
(Christopher) Yusheng Liu- Ph.D.
- Professor at University of Missouri–Kansas City
(Christopher) Yusheng Liu
- Ph.D.
- Professor at University of Missouri–Kansas City
About
94
Publications
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Introduction
(Christopher) Yusheng Liu currently works in the Office of Research & Economic Development and Department of Earth & Environment Science Projects and Biological Sciences, University of Missouri-Kansas City. The current project is 'Nature and Time on Earth - Project for a course and a book for virtual visits to past environments in learning programs for university students (coordinators Edoardo Martinetto, Emanuel Tschopp, Robert A. Gastaldo)'.
Current institution
Additional affiliations
August 2019 - present
January 2017 - July 2018
August 2015 - January 2017
Education
September 1989 - July 1992
Nanjing Institute of Geology & Palaeontology, Academia Sinica
Field of study
- Paleobotany
September 1986 - July 1989
Nanjing Institute of Geology & Palaeontology, Academia Sinica
Field of study
- Paleoclimate Studies
September 1982 - July 1986
Publications
Publications (94)
Microremains of fungi from Neogene deposits from the Gray Fossil Site (Tennessee, United States) and the Bełchatów Lignite Mine (Poland), similar to the enigmatic fossil-species Kutchiathyrites eccentricus R.K. Kar, 1979, were reconsidered as representatives of the modern mitosporic genus Mycoenterolobium Goos, 1970. A new combination, Mycoenterolo...
The spatio-temporal vegetation patterns of East Asia in the Eocene remain uncertain. In this present paper, we conduct numerical analyses of plant functional types (PFTs) for 80 Eocene floras, subdivided into three-time intervals: the early, middle, and late Eocene. Based on PFT diversity spectra, five groups are identified from cluster analysis an...
Plant–arthropod interaction offers insight into the evolution of terrestrial ecosystems in the geological past. In this study, leaf fossils with arthropod traces, collected from the Miocene Huaitoutala flora, Qaidam Basin, northern Tibetan Plateau, were studied to provide direct evidence of plant–arthropod interactions on the Tibetan Plateau. The r...
Large areas of Earth’s continents were covered by temperate forests before the dramatic increase of the human population in the past two millennia. Prior to human expansion, temperate forests were more extensive in the Neogene (23–2.6 Ma) when climate at the middle latitudes was slightly warmer and more equable than at the present. These temperate...
Pollen micromorphology provides one of the only morphological features characterising the phylogenetic lineages in oaks; therefore it is of great potential in understanding oak diversity in the geological past. In the present study, scanning electron microscopy (SEM) observations were made on the late Neogene pollen flora recovered from the well-kn...
The collision between India and Eurasia in the mid‐Palaeogene facilitated terrestrial floristic exchange. However, due to the complexity of this geological event and scarcity of fossil record, the plant migration patterns between the two plates are still highly debated. In this study, we focus on the Oligocene floristic exchange between India and P...
Interesting fungal remains were encountered during palynological investigation of the Neogene deposits at the Gray Fossil Site, Washington County, Tennessee, USA. Both Cephalothecoidomyces neogenicus and Trichothyrites cf. padappakarensis are new for the Neogene of North America, while remains of cephalothecoid fungus Cephalothecoidomyces neogenicu...
Fissistigma nanningense sp. nov. (Annonaceae) is described based on well-preserved mummified leaves from the Oligocene Yongning Formation of Nanning, Guangxi, southern China. They are characterized by retuse apex, a swollen petiole, eucamptodromous to simple brochidodromous secondary veins, percurrent tertiary veins, an obvious sub-vascular bundle...
The Gulf Stream, as part of the Atlantic Meridional Overturning Circulation (AMOC), is known as a major driver of latitudinal energy transport in the North Atlantic presently causing mild winters over northwestern Eurasia. The intensity of the AMOC throughout the Neogene, prior to the final closure of the Central American Seaway (CAS) in the early...
Paliurus (Rhamnaceae) is a small genus with a narrow and disjunct distribution in East Asia and the Mediterranean. Fossil evidence from the Late Cretaceous to the present suggests it once had a broad geographic distribution, encompassing parts of India, North America, Asia, and Europe. To reconstruct the evolutionary history of Paliurus and underst...
Abundant fossil records indicate that the genus Smilax L. was widely distributed in North America and Europe during the Paleogene and thrived in the Miocene. However, since the early Pliocene, the fossil occurrence of Smilax has become very rare. In this study, we describe three leaf taxa of Smilax from the upper Pliocene of West Yunnan, Southwest...
A middle Pleistocene flora from a low latitude of southern China was paleoclimatically studied through a quantitative reconstruction. The fossiliferous layer is correlated to the fourth terrace of the local Youjiang River and its age is revised to be the middle Pleistocene based on the presence of Paleolithic stones in the fourth terrace. The Coexi...
Late Neogene floras of North America are mainly represented by sites located along the east coast Piedmont and the Great Plains. To date, there are only two upper Neogene inland localities in the eastern half of North America, the Pipe Creek Sinkhole (Indiana) and the Gray Fossil Site (Tennessee). At both sites, a lacustrine environment was formed...
In Europe, fossil fruits and seeds of Rhodoleia (Hamamelidaceae) have been described from the Upper Cretaceous to the Miocene, whereas no fossil record of Rhodoleia has been reported in Asia, where the modern species occur. Herein, 21 fossil leaves identified as Rhodoleia tengchongensis sp. nov. are described from the Upper Pliocene of Tengchong Co...
Yunnan, southwestern China, represents a modern biodiversity center for Rubus (Rosaceae). The history for this high modern diversity remains poorly known due to the lack of fossil evidence. In this report, fossil pyrenes of Rubus are taxonomically studied from the late Pliocene (Piacenzian) of Lanping County, northwestern Yunnan. These pyrenes show...
It is widely accepted that the late Pliocene spans a time with globally warmer conditions compared to today. Regional specifics in temperature patterns from this period, however, remain poorly known. In this study, we reconstruct quantitatively late Pliocene climates for eight sites at the southeastern border of the Qinghai–Tibet Plateau (SBTP), ba...
The occurrences of Staphylea L. (Staphyleaceae) fossils have been abundantly documented from the Cenozoic of Eurasia, but none has been confirmed from North America to date. In this study, we describe Staphylea levisemia sp. nov. on the basis of seed remains from the latest Miocene to earliest Pliocene of northeastern Tennessee, southeastern USA. T...
Plant-insect interactions are vital for structuring terrestrial ecosystems. It is still unclear how climate change in geological time might have shaped plant-insect interactions leading to modern ecosystems. We investigated the effect of Quaternary climate change on plant-insect interactions by observing insect herbivory on leaves of an evergreen s...
East Asian Paleogene climates have long been regarded as controlled by the planetary wind system, which might result in a climate pattern with three latitudinally distributed zones. Two humid zones located separately in the north and south were lithologically designated by coals and oil shales, while an arid zone in the middle was represented by re...
Cenozoic climatic and environmental changes in the arid Asian interior, and their possible relations with global climatic changes and the Tibetan Plateau uplift, have been intensively investigated and debated over past decades. Here we present 40-Myr (million years)-long n-alkane records from a continuous Cenozoic sediment sequence in the Dahonggou...
The modern European climatic regime is peculiar, due to its unitary winter but diverse summer climates and a pronounced Mediterranean climate in the south. However, little is known on its evolution in the deep time. Here we reconstruct the European summer climate conditions in the Tortonian (11.62-7.246 Ma) using plant fossil assemblages from 75 we...
Fossil fruits including nuts and associated husk valves of a new species of Carya (Juglandaceae) are described from the latest Miocene to earliest Pliocene in northeastern Tennessee, eastern United States. The husk valves are elliptic, 1.2–4.5 mm thick, with a convex exterior face and a concave interior face; the nuts are globose to ovoid in shape,...
A new cycad species, Cycas fushunensis sp. nov., is described from the Lutetian Jijuntun Formation at Fushun Coalmine, Liaoning Province, northeast China, based on a well-preserved partial frond containing about 15 leaflets. The fossil is characterized by a single strong vein per leaflet, decurrent leaflet base and haplocheilic stomata, suggesting...
A new fossil species, Tsuga xianfengensis Xing et Zhou, n. sp., is reported based on two compressed seed cones. The fossil cones were discovered from the upper Miocene Xiaolongtan Formation at the Xianfeng Basin of Yunnan, southwestern China. The discovery of the Tsuga cones confirms the presence of Tsuga in the Miocene of central Yunnan and repres...
Continental Paleogene climates have been well studied in Europe and North America, but very little is known from Asia because paleoclimatic results have only been reported from particular geological intervals. Here, based on 29 plant assemblages from 8 well age-controlled fossiliferous sites, we quantitatively reconstruct the climates through most...
Today, the Gulf Stream causes considerable warming of the middle and higher latitudes of Western Eurasia also mirrored by vegetation distribution. Under the maritime climate of Western Eurasia vegetation types with a more thermophilous aspect exist compared to the eastern part of North America at the same latitude. Currently, discussion on changes...
The paleoclimate of the late Pliocene Longmen flora from Yongping County located at the southeastern boundary of the Qinghai-Tibet Plateau was reconstructed using two leaf physiognomy based methods, i.e. Leaf Margin Analysis (LMA) and Climate Leaf Analysis Multivariate Program (CLAMP), to understand the paleoclimate condition and geographical patte...
Climate change during the Quaternary played an important role in the distribution of extant plants. Herein, cone scales of Cedrus (Pinaceae) were uncovered from the Upper Pliocene Sanying Formation, Longmen Village, Yongping County of Yunnan Province in southwestern China. Detailed comparisons show that these fossils all belong to the genus Cedrus...
A new palaeopalynological investigation was conducted on 15 samples from four test-pits at the Gray Fossil Site (Bear Pit, Elephant Pit, Test Pit 2-2010, and Rhino Pit). In total, 50 morpho-species of miospores (including five species of spores, eight species of gymnosperm pollen, and 37 species of angiosperm pollen) and 18 morpho-species of freshw...
Quercus praedelavayi Xing Y.W. et Zhou Z.K. sp. nov. is reported from the upper Miocene of the Xianfeng flora in central Yunnan, southwestern China. The fossil species is identified based on the detailed leaf morphological and cuticular examinations. The primary venation is pinnate and the major secondary venation is craspedodromous with regular sp...
The relationship between leaf physiognomy and precipitation has been explored worldwide in regions under different climate conditions. Unlike the linear relationship established between the percentage of woody dicot species with entire margins and mean annual temperature, precipitation has been reported to correlate to different leaf physiognomic c...
The paleoclimate of the late Pliocene Longmen flora from Yongping County located at the southeastern boundary of the Qinghai-Tibet Plateau was reconstructed using two leaf physiognomy based methods, i.e. Leaf Margin Analysis (LMA) and Climate Leaf Analysis Multivariate Program (CLAMP), to understand the paleoclimate condition and geographical patte...
A new species of Cucubalus is described based on two fossil seeds recovered from the upper Pliocene Sanying Formation in northwestern Yunnan Province, southwestern China. The seeds are characterized by a reniform to circular outline in shape, and sinuous and discontinuous rugulae made of rod-like elements radiating from the hilum region to the dors...
Proxy-based quantitative estimates of Eocene climates can be made from marine isotope records for ocean conditions or fossil plants for terrestrial environment. However, our understanding about Eocene terrestrial climates is derived mainly from North America and Europe, and little is known about East Asia. Previous qualitative paleoclimate studies...
Today an effective Gulf Stream accounts for mild, maritime climate in Western Europe and causes significant longitudinal, climatic anomalies when comparing both sides of the North Atlantic, expressed in differentiated biome patterns. E.g. at ca. 40° northern latitude, evergreen broadleaved sclerophyllous woodland of the Northern Mediterranean corre...
In climatology, most variables are unequivocally defined and quantitatively described. These variables, such as temperature and precipitation, can also be quantified from geological proxies in paleoclimate studies. However, there are other climatic factors that, although strongly impacting ecosystems, have been ambiguously delineated and consequent...
Proxy-based quantitative estimates of Eocene climate conditions are abundantly available from marine isotope records and floral data. However, the available terrestrial data are mainly from North America and Europe, and only a few are known from East Asia. Previous qualitative studies on Chinese Eocene floras briefly illustrated the zonation of the...
The evolutionary history of Ginkgo is poorly understood for the Cenozoic Era because of the rarity of fossil reproductive organs. We here describe a new species, Ginkgo cranei sp. nov., on the basis of well-preserved ovulate organs and associated leaves from the Upper Paleocene Sentinel Butte Formation of North Dakota, USA. The ovulate organ is of...
Twenty-one fossil foliage, identified as Fokienia shengxianensis sp. nov. (Cupressaceae), were collected from the upper Miocene Shengxian Formation in Tiantai and Ninghai counties, Zhejiang Province of eastern China.These fossils can likely be distinguished from other extant genera in the family Cupressaceae s.l. except Fokienia by leaf external mo...
The late Miocene Xianfeng flora of Yunnan Province, southwestern China, was chosen to reconstruct the paleoclimate and the intensity of the Asian monsoon. Three available quantitative climate reconstruction methods from fossil plants, i.e. Leaf Margin Analysis (LMA), the Climate Leaf Analysis Multivariate Program (CLAMP), and the Coexistence Approa...
The timing of the development of the East Asian monsoon in the geologic
past is critically important for paleoclimatological studies, yet few
quantitative data are available. Based on palynomorphs from six
formations, supplemented by leaf fossils from one of these formations in
Fushun, northeastern China, we present a quantitative estimate of the
e...
Taxonomie révisée de certaines espèces d'endocarpes fossiles de Menispermaceae par une approche morphométrique. Plusieurs restes d'endocarpes du Cénozoïque de l'hémisphère nord ont été décrits comme ayant de fortes affinités avec soit Menispermum L. soit Sinomenium Diels, un groupe monophylétique de lianes des Menispermaceae. La synonymie de toutes...
The Miocene Lincang leaf assemblage is used in this paper as proxy data to reconstruct the palaeoclimate of southwestern Yunnan (SW China) and the evolution of monsoon intensity. Three quantitative methods were chosen for this reconstruction, i.e. Leaf Margin Analysis (LMA), Climate Leaf Analysis Multivariate Program (CLAMP), and the Coexistence Ap...
Neogene climates and vegetation history of western Yunnan are reconstructed on the basis of known fossil plants using the Coexistence Approach (CA) and Leaf Margin Analysis (LMA). Four Neogene leaf floras from Tengchong, Jianchuan and Eryuan in southwestern China are analyzed by the CA, and the paleoclimatic data of one Miocene carpoflora from Long...
The Miocene climate evolution in North China is preliminarily discussed by means of comparisons in seven climate parameters quantitatively reconstructed by the Coexistence Approach on 34 selected macro-and microfloras over North China. The Miocene temperatures show no great difference in the western and eastern part of North China. Temperature fluc...
This study focuses on morphometric and systematic analyses of the fossil Vitis seeds, recovered from the Gray Fossil Site (7–4.5Ma, latest Miocene–earliest Pliocene), northeastern Tennessee, U.S.A. A multivariate analysis based on eleven measured characters from 76 complete fossil seeds recognizes three morphotaxa. Further comparisons with both sel...
Pinus prekesiya Xing, Liu et Zhou sp. nov. was described as a new species on the basis of two well preserved ovulate cones from the upper Miocene of central Yunnan, southwestern China. It is the first fossil record of three dimensionally preserved Pinus ovulate cones from China. Morphological comparisons with 15 previously published Cenozoic cones...
Leaf margin analysis (LMA) is a widely used method that applies present-day linear correlation between the proportion of woody dicotyledonous species with untoothed leaves (P) and mean annual temperature (MAT) to estimate paleotemperatures from fossil leaf floras. Previous works demonstrate that LMA shows regional constraints and to date, no equati...
Plant fossils from the Citronelle Formation provide a rare window into the Pliocene flora and climate of the northeastern Gulf of Mexico Coastal Plain. Many of the taxa recovered to date inhabit the region today. However, analysis of Pinus pollen grains and fascicles indicates that the dominant pines were members of Pinus subgenus Strobus (i.e., "w...
The present study documents the first confirmed fossil record of Sinomenium in Menispermaceae, Sinomenium macrocarpum sp. nov., from the recently discovered Gray Fossil Site in Tennessee, southeastern USA. The fossil species is represented by more than 120 endocarps, all of which are characterized by their horseshoe-shaped form and occurrence of hi...
A large number of fossilized remains, consisting of leafy branchlets, seed cones, pollen cones, and seeds, of Metasequoia (Cupressaceae) recovered from Middle Eocene sediments of the Buchanan Lake Formation, Axel Heiberg Island, Canadian Arctic Archipelago are studied morphologically and anatomically. They are assigned to M occidentalis (NEWBERRY)...
The megafossil record of Chamaecyparis (Cupressaceae) in the Northern Hemisphere, especially that in Europe, is reviewed with the aim of gaining a better understanding
of the biogeographic history of this genus and providing an explanation of the causes of eastern Asian and western and eastern
North American intercontinental disjunction of extant m...
The late Miocene Xiaolongtan megaflora from Kaiyuan in southeast Yunnan (23°48′45″N, 103°11′52″E, 1050 m a.s.l.) was chosen for palaeoclimatic reconstruction using three quantitative techniques, i.e. the Coexistence Approach (CA), Leaf Margin Analysis (LMA), and the Climate–Leaf Analysis Multivariate Program (CLAMP). The reconstructed climatic para...
Eight fossil leaves identified as Exbucklandia tengchongensis sp. nov. (Hamamelidaceae) were collected from the Pliocene Mangbang Formation in Tengchong, Yunnan Province, Southwest China. The fossil leaves are characterized by the overall rounded lamina with entire margin, actinodromous venation, and cyclocytic stomata, which suggest the affinity w...
A newly discovered fossil pollen taxon is described as Lagerstroemia cathayensis sp. nov. on the basis of a combination of morphological characters including prolate shape with no or weakly developed pseudocolpi and rugulate‐verrucate tectum. The fossil pollen was recovered from a Miocene deposit in Zhejiang province, eastern China. It resembles po...
a b s t r a c t A new and convenient fluorescence spectroscopic method has been developed for the sep-aration and determination of perylene in fossil wood recovered from a late Miocene to early Pliocene Gray Fossil Site in Tennessee, USA. This is the first report where perylene was separated from fossil samples from this newly discovered fossil sit...
Fagus in China is never dominant in Late Cretaceous and Tertiary floras although it might reach its highest diversity in the Miocene. The genus Fagus was more widely distributed during the Palaeogene than in the Neogene. Furthermore, the ecological requirements of Fagus in the Palaeogene seem much broader than those in the Neogene onwards. This is...
In palaeopalynology oaks are rarely identified beyond the generic level. In order to recognize fossil evergreen and deciduous oak pollen, we compiled distinguishing criteria from the literature, most under the SEM, on the living oaks. One of the most significant criteria is the nature of the sculpturing under the SEM. Evergreen oak pollen exhibit a...
Abstract Recently, whether Archaefructus has bisexual multi-parted flowers or just inflorescences of unisexual flowers, and whether it is ancestral to all angiosperms or a derived eudicot have been debated. Here, from the same Yixian Formation, NE China, we report a new Archaefructus species, A. eoflora sp. nov., with the generic characteristics of...
Palynological studies of the Eocene Buchanan Lake Formation, Axel Heiberg Island, Canadian High Arctic, have yielded pollen grains closely comparable to those of extant Cathaya Chun et Kuang, a paleoendemic conifer of southwestern China. These palynomorphs are assigned to Cathaya gaussenii Sivak, which is here interpreted as the only species to whi...
Fagus in China is never dominant in Late Cretaceous and Tertiary floras although it might reach its highest diversity in the Miocene. The genus Fagus was more widely distributed during the Palaeogene than in the Neogene. Furthermore, the ecological requirements of Fagus in the Palaeogene seem much broader than those in the Neogene onwards. This is...
A species of fossil pollen Cathaya zhejiangensis sp. nov. from the Miocene of eastern China is described. This is the first authentic fossil record of Cathaya from China. Diagnostic features of the pollen morphology under LM and SEM of both fossil and living Cathaya are also presented. Moreover, the recent ecology of the genus Cathaya at the type l...
A revision on the Chinese Cenozoic megafossils of Fagus is undertaken. Seven species are recognized, among which one is represented by cupule fossils, while all the others are leaves. The oldest species, Fagus sp. 1 with similarities to two Chinese living endemic beeches, F. engleriana Seem, and F. longipetiolata Seem., is documented from the Late...
Two fossil leaves with cuticle described here were collected from the Pleistocene Changseling Formation of Baise Basin, Guangxi. A detailed comparison of the cuticular analysis between the fossils and their living equivalents indicated that the two fossil species belong to 2 genera of Lauraceae, that is, Alseodaphne cf, hainanensis Merr. and Pheobe...