Der Formenkreis von Corydalis cava Schwgg. et Koerte

Von Jos. Scholz

[Corydalis solida - Lerchensporn]

AR

Corydalis cava - Corydalis solida

AR

Lerchensporn - Corydalis cava - Corydalis solida

AR

紫堇属的系统学研究

紫堇属（Corydalis DC.），广义罂粟科Papaveraceae的最大属，隶属于荷包牡丹亚科Fumarioideae的紫堇族Corydaleae，属内440余种，广布于北温带地区。我国产300余种，大部分种类为特有且狭域分布。本属形态多变，且网状进化明显，分类上十分困难。首先，鉴于对本属的系统划分及组间关系上所存较多争论，我们期望通过本研究获取一更自然的分类系统并追述真实的属下辐射进程。 研究内容包括两部分：分子系统学及孢粉学。 选取紫堇属100余种，几乎包括各组代表，通过测取叶绿体rps 16及matK序列信息，重建本属系统发育，实验获得98种rps16和78种的matK序列数据。分析显示，两个序列信息分别构建的系统树拓扑结构一致，支持5个分支结构。一些组的系统位置得以确定，一些类群的分类等级被界定，组间发育关系与传统观点差异显著。 根据对130余种，几含全部组代表的孢粉学研究观察，其结果支持分子系统学所得的多数结论，其它部分结论如下：1. 大叶紫堇组及高紫堇组所具的孢粉形态为次生性状，是由更原始的近光滑型及穿孔型演化而来;2. 糙果紫堇组，曲花紫堇组，鳞茎紫堇组做为近缘组，孢粉形态复杂而特化，组内个别系的孢粉形态与其它系的差异大于属下组间，如：Sect. Rupiferae Ser. Feddeana 该系种类外壁纹饰更近于穿孔型。3.刻叶紫堇组是一不自然的类群，支持其中个别种类与毛茎紫堇组这一单型组近缘。此外，也探讨了本属植物孢粉形态的演化趋势。 综合考虑两项研究的结果，结合形态信息，主要结论有： 其一：直茎黄堇组所代表的形态特征，如：植株具主根;叶羽状;花具短距，黄色;花柱柱头简单，乳突不为双生等, 具稀穿孔的近光滑孢粉外壁纹饰等为本属的原始形态特征。 其二：个别形态上一致的种类，实源于趋同进化，系统发育上即非一自然类群，化归为一类也无法真正体现属下真实的网状进化及形态趋同过程，如糙果组及鳞茎组两者的部分种类应并入曲花紫堇组，并且，后者应至少分立出大海黄堇组，并属于不同的亚属;同时，多叶紫堇组与钩距黄堇组近缘;大叶紫堇组与高紫堇组近缘;空根紫堇组与叠生延胡索组等块茎类关系极为密切。 其三：与传统处理不同，主张划分本属为5亚属，即：直茎亚属Subg. Cremnocapnos;黄堇亚属Subg. Sophorocapnos;延胡索亚属Subg. Corydalis;曲花亚属Subg. Rapiferae (C.Y.Wu et H. Chuang) Y. W. Wang stat. nov.;簇根亚属Subg. Fasciculatae (Maxim.) Y. W. Wang stat. nov.。 其四：推测本属植物在其演化历史上发生过至少两次较大规模的分化，第一次发生在晚白垩纪，期间适应各种气候类型的多年生原始种类出现;至第三纪早期开放的白令海峡允许不具长距离扩散能力的陆地植物类群扩散到北美;第二次发生在喜马拉雅隆升过程中，区域的气候变化使须根类群迅速发展，并形成该属位于青藏高原及横断山区的现代分布中心。

三种藏药材的化学成分研究

本学位论文报道了西藏产三种藏族传统植物药材的化学成分研究。论文由四章组成，前三章是实验部分，分别报道了尼泊尔黄堇(Corydalis hendersonii Hemsl.)、藏波罗花(Incarvillea younghusbandii Sprague)和全缘叶绿绒蒿(Meconopsis interifolia Franch.)的化学成分研究结果。从这三种青藏高原药用植物中共分离鉴定出33 个化合物，其中1 个是新化合物。第四章概述了罂粟科紫堇属植物的化学和药理研究进展。 第一章为尼泊尔黄堇的化学成分研究。通过正、反相硅胶柱色谱等分离方法从药用植物尼泊尔黄堇的地上部分共分离纯化得到12 个化合物。运用MS、1H-NMR、13C-NMR、DEPT、HMBC、NOESY 等现代波谱学方法将它们的结构鉴定为：刺罂粟碱(1) ， 普托品(2) ， 新那亭(3) ， 斯可任(4) ， tetrahydrothalifendine (5) ，9-methyl-decumbenine C (6)，tetrahydroberberrubine (7)，隐品碱(8)，α-别隐品碱(9)，6,7-methylenedioxy-1(2H)-oxoisoquinolinone (10)，6-丙酮基-5,6 -二氢血根碱(11)和β-谷甾醇(12)。其中化合物6 为新化合物，为首次发现的分子骨架上C-9 位连有甲基的苯肽异喹啉类型生物碱。另外，除化合物1 和2 外，其它9 个生物碱（3～11）均为首次从该种植物中分离得到。同时，我们还对对尼泊尔黄堇中的总生物碱进行了串联质谱分析。 第二章为藏波罗花的化学成分研究。从该药用植物的地上部分共分离得到16个化合物，通过理化常数和波谱数据鉴定为：异佛手柑内酯(1)，6-甲氧基当归素(2)，欧前胡素(3)，花椒毒内酯(4)，珊瑚菜素(5)，水合氧化前胡素(6)，rivulobirin A (7)，齐墩果酸甲酯(8)，咖啡酸甲酯(9)，银桦酸(10)，(D)-boschniakinic acid (11)，对羟基苯甲酸(12) ， tert-O-β-D-glucopyranosyl-(R)-heraclenol (13) ， 5-methoxy-8-O-β-D-glucopyranosyloxypsoralen (14)，前胡苷V(15)和苯乙醇-O-β-D-吡喃葡萄糖-(1→2)-O-β-D-吡喃葡萄糖苷(16)。所有以上化合物均为首次从该种植物中分离得到。另外我们还首次对藏波罗花挥发油的化学成分进行了气相色谱-质谱(GC-MS)联用分析，共鉴定出39 个挥发性成分。 第三章为全缘叶绿绒蒿化学成分的分离鉴定。从传统藏药材全缘叶绿绒蒿地上部分共分离纯化出8 个化合物。通过理化常数和波谱数据将他们的结构分别鉴定为：去甲血根碱(1)，β-谷甾醇(2)，3-羟基-齐墩果烷-12(13)-烯-30-酸(3)，6-丙酮基-5,6-二氢血根碱(4)，木犀草素(5)，胡萝卜苷(6)，quercetin 3-O-β-D-glucopyranosyl-(1→6)-β-D-glucopyranoside (7)和普托品(8)。其中化合物1，4 和7 为首次从该种药用植物中分离得到。 第四章为综述，总结和归纳了近年来罂粟科紫堇属植物的化学和药理研究进展。 This dissertation consists of four parts. The first, second and third parts report the studies on the chemical constituents from the medicinal plants of Corydalis hendersonii, Incarvillea younghusbandii and Meconopsis interifolia. The forth part reviews the progress of the studies on Corydalis species. The first chapter is about the isolations and identifications of alkalids from the aerial parts of C. hendersonii which is a traditional Tibetan medicine to treat febrifuge, high blood pressure and hepatitis. A new isoquinoline alkaloid, 9-methyl-decumbenine C (6), together with ten known alkaloids, stylopine (1), protopine (2), canadine (3), scoulerine (4), tetrahydrothalifendine (5), tetrahydroberberrubine (7), cryptopine (8), α-allocryptopine (9), 6,7-methylenedioxy-1(2H)-isoquinolinone (10) and 6-acetonyl-5,6-dihydrosanguinarine (11), and β-sitosterol (12) were isolated. Their structures were elucidated by spectroscopic methods. Furthermore, the total alkaloids were analyzed by ESI-MSn. The second chapter is about the isolations and identifications of chemical constituents from the aerial parts of I. younghusbandii. Sixteen compounds were isolated and purified by normal and reversed phase silica gel column chromatography. By spectral analysis, there structures were identified as isobergapten (1), sphondin (2), imperatorin (3), xanthotoxin (4), phellopterin (5), heraclenol (6), rivulobirin A (7), methyl oleanolate (8), methyl caffeate (9), grevillic acid (10), (D)-boschniakinic acid (11), 4-hydroxybenzoic acid (12), tert-O-β-D-glucopyranosyl-(R)-heraclenol (13), 5-methoxy-8-O-β-D-glucopyranosyloxypsoralen (14), decuroside Ⅴ(15), and phenylethyl-O-β-Dglucopyranosyl-(1→2)-β-D-glucopyranoside (16). All of these compounds were isolated from this plant for the first time．By the way, the chemical components of the essential oil from I. younghusbandii were analyzed by GC-MS for the first time. The third chapter is about the the isolations and identifications of the chemical constituents of M. interifolia. Eight compounds were isolated and identified as norsanguinarine (1), β-sitosterol (2), 3-hydroxyolean-12(13)-en-30-oic acid (3), 6-acetonyl-5,6-dihydrosanguinarine (4), luteolin (5), daucosterol (6), quercetin 3-O-β-D-glucopyranosyl-(1→6)-β-D-glucopyranoside (7) and protopine (8). The compounds 1, 4 and 7 were isolated from this herb for the first time. The last chapter is a review of the research progress of the studies on Corydalis species, which includes the chemical constituents in this genus and their pharmacology.

Biosynthesis of benzyliasoquinoline alkaloids

This research was carried out to obtain a convenient route for the synthesis of [7_ 14C]-p-hydroxy benzaldehyde. Section 1 of the thesis includes a route involving intermediates with protecting groups like benzyl and methyl ethers of the phenols. The benzyl ethers afforded the product in relatively better yield. The overall synthesis involves four steps. Section 2 describes the reactions carried out directly on phenols, and a three step pathway is obtained for the synthesis of p-hydroxy benzaldehyde, which was repeated on labelled compounds to obtain [7_14C]p- hydroxy benzaldehyde. The synthesis involves the reaction of p-bromophenol with Cu14CN to yield [7_ 14C]-p-cyano phenol, which is then reduced to the aldehyde by means of a simple and clean photolysis method. The same route was tried out to get 3,4-dihydroxybenzaldehyde and was found to work equally well for the synthesis of this compound. Section 3 deals with the isolation of labelled alkaloids, corydaline, protopine and reticu1ine from [2-3H,1-14C]-dopamine (3H/ 14C ratio = 4) fed Corydalis solida. 3H/14C ratios in the labelled alkaloids were determined. The uncorrected values showed almost 50% loss of 3H relative to 14C in reticuline, and roughly 75% loss of the 3H relative to 14C in corydaline and protopine.

Pollen profiles from 8 sediment cores from the Degersee, Southern Germany

The discovery of a neolithic pile field in the shallow water near the eastern shore of the Degersee confirmed earlier palynological and sedimentological studies stating that early man was active in the region since more than 6000 years. The already available off-site data were freshly assessed, completed by additional data from old and new cores and the interpretations revised. A common time scale for the off-site data and the on-site data was obtained by AMS dating of terrestrial macro remains of the neolithic section of off-site core De_I+De_H. The ages can thus be parallelled with AMS ages of construction timber on-site. Pollen analyses from all cores provide a further time scale. The continuously and densely sampled pollen profile of the profundal zone embracing the entire Late glacial and Holocene serves as a reference. From the Boreal onwards the relative ages are transformed by AMS ages and varve counts into calibrated and absolute. A transect cored close to the neolithic pile field across the lake marl-platform demonstrates its geological architecture in the shallow water since the Lateglacial. Studies of the microfabric of thin sections of drilled cores and of box cores from the excavations demonstrate that neolithic settlements now at 2-3,5 m water depth had been erected on lake marl freshly fallen dry, thus indicating earlier lake levels dropped by 1.5-2 m. The neolithic section of the highly resolved off-site profile in the lake=s profundal zone has laminated and calcareous zones alternating with massive ones. Assemblages of diatoms and concentrations of trace elements changing simultaneously characterise the calcareous sections as deposits of low lake levels that lasted between some 40 and more than 300 years. The ages of discovered lake shore dwellings fall into calcareous segments with low lake levels. From the end of the Upper Atlantic period (F VII) appear Secondary Forest Cycles in the beech forest, a man-made sequence of repeated vegetational development with an identical pattern: With a decrease of beech pollen appear pollen of grasses, herbs and cultural indicators. These are suppressed by the light demanding hazel and birch, those again by ash, and finally by the shade demanding beech forming a new pollen peak. Seven main Forest Cycles are identified In the upper Neolithic period each comprising some 250, 450 or 800 years. They are subdivided into subcycles that can be broken down by very dense sampling in even shorter cycles of decadal length. Farming settlers have caused minor patchy clearances of the beech-mixed-forest with the use of fire. The phases of clearance coincide with peaks of charcoal and low stands of the lake levels. The Secondary Forest Cycles and the continuous occurrence of charcoal prove a continued occupation of the region. Together with the repeated restoration of the beech climax forest they point to pulsating occupation probably associated with dynamic demography. The synchronism of the many palynological, sedimentological and archaeological data point to an external forcing as the climate that affects comprehensively all these proxies. The fluctuations of the activity of the sun as manifested in the residual d14C go largely along with the proxies. The initial clearances at the begin of the forest cycles are linked to low lake levels and negative values of d14C that point to dry and warm phases of a more continental climate type. The subcycles exist independent from climatic changes, indicating that early man acted largely independent from external forces.

High-resolution multi-proxy record of the last interglacial period from Lake Van, eastern Anatolian high plateau, Turkey

A high-resolution multi-proxy record from Lake Van, eastern Anatolia, derived from a lacustrine sequence cored at the 357 m deep Ahlat Ridge (AR), allows a comprehensive view of paleoclimate and environmental history in the continental Near East during the last interglacial (LI). We combined paleovegetation (pollen), stable oxygen isotope (d18Obulk) and XRF data from the same sedimentary sequence, showing distinct variations during the period from 135 to 110 ka ago leading into and out of full interglacial conditions. The last interglacial plateau, as defined by the presence of thermophilous steppe-forest communities, lasted ca. 13.5 ka, from ~129.1-115.6 ka BP. The detailed palynological sequence at Lake Van documents a vegetation succession with several climatic phases: (I) the Pistacia zone (ca. 131.2-129.1 ka BP) indicates summer dryness and mild winter conditions during the initial warming, (II) the Quercus-Ulmus zone (ca. 129.1-127.2 ka BP) occurred during warm and humid climate conditions with enhanced evaporation, (III) the Carpinus zone (ca. 127.2-124.1 ka BP) suggest increasingly cooler and wetter conditions, and (IV) the expansion of Pinus at ~124.1 ka BP marks the onset of a colder/drier environment that extended into the interval of global ice growth. Pollen data suggest migration of thermophilous trees from refugial areas at the beginning of the last interglacial. Analogous to the current interglacial, the migration documents a time lag between the onset of climatic amelioration and the establishment of an oak steppe-forest, spanning 2.1 ka. Hence, the major difference between the last interglacial compared to the current interglacial (Holocene) is the abundance of Pinus as well as the decrease of deciduous broad-leaved trees, indicating higher continentality during the last interglacial. Finally, our results demonstrate intra-interglacial variability in the low mid-latitudes and suggest a close connection with the high-frequency climate variability recorded in Greenland ice cores.

Pollen record and dating of a sediment profile from Ahlequellmoor in Germany

A pollen diagram from the Ahlequellmoor in the Solling area shows the history of vegetation and settlement over the last 7,800 years. In the early Atlantic period mixed deciduous forest with mainly Tilia together with Ulmus and Quercus grew in the area. In the late Atlantic period Quercus became most abundant. Fagus spread in the Sub-boreal period at about 2700 B.C. Since ca. 900 B.C. the Solling was covered by beech forests with some oak. In prehistoric times woodland grazing is indicated. Only in Medieval times are two settlements in the vicinity of the Ahlequellmoor reflected in the pollen diagram. The earlier one is dated to about A.D. 750-1020, and may be connected with the former Monastery of Hethis, which is thought to have existed close to the fen from A.D. 815 to 822. The second Medieval settlement dates to the 11th-12th century. The large-scale woodland destruction of late Medieval and modern times is not clearly visible. The silvicultural measures of the last 200 years are reflected by increasing values of spruce and grassland taxa.

Palynology on sediment profile Tso Kar in Ladakh

Palynological investigation of a 410 cm long core section from Tso Kar (33°10'N, 78°E, 4527 m a.s.l.), an alpine lake situated in the arid Ladakh area of NW India at the limit of the present-day Indian summer monsoon, was performed in order to reconstruct post-glacial regional vegetation and climate dynamics. The area was covered with alpine desert vegetation from ca. 15.2 to 14 kyr BP (1 kyr=1000 cal. years), reflecting dry and cold conditions. High influx values of long-distance transported Pinus sylvestris type pollen suggest prevailing air flow from the west and northwest. The spread of alpine meadow communities and local aquatic vegetation is a weak sign of climate amelioration after ca. 14 kyr BP. Pollen data (e.g. influx values of Pinus roxburghii type and Quercus) suggest that this was due to a strengthening of the summer monsoon and the reduced activity of westerly winds. The further spread of Artemisia and species-rich meadows occurred in response to improved moisture conditions between ca. 12.9 and 12.5 kyr BP. The subsequent change towards drier desert-steppe vegetation likely indicates more frequent westerly disturbances and associated snowfalls, which favoured the persistence of alpine meadows on edaphically moist sites. The spread of Chenopodiaceae-dominated vegetation associated with an extremely weak monsoon occurred at ca. 12.2-11.8 kyr BP during the Younger Dryas interstadial. A major increase in humidity is inferred from the development of Artemisia-dominated steppe and wet alpine meadows with Gentianaceae after the late glacial/early Holocene transition in response to the strengthening of the summer monsoon. Monsoonal influence reached maximum activity in the Tso Kar region between ca. 10.9 and 9.2 kyr BP. The subsequent development of the alpine meadow, steppe and desert-steppe vegetation points to a moderate reduction in the moisture supply, which can be linked to the weaker summer monsoon and the accompanying enhancement of the winter westerly flow from ca. 9.2 to 4.8 kyr BP. The highest water levels of Tso Kar around 8 kyr BP probably reflect combined effect of both monsoonal and westerly influence in the region. An abrupt shift towards aridity in the Tso Kar region occurred after ca. 4.8 kyr BP, as evidenced by an expansion of Chenopodiaceae-dominated desert-steppe. Low pollen influx values registered ca. 2.8-1.3 kyr BP suggest scarce vegetation cover and unfavourable growing conditions likely associated with a further weakening of the Indian Monsoon.

Fossil pollen record of composite sediment core TMD from Tso Moriri, analysis of modern surface pollen samples, mean annual precipitation reconstruction, and digitisation and recalibration of different discussed palaeoclimate proxy records

This paper presents a new fossil pollen record from Tso Moriri (32°54'N, 78°19'E, 4512 m a.s.l.) and seeks to reconstruct changes in mean annual precipitation (MAP) during the last 12,000 years. This high-alpine lake occupies an area of 140 km**2 in a glacial-tectonic valley in the northwestern Himalaya. The region has a cold climate, with a MAP <300 mm, and open vegetation. The hydrology is controlled by the Indian Summer Monsoon (ISM), but winter westerly-associated precipitation also affects the regional water balance. Results indicate that precipitation levels varied significantly during the Holocene. After a rapid increase in MAP, a phase of maximum humidity was reached between ca. 11 to 9.6 cal ka BP, followed by a gradual decline in MAP. This trend parallels the reduction in the Northern Hemisphere summer insolation. Comparison of different palaeoclimate proxy records reveal evidence for a stronger Holocene decrease in precipitation in the northern versus the southern parts of the ISM domain. The long-term trend of ISM weakening is overlaid with several short periods of greater dryness, which are broadly synchronous with the North Atlantic cold spells, suggesting reduced amounts of westerly-associated winter precipitation. Compared to the mid and late Holocene, it appears that westerlies had a greater influence on the western parts of the ISM domain during the early Holocene. During this period, the westerly-associated summer precipitation belt was positioned at Mediterranean latitudes and amplified the ISM-derived precipitation. The Tso Moriri pollen record and moisture reconstructions also suggest that changes in climatic conditions affected the ancient Harappan Civilisation, which flourished in the greater Indus Valley from approximately 5.2 to 3 cal ka BP. The prolonged Holocene trend towards aridity, punctuated by an interval of increased dryness (between ca. 4.5 to 4.3 cal ka BP), may have pushed the Mature Harappan urban settlements (between ca. 4.5 to 3.9 cal ka BP) to develop more efficient agricultural practices to deal with the increasingly acute water shortages. The amplified aridity associated with North Atlantic cooling between ca. 4 to 3.6 and around 3.2 cal ka BP further hindered local agriculture, possibly causing the deurbanisation that occurred from ca. 3.9 cal ka BP and eventual collapse of the Harappan Civilisation between ca. 3.5 to 3 cal ka BP.