北纬35°以南至北纬39°以北地区；O-2——北纬35°以北地区；O-1——北纬39。以北地区。我们在分析化石组合中也使用了这些含义。

4　沉积相和软体化石

图2概述了Shimosa群旋回层序的古环境再造。Shimosa群中每个沉积层序包括2个体系域：海侵体系域（TST）和高水位体系域（HST）（图2）。TST表现为港湾泥岩、海侵滞后沉积和近海泥质砂岩。港湾泥岩相形成于海平面上升早期的海湾环境。海侵滞后相沉积于海平面上升早期的开阔海岸环境。TST和HST的分界面（下超面）在Shirnosa群中很容易辨认；TST的顶部具有弱胶结的化石密集层，形成一个凝缩段。HST表现为滨前和海滩砂。

图2　Shimosa群沉积期水深变化一览表。

氧同位素记录为V28-239。Jz—Jizodo组；Yb—Yabu组；Km—Kamiizumi组；Ky—Kiyokawa组；Yk—Yokota组；DS—沉积层序；TST—海侵体系域；HST—高水位体系域。

保存在Shimosa群中的软体化石是水深和海洋气候的有效指示物（图2）。从上潮下带冷水软体动物，经下潮下带暖水软体动物，再回到上潮下带冷水软体动物的旋回变化，出现在每一个沉积层序中。TST的底部包括浅海相软体化石，如在港湾泥岩中原地的Crassostreagigas和Potamocorbura amurensis，或砾状砂岩中外来的Glycymeris yessoensis和Dosiniatroscheli。下潮下带暖水软体化石的比例向TST的顶部方向增加。凝缩段包括下潮下带暖水软体动物，如Keenaea samarangae、Glycymeris rotunda、Glycymeris pilsbryi和Cryptopecten vesiculosus。在HST中，上潮下带冷水软体化石沿层序向上变得越来越丰富，如外来的Gly-cymeris yessoensis和Pseudocardium sachalinense；而下潮下带暖水软体化石不再出现。所以HST被解释为形成于气候变冷的条件下海平面下降的初期。这些动物群旋回反映了冰川海平面的升降。

5　讨论和总结

（1）Jizodo组包括3个沉积层序，Yabu组包括2个。所以，除位于Shimosa群最上部单元的Kioroshi组外，该群包括8个沉积层序，每个都对应于一个海侵－海退旋回（图2）。尽管在旋回中基本旋回结构相同，但每个沉积层序都有其特有的要素，如沉积相序和TST/HST的相对厚度等。例如，在最下部的Jizodo组中旋回结构是高度不对称的，TST不足3m，而HST厚得多，超过20m。在Kiyokawa组中，TST和HST具有大致相同的厚度。这些差异反映了沉积盆地内地理环境的不同。此外，从下部到上部，从不对称旋回到对称旋回的总趋势指示了盆地的逐渐变浅。另外，每个沉积层序在TST的底部内有不同类型的软体动物组合和沉积相，它们由海平面上升早期不同的沉积环境引起。例如，沉积层序1的底部（图2）包括泥质沉积内原地的港湾相软体动物，而沉积层序2的底部（图2）包括海侵滞后沉积内外来的浅海相软体化石。

（2）根据关键的火山碎屑的裂变径迹法（图2）和软体动物壳的电子自旋共振法测年结果（如文献[23，16]），Shimosa群的中下部的时限大约为0.4～0.2Ma。0.1Ma级别的气候变化和海平面升降被认为在0.6Ma之后才占优势，它包括了Shimosa群的沉积期（如文献[26，21]）。实际上，以0.1Ma为周期的冰川性海平面升降造成的沉积层序，在Kanto地区的更新世浅海相沉积中已有报道[4，14，18]。然而，Shimosa群中的每个沉积层序被认为是在以大约20ka或40ka为周期的冰川性海平面升降影响下形成的。据米兰科维奇理论，它对应于轨道岁差或倾斜度的周期。由每个沉积层序中的软体化石组合作出的水深曲线，对应于来自V28-239的氧同位素曲线[22]。在Shimosa群的中下部，每个旋回对应于氧同位素地层的第11、9和7段的8个旋回中的海侵和海退（图2）。

致谢　感谢大阪大学的Fujio Masuda教授和京都大学的Kiyotaka Chinzei教授对这项研究提出有益的见解。

（余青译，聂浩刚校）

参考文献

[1]S.T.Abbott and R.M.Carter.The sequence architecture of mid-Pleistocene（c.1.1—0.4Ma）cyclothems from New Zealand:facies development during a period of orbital control on sea-level cyclicity.Spec.Publs.Int.Ass.Sediment.，1994，19，367～394.。

[2]N.Aoki and K.Baba.Pleistocene molluscan assemblages of the Boso Peninsula，Central Japan.Sci.Rep.，Inst.Geosci.，Tsukuba Univ.，（Sec.B），1980，1，107～148.。

[3]R.M.Carter.S.T.Abbott.C.S.Fulthorpe，D.W.Haywick and R.A.Henderson.Application of global sea-level and sequence-stratigraphic models in Southern Hemisphere Neogene strata from New Zealand.Spec.Publs.Int.Ass.Sediment.，1991，12，41～65.。

[4]M.Ito.High-frequency depositional sequences of the upper part of the Kazusa Group，a middle Pleistocene forearc basin fill in Boso Peninsula，Japan.Sediment.Geol.，1992，76，155～175.。

[5]M.Ito.Stratigraphic records of glacio-eustasy in the Shimosa Group，a middle to late Pleistocene sedimentary fill in Paleo-Tokyo Bay，Japan.J.Coll.Arts and Sci.Chiba Univ.，1993，B-26，31～40.。

[6]M.Ito and S.O'Hara.Depositional sequences of the lower part of the Shimosa Group in Kimitsu and Futtsu Cities，Boso Peninsula，Japan.Rep.Environ.Res.Organization Chiba Univ.，1990，16，1～8（in Japanese with English abstract）.。

[7]M.Ito and S.O'Hara.Diachronous evolution of systems tracts in a depositional sequence from the middle Pleistocene palaeo-Tokyo Bay，Japan.Sedimentology，1994，41，677～697.。

[8]T.Kamataki and Y.Kondo.under review（in Japanese with English abstract）.。

[9]A.Kitamura and Y.Kondo.Cyclic changes of sediments and molluscan fossil associations caused by glacio-eustatic sea-level changes during the early Pleistocene——a case study of the middle part of the Omma Formation at the type locality.J.Geol.Soc.Jap.，1990，96，19～36（in Japanese with English abstract）.。

[10]A.Kitamura，H.Sakai and M.Horii.Sedimentary cycles caused by glacio-eustacy with the 41000-year orbital obliquity in the middle part of the Omma Formation（1.3—0.9Ma）.J.Sediment.Soc.Jap.，1993，38，67～72（in Japanese with English abstract）.。

[11]A.Kitamura，Y.Kondo，H.Sakai and M.Horii.Cyclic changes in lithofacies and molluscan content in the early Pleistocene Omma Formation，Central Japan related to the 41000-year orbital obliquity.Palaeogeogr.，Palaeoclimatol.，Palaeoecol.，1994，112，345～361.。

[12]Y.Kondo.Faunal condensation in early phases of glacio-eustatic sea-level rise，found in the middle to late Pleistocene Shimosa Group，Boso Peninsula，central Japan.In:Sedimentary facies in the active plate margin.A.Taira and F.Masuda（Eds.）.TERRAPUB，Tokyo，1989，197～212.。

[13]Y.Kondo，S.Matsui and K.Chinzei.Taphonomy and paleoecology of the Pleistocene molluscs in the Boso Peninsula.In:Island Arcs:Cenozoic stratigraphy and tectonics of Japan.H.Kato and H.Noro（Eds.）.Guide Book vol.2 of 29th IGC Field Trip B22，1992，99～108.。

[14]N.Murakoshi and F.Masuda.Estuarine，barrier-island to strand-plain sequence and related ravinement surface developed during the last interglacial in the Paleo-Tokyo Bay，Japan.Sediment.Geol.，1992，80，167～184.。

[15]H.Nakazato.Stratigraphic Relationship between the Kiyokawa and Kamiiwahashi Formations of the Middle-upper Pleistocene Shimosa Group，Chiba Prefecture，Central Japan.J.Nat.Hist.Mus.Chiba，1993，2，115～124（in Japanese with English abstract）.。

[16]H.Nakazato，K.Shimokawa and N.Imai.ESR age dating of the middle to upper Pleistocene Kazusa and Shimosa Groups.Earth Manthly（Gekkan Chikyu），1990，12，37～42（in Japanese）.。

[17]S.O'Hara.Molluscan fossils from the Higashiyatsu formation.Rep.Environ.Res.Organization Chiba Univ.，1973，B-6，67～83（in Japanese with English abstract）.。

[18]H.Okazaki.Sequence stratigraphy of the Shimosa Group.In:A Plio-Pleistocene fore-arc basin-fill in the Boso Peninsula，central Japan.Y.Makino，F.Masuda et al.（Eds.）.Guide Book of 29th IGC Field Trip A10，1992，52～60.。

[19]K.Oyama.Cthe vertical distribution of marine mollusca.Venus（Japan.J.Malacol.），1952，17，27～35（in Japanese with English abstract）.。

[20]K.Oyama.Revision of Matajiro Yokoyama's Type Mollusca from the Tertiary and Quaternary of the Kanto Area.Palaeont.Soc.Japan.Spec.Pap.，1973，17，148.。

[21]W.F.Ruddiman，M.E.Raymo，D.G.Martinson，B.M.Clement and J.Backman.Pleistocene evolution:Northern hemisphere ice sheets and North Atlantic Ocean.Paleoceanography，1989，4，353～412.。

[22]N.J.Shackleton and N.D.Opdyke.Oxygen-isotope and paleomagnetic stratigraphy of Pacific core V28-239:Late Pliocene to Latest Pleistocene.In:Investigations of Late Quaternary Paleoceanography and Paleoclimatology.R.M.Cline and J.D.Hays（Eds.）.Geol.Soc.Am.Mem.，1976，145，449～464.。

[23]M.Suzuki and S.Sugihara.Flssion-track age constraints on the Plio-Pleistocene boundary in the Kazusa Group.Abs.Ann.Meeting.Japan Assoc.Quat.Res.，1983，13，69～70（in Japanese）.。

[24]S.Tokuhashiand H.Endo.Geology of the Anesaki District.Quadrangle Series，scale1∶50000.Geological Survey of Japan，1984（in Japanese with English abstract）.。

[25]S.Tokuhashi and Y.Kondo.Sedimentary cycles and environments in the middle-late Pleistocene Shimosa Group，Boso Peninsula，central Japan.J.Geol.Soc.Jap.，1989，95，933～951（in Japanese with English abstract）.。

[26]D.G.Williams，R.C.Thunell，E.Tappa.D.Rio and I.Raffl.Chronology of the Pleistocene oxygen isotope record:0—1.88 m.y.B.P..Palaeogeog.，Palaeoclimatol.，Palaeoecol.，1988，64，221～240.。

原文地址：http://www.qianchusai.com/tracts-100.html