Qujing Economic and Technological Development Zone (QETDZ) is a significant provincial development zone approved by the Yunnan Provincial Government in August 1992. Located in the eastern part of urban Qujing, which is the second largest city in Yunnan in terms of economic strength, QETDZ holds a pivotal position as the economic, political, and cultural center of Qujing.
Qujing Economic and Technological Development Zone (QETDZ) stands as a cornerstone of economic vitality and urban development in Yunnan Province. With its strategic location, robust administrative framework, and ambitious development goals, QETDZ is poised to play a pivotal role in driving regional prosperity, fostering innovation, and promoting sustainable growth in the years to come.
Kunming Airport Economic Zone (KAEZ) is a significant economic development initiative strategically located around the Kunming Changshui International Airport in Yunnan Province, China. This zone is designed to leverage the airport’s pivotal role as a major transportation hub in Southwest China, promoting economic growth, industrial development, and international connectivity.
Location: Kunming Airport Economic Zone is situated adjacent to Kunming Changshui International Airport, approximately 24 kilometers northeast of Kunming City, the provincial capital of Yunnan Province.
Purpose: The primary objective of KAEZ is to integrate regional economic development with the operational capabilities of Kunming Changshui International Airport. It aims to enhance industrial competitiveness, attract investment, and foster innovation-driven industries.
The Kunming Airport Economic Zone plays a crucial role in advancing regional economic development, industrial diversification, and international connectivity in Yunnan Province. By leveraging the strategic location and operational capabilities of Kunming Changshui International Airport, KAEZ creates opportunities for business innovation, investment attraction, and sustainable development. Experience the synergy of logistics excellence, technological advancement, and economic dynamism at Kunming Airport Economic Zone, driving forward the economic prosperity and global competitiveness of Southwest China.
Kunming Dianchi Lake is among the 12 national tourism resorts in China approved by the State Council in 1992 and the only one located in an inland province. At present, it covers an area of 47.5 square kilometers, including Haigeng District with 22.5 square kilometers and Dayu District with 25 square kilometers, and has a total population of 110,000.
The Dianchi Lake Scenic Area is located in the southwest part of Kunming City. Dianchi Lake is the center of the resort. There are numerous attractions along the lake captivating tourists. Among these are the Yunnan Ethnic Villages, Daguan Park, Baiyukou Park, Haigeng Bank, Kwan-yin Hill, Xishan Forest Park, temples and pagodas.Towns, big or small near the lake provide visitors with an opportunity to experience customs of the local people.
Dianchi Lake(滇池)
Dianchi Lake is about 300 square kilometers (74,132 acres). It is the largest freshwater lake in Yunnan Province and the sixth largest one in China. With picturesque scenery and its location on the Yungui Plateau, the lake has a reputation as ‘A Pearl on the Plateau’. Unfortunately, the lake has been badly polluted. Although efforts have been made to save the lake, they have been largely unsuccessful.
The lake is crescent-shaped, about 39 kilometers (24 miles) in length and 13 kilometers (8 miles) in width at its widest. Its natural banks are formed by mountains on all four sides. More than twenty rivers nurture the lake which has a shoreline of 163.2 kilometers (101 miles). Four surrounding hills contribute to the picturesque landscape, making visitors intoxicated and linger around. You may appreciate the beauty of the lake and hills from a boat, and explore this cradle of Yunnan culture.
Yunnan Ethnic Villages ( 云南民族村)
The Yunnan Ethnic Village acts as a good shortcut to understand the social customs of the ethnic groups in Yunnan. It has a natural sun-bathing area where you can escape from the heat of summer. Twenty-five ethnic nationalities have their respective villages and conduct many activities to present their unique folkways and beautiful clothes. Also you can enjoy the water screen movie and an elephant performance, have a taste of the local dishes and buy pretty handicrafts.
Daguan Park (大观园)
Daguan Park is vibrant with rock gardens, pavilions, bridges and murmuring water. It is famous for the longest couplets in China on the Daguan Pavilion (dà guān lóu 大观楼). The Daguan Pavilion was built in the year 1828. It commands a lovely view. The couplet written in the Qing (qīng 清) Dynasty (1644-1911), contains 180 characters brimming with literary grace. During festival evenings, gatherings take place here
Baiyukou Park (白鱼口公园)
Baiyukou Park is on the west bank of Dianchi Lake. Here a small hill looks like a white fish opening its mouth to Dianchi Lake. Near the Irregular shore line, beautiful gardens are hidden among green trees. In spring, the cherry trees are in blossom, adding luster to this serene place. Overlooking Dianchi Lake, you can see white sails of boats on the glistening lake and gulls skimming over the waves.
Haigeng Bank (海埂)
Haigeng Bank is about four kilometers (2.5 miles) long while ranging in width from forty meters (131 feet) to three hundred meters (984 feet). The bank, like a floating jade belt, is in fact a watershed of the Dianchi Lake. Slender willow twigs sweep the lake in the gentle breeze. In the south is a wonderful natural swimming pool which is always crammed with people in midsummer.
Kwan-yin Hill(观音山)
Kwan-yin Hill is bordered by the vast lake and has an altitude of 2,040 meters (6,693 feet). Lofty peaks on this hill seem to thrust themselves straight towards the sky. A Kwan-yin Temple built here in the Ming Dynasty (1368-1644) was once a popular resort of Buddhism. Remaining are a seven-tier brick pagoda, houses, and a gate to the Kwan-yin Temple.How to get there: A Taxi ride to the northern section of the lake near Daguan Tower lakeside from the city center should cost you a mere Y15. You can also take bus 24 , 44 and get off at Haigeng Bank.
Take Bus 24, 44, 73, 94, 135, 172 or 233, and get off at Haigeng Gongyuan (Haigeng Park) Station.
Take a taxi to the Haigeng Park (near Dianchi Lake Scenic) costs about RMB25 yuan, it is about 12 kilometers from the Nanping Pedestrian Street of Kunming.
There is special line for traveling to Dianchi, you can take that car in the city center.
If you want to get rid of hustle of public transportation and troublesome navigation, you can book a private tour package which covers sightseeing, dining and transfer from us. Our local tour guide and driver will escort you to Dianchi Lake with speed and convenience, and take care of all the details. You just need to focus on sightseeing.
1.Recommended travel itinerary in Kunming including the Dianchi Lake: Visitors can firstly go to the West Hill Forest Park for a visit, then take the cable car from Longmen (the gate of the dragon) to Dianchi lake (Ticket price at RMB30).
2.There is no entrance fee charged at the Dianchi Lake, the entrance fee for Haigeng Park is RMB8 yuan. If guest do not want to take boat during the visit, a half day is enough for a visit to Dianchi Lake. If you want to explore the lake further, you can rent a bicycle and spend two days to cycle around the Dianchi, it is about 200 km.
Wanding Border Economic Cooperation Zone (WTBECZ) is a Chinese State Council-approved Industrial Park based in Wanding Town, Ruili City, Dehong Prefecture, Yunnan, China, founded in 1992 and was established to promote trade between China and Myanmar. The zone spans 6 km sq. and is focused on developing trading, processing, agriculture resources and tourism.
Wanding Border Economic Cooperation Zone (WTBECZ) is a State Council-approved industrial park located in Wanding Town, Ruili, Dehong Prefecture, Yunnan Province, China. Established in 1992, this zone is strategically positioned to facilitate trade and economic cooperation between China and Myanmar (Burma).
The Wanding Border Economic Cooperation Zone (WTBECZ) plays a crucial role in promoting economic cooperation, industrial development, and cultural exchange between China and Myanmar. With its strategic location and supportive policies, WTBECZ continues to facilitate trade, attract investments, and contribute to the economic prosperity of the region.
The Kunming Economic and Technology Development Zone (KETDZ), is a state-level economic development zone established on February 13, 2000 in East Kunming, Yunnan Province, China. It is administratively under Kunming Prefecture. It has a developed area of 6 square kilometers.
Kunming Economic and Technological Development Zone (KETDZ) is a national-level development zone approved by the State Council of China. Established in 1992, it is strategically located in Kunming, the capital city of Yunnan Province in southwest China.
The KETDZ has formed the industrial chain with the following major industries as its pillar industries:
The KETDZ is 4 kilometers from the downtown Kunming, where the highways lead straight to the China-Laos border town of Mohan, the China-Vietnam border town of Hekou, and the China-Myanmar (Burma) border town of Ruili. All three border towns are rated as Grade A border ports of China. All the highways within a radius of 200 kilometers from Kunming are of high-grade standards.
A railroad network has been built around Kunming, consisting of the Guiyang-Kunming, Chengdu-Kunming, Nanning-Kunming, Guangtong-Dali, and Yunnan-Vietnam Railways. The KETDZ is 2 kilometers away from the Kunming East Railway Station, and 4 kilometers from the Kunming South Railway Station, both are rail centers for both cargo and passenger transportation.
The Kunming International Airport, 1.8 kilometers from the KETDZ, is Yunnan’s most important gateway to international destinations. It operates eight air routes to overseas airports such as Singapore, Rangoon, Kuala Lumpur, Seoul, Osaka, and more than 70 domestic routes to Hong Kong, Macao, and other cities.
The KETDZ has access to ocean shipping at the Beihai and Fangcheng Ports in Guangxi province via the Nanning-Kunming Railway, at Zhanjiang Port of Guangdong province via the Guiyang-Kunming Railway, at Shanghai Port, and at Haiphong of Vietnam via the Yunnan-Vietnam Railway.
The Kunming Economic and Technological Development Zone (KETDZ) plays a pivotal role in advancing regional economic development, industrial diversification, and international connectivity in Yunnan Province. By leveraging its strategic location and comprehensive development strategies, KETDZ continues to attract investments, foster innovation, and contribute to the economic prosperity of Southwest China.
Yunnan Province in China hosts several Economic and Technological Development Zones (ETDZs), each contributing to regional economic growth, industrial development, and international trade. Here are some notable ETDZs in Yunnan:
These ETDZs in Yunnan Province play critical roles in attracting investment, promoting industrial transformation, fostering innovation, and facilitating international trade. They contribute significantly to Yunnan’s economic development strategies and regional prosperity.
These zones are integral to Yunnan’s strategy for economic growth, international trade facilitation, and tourism development, leveraging the province’s diverse resources and strategic location.
Yunnanosaurus (/ˌjuːnænoʊˈsɔːrəs/ YOO-nan-o-SAWR-əs) is an extinct genus of sauropodomorph dinosaur that lived approximately 201 to 168 million years ago in what is now the Yunnan Province, in China. Yunnanosaurus was a large sized, moderately-built, ground-dwelling, quadrupedal herbivore, that could also walk bipedally, and ranged in size from 7 meters (23 feet) long and 2 m (6.5 ft) high to 4 m (13 ft) high in the largest species.
Yang Zhongjian (also known as C. C. Young) discovered the first Yunnanosaurus skeletons in the Lufeng Formation of Yunnan, China. The fossil find was composed of over twenty incomplete skeletons, including two skulls, it was excavated by Tsun Yi Wang. When first discovered, Yunnanosaurus was considered to be closely related to Lufengosaurus, but more recent research by Novas et al. (2011) shows that it is most closely related to Anchisaurus and Jingshanosaurus.
There were more than sixty spoon shaped teeth in the jaws of Yunnanosaurus, and were unique among early sauropodomorphs in that its teeth were self-sharpening because they “[wore] against each other as the animal fed.”[2] Scientists consider these teeth to be advanced compared to other early sauropodomorphs, as they share features with the sauropods.[2] However, scientists do not consider Yunnanosaurus to be especially close to the sauropods in phylogeny because the remaining portions of the animals body are distinctly “prosauropod” in design.[2] This critical difference implies that the similarity in dentition between Yunnanosaurus and sauropods might be an example of convergent evolution.[2]
In 2007, Lü Junchang and colleagues described another species of Yunnanosaurus, Y. youngi (named in honor of C. C. Young). In addition to various skeletal differences, at 13 meters (42 ft) long Y. youngi was significantly larger than Y. huangi (which reached only 7 meters [23 ft]). Y. youngi is found later in the fossil record, hailing from the Middle Jurassic. The holotype specimen CXMVZA 185 consists of ten cervical vertebrae, fourteen dorsal vertebrae, three fused sacral vertebrae, seventeen caudal vertebrae, both pubic bones, both ischia, and the right illium. The skull of this species is not known.[3]
In 2013, Sekiya et al. described the discovery of a juvenile individual which was assigned to what the authors termed “Yunnanosaurus robustus” (i.e. Y. huangi).[Note 1]Specimen ZMNH-M8739 consists of partial cranial material and an almost complete post-cranial skeleton. This individual possesses characteristic dentition that suggests a potentially unique feeding mechanism as evidenced a tooth–tooth wear facet on its mesial maxillary and dentary teeth, and maxillary teeth that have coarse serrations. Comparison of this juvenile specimen with adult specimens of Yunnanosaurus huangi reveals very distinctive growth changes.[4]
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The type species, Y. huangi, was named by C. C. Young in 1942, who erected the family Yunnanosauridae to contain it, though the family currently comprises only this genus and sometimes Jingshanosaurus.[5] Young also named a second species, Y. robustus, in 1951,[2][6] but this has since been included in the type species.[2] The confusion in classification arose due to that the earliest specimens of Y. huangi were of juveniles individuals while the “Y. robustus” specimens represented fully grown adults.[2]Yunnanosaurus had been assigned to several taxa over the years, including Thecodontosauridae and Plateosauridae, but more recent phylogenetic analysis conducted by Novas et al. (2011) shows that this genus is part of the taxon Massopodain a clade with Anchisaurus and Jingshanosaurus.[1] Apaldetti et al. (2011) also found that Yunnanosaurus belonged in Massopoda, but found that this genus was more primitive than both Jingshanosaurus and Anchisaurus.[7]
A diagnosis is a statement of the anatomical features of an organism (or group) that collectively distinguish it from all other organisms. Some, but not all, of the features in a diagnosis are also autapomorphies. An autapomorphy is a distinctive anatomical feature that is unique to a given organism.
According to Sekiya et al. (2013), Yunnanosaurus can be distinguished from other dinosaurs based on the following characteristics:
According to Lu et a. (2007), Yunnanosaurus youngi can be distinguished from Yunnanosaurus huangi based on the following characteristics:
The type specimens of Yunnanosaurus huangi and Yunnanosaurus robustus were recovered in the Huangchiatien (Dahungtien) locality of the Lufeng Formation in Yunnan, China. The Y. huangi holotype specimen IVPP V20 and the Y. robustus holotype specimen IVPP V93, were collected by Chung Chien Young in terrestrial sediments from the upper dark/deep red beds of the Zhangjiawa Member of this formation, that are believed to have been deposited during the Sinemurian stage of the Jurassic period, approximately 199 to 190 million years ago.[8] Several other specimens assigned to Y. huangi (IVPP V54, IVPP V47, IVPP V61, IVPP V62, IVPP V63, IVPP V96, IVPP V264), and Y. robustus (IVPP V39, IVPP V94) were also recovered by Young in this locality. These specimens are all housed in the collection of the Institute of Vertebrate Paleontology and Paleoanthropology, in Beijing, China. In the years to come several more specimens assigned to these two species were recovered from Zhangjiawa Member of this formation.
Chung Chien Young had also explored the lower dark/dull purple beds of the Shawan Member of the Lufeng Formation and found more specimens that he later assigned to Y. huangi. Specimen IVPP V32 was collected by Young in 1938 in dark red, argillaceous sandstone that is believed to have been deposited during the Hettangian stage of the Jurassic period, approximately 201 to 199 million years ago.[8] Specimens IVPP V57, IVPP V60 and IVPP V272 were collected by Young in blue mudstone from the same formation and were also assigned to Y. huangi. These specimens from the Shawan Member are also housed in the collection of the Institute of Vertebrate Paleontology and Paleoanthropology.
The type specimen of Yunnanosaurus youngi was recovered at the Banqing Houshanliangzi locality of the Zhanghe Formation, in Yuanmou County of Yunnan Province, China. The holotype specimen CXMVZA 185 was collected in 2000 in terrestrial sediments deposited during the Aalenian and Bajocian stages of the Middle Jurassicperiod, approximately 174 to 168 million years ago. This specimen is housed in the collection of the Chuxiong Museum.
Yunnanosaurus huangi and Yunnanosaurus robustus shared their paleoenvironment with the ornithischians Bienosaurus, and Tatisaurus, the sauropodomorphsGyposaurus, Lufengosaurus, and Jingshanosaurus, and the theropods Sinosaurus triassicus and Eshanosaurus.
Yunnanolepis is an extinct genus of primitive antiarch placoderm. The fossils of the various species are found in Early to Middle Devonian strata in Southern China and Middle Devonian strata in Vietnam. Yunnanolepis is a genus of early vertebrate fish known from Yunnan Province, China.
Discovery and Naming
Physical Characteristics
Classification
Paleoecology
Significance
Yunnanolepis represents an important find in the study of early vertebrate evolution, particularly within the context of Paleozoic marine environments in Yunnan Province, China.
Yuanmousaurus was a sauropod dinosaur from the Middle Jurassic period of China. Known from incomplete remains, it was discovered in 2000 from the Zhanghe Formation in Yuanmou County, Yunnan Province. The type species, Yuanmousaurus jiangyiensis, was described in 2006 by Lü Junchang and colleagues. This dinosaur was a relatively large sauropod, potentially reaching about 17 meters (56 feet) in length. It is classified as a basal member of the Sauropoda, although its exact systematic position remains unclear. Recent studies have placed Yuanmousaurus within the family Mamenchisauridae.
Yuanmousaurus was estimated to be approximately 17 meters (56 feet) long. The fossil record for this dinosaur is incomplete, with the skull missing and the neck represented only by a fragment of a posterior cervical vertebra. This fragment suggests that the neck vertebrae were elongated, similar to those of mamenchisaurid sauropods, but unlike the shorter neck vertebrae of the more basal Shunosaurus.
From the trunk and tail, nine dorsal, three sacral, and seven caudal vertebrae were found. While the shoulder and pelvic girdles are mostly missing, except for one ilium, the limbs are better represented. The fossils include the humerus, ulna, radius, thigh bone, tibia, fibula, astragalus, and a claw from the hind foot. The forelimbs of Yuanmousaurus were proportionally longer than those of the short-necked Shunosaurus but shorter than those of Omeisaurus. Specifically, the length ratio between the humerus and thigh bone was 0.72 in Yuanmousaurus, compared to 0.56 in Shunosaurus and 0.80 in Omeisaurus.
Yuanmousaurus is considered a basal member of the Eusauropoda, which is outside the Neosauropoda that comprises all more derived sauropods. In its species description, Lü Junchang and colleagues initially classified Yuanmousaurus as a member of the Euhelopodidae, suggesting it was closely related to Patagosaurus, more basal than Euhelopus, and more derived than Omeisaurus. However, the Euhelopodidae has been largely abandoned by many paleontologists due to the controversial systematic position of Euhelopus itself. A newer analysis by Toru Sekiya places Yuanmousaurus within the Mamenchisauridae, along with Mamenchisaurus, Tienshanosaurus, and Chuanjiesaurus.
The only known skeleton of Yuanmousaurus (specimen YMV 601) was recovered in May 2000 in the village of Jiangyi in Yuanmou County, Yunnan Province. The excavation was led by paleontologists from the Yunnan Provincial Institute of Cultural Relics and Archaeology, the Yuanmou Museum, and the Chuxiong Museum. Today, the fossils are part of the Yuanmou Museum collection. The name Yuanmousaurus jiangyiensis refers to Yuanmou County and the village of Jiangyi, where the fossils were found.
Yizhousaurus is a genus of basal sauropodiform dinosaurs which existed in what is now Lower Lufeng Formation, Yunnan Province of southern China during the lower Jurassic period. Identified from a nearly complete and exquisitely preserved skeleton, it is the most complete basal sauropod currently known with intact skull. Although its name was revealed in a 2010 Geological Society of America abstract by Sankar Chatterjee, T. Wang, S.G. Pan, Z. Dong, X.C. Wu, and Paul Upchurch, it wasn’t validly named and described until 2018. The type species is Yizhousaurus sunae.
Discovery and Naming
Physical Characteristics
Classification
Paleoecology
Significance
Yizhousaurus is an important fossil find that adds to our knowledge of prosauropod dinosaurs and the ancient ecosystems of Yunnan Province, China.
Yimenosaurus (meaning “Yiman reptile”) is an extinct genus of plateosaurid sauropodomorph dinosaur that lived in China in the Early Jurassic. The genus was first named in 1990 by Ziqi Bai, Jie Yang and Guohui Wang, along with its type and only species, Yimenosaurus youngi. The species name honours renowned Chinese paleontologist Yang Zhongjian, the father of Chinese paleontology, known as C.C. Young in English. Known material includes the holotype, an almost complete skull and mandible, as well as incomplete cervical and dorsal vertebrae, a mostly complete sacrum, an ilium, ischia, partial ribs and complete femur, and a paratype, a well-preserved postcrania with a fragmentary skull.
Known from two specimens, Yimenosaurus is relatively complete for its type of sauropodomorph. The specimens were described originally in 1990 by Ziqi Bai, Jie Yang and Guohui Wang, and the describers named for them a complete binomial, Yimenosaurus youngi. Bai et al. created the genus name from Yimen county, the place of discovery in Yunnan Province, and the Latin word saurus, meaning “reptile”. For the species, it was chosen to honour Yang Zhongjian, the father and founder of all Chinese paleontology, who was well known for his work on “prosauropods”, and called in English C.C. Young. Of the two specimens, the holotype was chosen, known from a more complete skull. The holotype, YXV 8701, is known from a complete skull and mandibleonly lacking the anterior end of the jaw and minor fragments of bone around the orbit, as well as the postcranial elements of fragmentary cervical and dorsal vertebrae, all sacral vertebrae, an ilium, both ischia, a complete femur, and incomplete and damaged ribs. YXV8702, the paratype, is known from an only incomplete skull, many cervical and dorsal vertebrae, three sacrals, a few caudal vertebrae, a scapula-coracoid, an entire pelvis, and almost both entire hindlimbs.
Discovery and Naming
Physical Characteristics
Classification
Paleoecology
Significance
Yimenosaurus is an important fossil find that adds to our knowledge of sauropodomorph dinosaurs and the ancient ecosystems of Yunnan Province, China.
Xixiposaurus is a genus of prosauropod dinosaur which existed in what is now Lower Lufeng Formation, China during the lower Jurassic period.[1] It was first named by Sekiya Toru in 2010 and the type species is Xixiposaurus suni.
The remains of Xixiposaurus were found in 1984 at the Yujingzi Basin in China. These fossils were uncovered within layers of rock known as the Early Cretaceous Huiquanpu Formation, which has proven rich in specimens. Thanks, to preserved findings of Xixiposaurus scientists have gained valuable insights into its anatomy and behavior.
Located in Chinas Gansu Province these creatures roamed the Earth 160 million years ago during the Jurassic period. Belonging to the Oviraptorosauria family this dinosaur was estimated to reach a height of, around 1 meter and a length of 2 meters. It had a diet that consisted of plants possibly supplemented with insects or animals.
One of the characteristics of Xixiposaurus is its feathered body. Chinese paleontologists discovered this in 2012 when they unearthed the dinosaur’s remains. Recent research has confirmed that this dinosaur was indeed covered in feathers making it one of the known feathered dinosaurs.
Another intriguing feature of Xixiposaurus is its slender snout indicating that it may have been selective in its omnivorous diet choices. Its teeth were serrated, suggesting it possessed a biting force and could consume vegetation.
The finding of this dinosaur has provided insights into dinosaur evolution. Its feathered body suggests a link to birds as an ancestor. Scientists believe it offers a glimpse, into how dinosaurs developed feathers during their early stages. Interestingly the fossils of Xixiposaurus contained the remains of dinosaurs suggesting that it might have lived in groups or packs similar, to how many modern birds exhibit behaviors.
The Xixiposaurus was a dinosaur measuring around six feet in length. It had a body, and a tail and stood on two legs. Its front limbs were shorter than its hind limbs allowing it to move swiftly on two legs. Its skull was. Featured a snout. Interestingly it possessed a beak without teeth that it used for consuming vegetation.
This creature was classified as a dinosaur with an approximate length of 6.5 feet. It had a head, a neck, and a relatively short tail. The dinosaur had a physique. It is categorized as an ornithopod dinosaur due to its bird-like hip structure.
Scientists deduce from the shape of its teeth that the Xixiposaurus was an herbivore primarily relying on plants, for sustenance. The dinosaur likely utilized its beak to consume vegetation while using its molars to grind it up. Not much information is available, about the behavior of this dinosaur. It is believed that this dinosaur was a creature that lived in groups.
As mentioned before the Xixiposaurus was a dinosaur that primarily consumed plants. Its beak, which lacked teeth suggests that it used its mouth to trim vegetation. During the period the Yujingzi Basin was rich with forests and abundant plant life for the Xixiposaurus to feed on.
The discovery of these dinosaurs carries importance for many reasons. Firstly it contributes to our knowledge of the range of dinosaur species that thrived during the Mesozoic era. Additionally, it offers insights into the evolution of dinosaurs which were among the most successful dinosaur groups. Moreover finding Xixiposaurus fossils in the Lianmuqin Formation indicates that this region experienced levels of dinosaur diversity during the Cretaceous period.
Despite its stature, It holds value within scientific circles. As an unearthed species it enhances our understanding of dinosaur evolution and diversity throughout the period. Through analyzing its anatomy we can gain insights, into how ornithopods adapted to their changing environment over time.
Similar to dinosaur species there are still many unknowns, about the Xixiposaurus. Scientists will continue examining these fossils to gain insights into the traits, behaviors, and ecological roles of this dinosaur. This research has the potential to unveil revelations about the path of ornithopod dinosaurs and deepen our understanding of biodiversity during the Mesozoic era.
Belonging to the sauropod group renowned for their necks and tails one distinctive feature of this dinosaur was its adaptation. It possessed breathing tubes that extended from its nostrils to its lungs functioning as a snorkel that allowed it to breathe while submerged in water.
It shared a kinship with another sauropod called Mamenchisaurus. Both dinosaurs exhibited characteristics such as necks, tails, and dentition.
Like dinosaurs, it is speculated that these creatures utilized vocalizations as a means of communication with other members of their species. However, due to the preservation of tissues, in dinosaur fossils determining what these vocalizations sounded like remains challenging.
Discovery and Naming
The genus Xixiposaurus was named in 1983 by Dong Zhiming. Fossils were found in the Lower Lufeng Formation of Yunnan, which dates to the Sinemurian stage of the Early Jurassic.
Description
Xixiposaurus is characterized by its medium size and typical features of basal sauropodomorphs. It likely had a bipedal stance, though some remains suggest it might have been capable of quadrupedal locomotion.
Paleobiology
Like other sauropodomorphs of its time, Xixiposaurus was herbivorous and would have grazed on vegetation. Its skeletal structure indicates adaptations for supporting its body weight and efficient locomotion.
Paleoecology
The Lower Lufeng Formation in Yunnan, where Xixiposaurus fossils were found, is known for its rich dinosaur fauna. It includes other sauropodomorphs like Lufengosaurus, Yunnanosaurus, and Jingshanosaurus, as well as various theropods and early mammals.
Significance
Xixiposaurus contributes to our understanding of the early evolution of sauropodomorph dinosaurs in Asia, particularly in the context of the diverse fauna of the Early Jurassic Yunnan ecosystem.
Qujing Economic and Technological Development Zone (QETDZ) is a significant provincial development zone approved by the Yunnan Provincial Government in August 1992. Located in the eastern part of urban...
Kunming Airport Economic Zone (KAEZ) is a significant economic development initiative strategically located around the Kunming Changshui International Airport in Yunnan Province, China. This zone is designed to leverage...
Kunming Dianchi Lake is among the 12 national tourism resorts in China approved by the State Council in 1992 and the only one located in an inland province. At...
Wanding Border Economic Cooperation Zone (WTBECZ) is a Chinese State Council-approved Industrial Park based in Wanding Town, Ruili City, Dehong Prefecture, Yunnan, China, founded in 1992 and was established to promote trade between China an ...
The Kunming Economic and Technology Development Zone (KETDZ), is a state-level economic development zone established on February 13, 2000 in East Kunming, Yunnan Province, China. It is administratively under Kunming Prefecture. It has a dev ...
Yunnan Province in China hosts several Economic and Technological Development Zones (ETDZs), each contributing to regional economic growth, industrial development, and international trade. Here are some notable ETDZs in...
Yunnanosaurus (/ˌjuːnænoʊˈsɔːrəs/ YOO-nan-o-SAWR-əs) is an extinct genus of sauropodomorph dinosaur that lived approximately 201 to 168 million years ago in what is now the Yunnan Province, in China. Yunnanosaurus was a large sized, moderat ...
Yunnanolepis is an extinct genus of primitive antiarch placoderm. The fossils of the various species are found in Early to Middle Devonian strata in Southern China and Middle Devonian strata in Vietnam. Yunnanolepis is a genus of early...
Yuanmousaurus was a sauropod dinosaur from the Middle Jurassic period of China. Known from incomplete remains, it was discovered in 2000 from the Zhanghe Formation in Yuanmou County, Yunnan...
Yizhousaurus is a genus of basal sauropodiform dinosaurs which existed in what is now Lower Lufeng Formation, Yunnan Province of southern China during the lower Jurassic period. Identified from a nearly complete and exquisitely preserved sk ...
Yimenosaurus (meaning “Yiman reptile”) is an extinct genus of plateosaurid sauropodomorph dinosaur that lived in China in the Early Jurassic. The genus was first named in 1990 by Ziqi Bai, Jie Yang and Guohui Wang, along with...
Xixiposaurus is a genus of prosauropod dinosaur which existed in what is now Lower Lufeng Formation, China during the lower Jurassic period. It was first named by Sekiya Toru in 2010 and the type species is Xixiposaurus suni. Where was i ...
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Address: Building 4, Yifuyuan, Hehong Road, Xishan District, Kunming, Yunnan, China
Wechat/QQ: 270384698
Office Call: 86-18812220370
Email: Trip@YasoTrip.com
Facebook Page:
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Tel/WhatsApp: +8618088243690
Trip@YasoTrip.com