Next Article in Journal
Seed Germination Ecology of Chenopodium album and Chenopodium murale
Next Article in Special Issue
Fossil Fruits of Ceratophyllum from the Upper Eocene and Miocene of South China
Previous Article in Journal
Long-Term Survival and Curative-Intent Treatment in Hepatitis B or C Virus-Associated Hepatocellular Carcinoma Patients Diagnosed during Screening
Previous Article in Special Issue
A New Fern-like Plant Xinhangia spina Gen. et sp. Nov. from the Upper Devonian of China
 
 
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Communication

A Flower Bud from the Lower Cretaceous of China

1
Key Laboratory of National Forestry and Grassland Administration for Orchid Conservation and Utilization, the National Orchid Conservation Center of China and the Orchid Conservation & Research Center of Shenzhen, Shenzhen 518114, China
2
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and CAS Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, China
*
Author to whom correspondence should be addressed.
Biology 2022, 11(11), 1598; https://doi.org/10.3390/biology11111598
Submission received: 26 September 2022 / Revised: 27 October 2022 / Accepted: 27 October 2022 / Published: 1 November 2022
(This article belongs to the Special Issue Recent Advances in Palaeobotany)

Abstract

:

Simple Summary

Flowers are beautiful due to their perianth which is frequently colourful and conspicuous. The existence of the colourful perianth is closely related to insect pollination in extant angiosperms. The Early Cretaceous (1.25 million years ago) Yixian Formation in Northeastern China is famous for its great diversity of reproductive organs of early angiosperms. However, unlike typical flowers in extant angiosperms, the previously documented fossil flowers are “naked”, namely, they do not have typical perianth, suggestive of a strategy different than the extant one adopted in the reproduction of early angiosperms. However, without fossil evidence, whether there is perianth and whether androecium and gynoecium are protected in early flowers are open questions. In this paper, we document the first flower bud fossil, Archaebuda lingyuanensis, from the Yixian Formation. Besides being the first recorded flower bud (which is fragile and unlikely to be fossilized) in the Early Cretaceous, the flower bud does protect its internal parts, which are vulnerable to various attacks and harm, using the perianth. In addition, perianth plays an important role in attracting insects for successful pollination of early angiosperms. This knowledge on the reproduction of early angiosperms is otherwise unavailable if only the previous fossils are taken into consideration.

Abstract

Background: Although various angiosperms (including their flowers) have been reported from the Yixian Formation (Lower Cretaceous) of China, which is famous worldwide for its fossils of early angiosperms, no flower bud has hitherto been seen in the Early Cretaceous. Such a lack of examples hinders our understanding of the evolution of flowers. Methods: The specimen studied in the present paper was collected from an outcrop of the Yixian Formation (the Barremian-Aptian, Lower Cretaceous) of Dawangzhangzi in Lingyuan, Liaoning, China. The specimen was photographed using a Nikon D200 digital camera, its details were observed and photographed using a Nikon SMZ1500 stereomicroscope, and some of its details were observed using a Leo 1530 VP SEM. Results: We report a fossilized flower bud, Archaebuda lingyuanensis gen. et sp. nov, from the Yixian Formation of China. The debut of Archaebuda in the Yixian Formation provides first-hand material for debate on the early evolution of angiosperm flowers and underscores the great diversity of angiosperms in the Yixian Formation.

1. Introduction

Angiosperms have more than 300,000 species spread over Earth’s ecosystems, accounting for more than 90% of the species diversity of land plants. They are not only an indispensable component of the ecological background, in which human beings originated and evolved, but they also supply most of the materials necessary for the sustainable development and survival of humans. Despite the importance of angiosperms, their origin and early evolution have been perplexing and mysterious, therefore, these questions have become foci of botanical debates for a long time. Fossil evidence plays an important role in our understanding of the origin and evolution of angiosperms and their flowers. The discovery of the bisexual reproductive organs of Bennettitales [1] became crucial fossil evidence for Arber and Parkin [2], who proposed Magnoliales as the ancestral type in angiosperms, and this school of botany was highly dominant in botany until the 1990s. It is obvious that fossil evidence can lend a hand to botanists in their academic debates. Unfortunately, fossils are not always easy to access, especially those of the more fragile parts of plants, such as flower buds. Early angiosperms, including Archaefructus and other pioneer angiosperms [3,4,5,6,7,8,9,10,11,12,13,14,15], have been repeatedly documented from the Yixian Formation of northeastern China. These valuable specimens have supplied important first-hand materials for the debates over angiosperm evolution. However, flower buds have so far been lacking in the Yixian Formation. This lack of information makes many hypotheses on flower evolution open to question. To make our knowledge of early angiosperms comprehensive, we report here a flower bud fossil from the Yixian Formation (Lower Cretaceous). Archaebuda is the first flower bud found from the Yixian Formation. The debut of Archaebuda in the Formation adds to the already great diversity of angiosperms in the Lower Cretaceous and sheds new light on the evolution of early flowers.

2. Materials and Methods

The Yixian Formation of Northeastern China has yielded various fossilized animals and plants [3,4,5,7,8,9,10,11,12,13,14,15,16,17,18,19,20,21,22,23,24,25,26,27,28,29,30,31,32,33,34,35,36], and stratigraphers have intensively studied the formation [37,38,39,40,41,42,43,44,45,46]. Although the age of the formation used to reach up to the Jurassic, recent works converge on a general consensus of approximately 125 Ma (Barremian-Aptian, Lower Cretaceous) [47]. The fossil specimen studied here was collected from the Dawangzhangzi outcrop of the Yixian Formation near Lingyuan, Liaoning, China (Figure 1). The specimen was preserved as a compression/impression embedded in thin-layered siltstone. The specimen is 32 mm long and 8.6 mm wide, preserved on slightly yellowish-grey siltstone (Figure 2a). The whole specimen was imaged using a Nikon D300S digital camera. Morphological details were imaged using a Nikon SMZ1500 stereomicroscope equipped with a Nikon DS-Fi1 digital camera and a Leo 1530 VP scanning electron microscope (SEM) at the Nanjing Institute of Geology and Palaeontology, CAS (NIGPAS). A sketch was drawn from photographic images of the specimen, and all figures are organized using Photoshop 7.0.

3. Results

Genus Archaebuda gen. nov.
Generic diagnosis: Flower bud—long-stalked. Stalk—straight, bearing scaly leaves. Scaly leaves—long–triangular and spirally arranged along the stalk. Bud—elongated oval, including two types of foliar appendages. Foliar appendage of type I—smaller, keeled, and round-tipped. Foliar appendage of type II—bigger, keel free, papery, notched at the tip, overlapping each other, and consisting of at least three layers. Stamens and gynoecium—unknown.
Type species: Archaebuda lingyuanensis gen. et sp. nov.
Etymology: Archae- Latin word for ancient and -buda from the English word bud.
SpeciesArchaebuda lingyuanensis sp. nov.
Species diagnosis: The same as that of the genus.
Description: The specimen includes a stalk and a flower bud on the terminal of the stalk (Figure 2a). The stalk is slender, long, and straight, 15.5 mm long and 1.9 mm wide, bearing scaly leaves (Figure 2a). The scaly leaves are 3–3.5 mm long and 0.9–1.1 mm wide, spirally adnate to the stalk for 85% of its length, only 15% of the distal portion is free from the stalk, slightly crenate-margined, keel-free, long–triangular, with longitudinally oriented epidermal cells (Figure 2a–f and Figure 3a,b). The bud is elliptical in shape, 17 mm long and 9 mm wide (Figure 2a,b). Foliar appendages of type I are at the base of the bud, smaller than the foliar appendages of type II, 2.6 mm long and 3 mm wide, keeled, with a round tip, and longitudinally oriented epidermal cells (Figure 3c,d). Foliar appendages of type II are bigger than the foliar appendage of type I, 4.8–16.8 mm long and 4.1–7.6 mm wide, keel-free, papery, frequently notched at the tip, overlapping each other, consisting of at least three layers, and with longitudinally oriented epidermal cells (Figure 2b,c and Figure 3a,b).
Etymology: lingyuan-, for Lingyuan City, Liaoning, China, the fossil locality.
Holotype: 20130506025 (Figure 2 and Figure 3).
Type locality: Dawangzhangzi, Lingyuan, Liaoning, China (41°15′ N, 119°15′ E, Figure 1).
Type horizon and age: the Yixian Formation, equivalent to the Barremian-Aptian, Lower Cretaceous (approximately 125 Ma).
Depository: the National Orchid Conservation Center of China and the Orchid Conservation & Research Center of Shenzhen, Shenzhen 518114, China.

4. Discussions

The scaly leaves on the stalk of Archaebuda are adnate to the stalk for most of their length, with triangular pointed tips (Figure 2d–f). Among known gymnosperms, scaly leaves of similar morphology are frequently seen in conifers, but so far have never been seen in Bennettitales, Ginkgoales, and Gnetales [48,49,50,51,52,53,54]. Although cataphylls similar to scaly leaves in Archaebuda are seen in the bottom of some cycad cones, these cataphylls have distal pricks that are lacking in the scaly leaves of Archaebuda (Figure 2d–f), and numerous peltate shields or tapering segments of “sporophylls” on the surface of cycad cones [55,56,57,58,59] distinguish cycads from Archaebuda (Figure 2a–c). The reproductive organs in these gymnosperms (including cycads) usually have either isolated projecting ovules/seeds (Ginkgoales) or radially arranged lateral appendages (Bennettitales and Gnetales) [48,60,61,62] rather than longitudinally-oriented foliar appendages in at least three layers as in Archaebuda (Figure 3a,b) and Magnolia (Figure S1a). Furthermore, all reproductive organs in gymnosperms (fossil and extant) are never known to have more than two layers of papery lateral appendages overlapping each other as in Archaebuda (Figure 3a,b). These differences distinguish our fossil from Bennettitales, Ginkgoales, Pentoxylales, Corystopsermales, Peltaspermales, and Gnetales [48,49,50,51,52,53,54]. Therefore, these gymnosperm groups are not further considered.
Since scaly leaves similar to those of Archaebuda are seen in some Coniferales, it is necessary to exclude conifers before further consideration. Reproductive organs play a more important role in plant taxonomy than foliages do. Some conifer cones (especially those of Abies and Picea in Pinaceae) [52,53,63,64] indeed demonstrate a certain resemblance (in general profile and terminal position) to Archaebuda. However, the following differences are obvious enough to distinguish them from Archaebuda: One, none of the gymnosperms have more than two layers of their lateral appendages overlapping each other, in strong contrast to three layers of overlapping papery foliar appendages seen in Figure 3a,b. This difference alone is enough to distinguish Archaebuda from all gymnosperm cones (fossil and extant). Two, although both are stalked, the stalk of Archaebuda is much more slender and elongated (as seen in tulip and poppy flowers) (Figure 2a) while the stalks are much more stout in most conifer cones [65,66] (except Amentotaxus, which has an elongated stalk but its integral aril is distinct from the overlapping papery foliar appendages in Archaebuda) [63]. Three, a conifer cone usually has multiple lateral appendages helically and vertically arranged around a central axis, and its surface is usually covered with apophyses (except Calocedrus and Juniperus) [52,53,54,63,64,66] (Figure S1b), while the surface of Archaebuda is relatively smooth, covered with papery foliar appendages lacking any special features except notched tips (Figure 2b and Figure 3a,b). Indeed, there are exceptional cones in Calocedrus and Juniperus that have a single bract covering almost the whole length of the cones [64,67], and thus demonstrate more similarity to Archaebuda than other conifer cones do. However, the bracts of Calocedrus have distal pricks, in contrast to the rounded tip (sometimes notched) of foliar appendages of type II in Archaebuda. The bracts in Juniperus have no distal pricks, but these bracts are fleshy and of only one layer [67], in strong contrast to at least three layers of papery foliar appendages overlapping each other in Archaebuda. Furthermore, pinaceous cones are characterized by their bracts separate from the scales and frequently visible on the cone surface [63,68], which are fully lacking in Archaebuda (Figure 2a–c). Some cupressoids (especially Athrotaxoideae, extant and fossil) may appear similar to Archaebuda in certain aspects. However, a careful examination can easily exclude this possibility. There are at most two lateral appendages of conifer cones partially overlapping each other, while there are three or more layers of overlapping papery foliar appendages in Archaebuda (Figure 3a,b). The latter case is routine and typical in flower buds of living angiosperms, for example, in Magnolia (Figure S1a) and many other angiosperms. Four, the foliar appendages of type I and II in Archaebuda are of distinct sizes and morphologies (Figure 3a–d) while lateral appendages (bract–scale–seed complexes) in conifer cones are either uniform or of a gradually transitional appearance (Figure S1b) [52,53,54,63,64]. All these differences culminate in the conclusion that Archaebuda is not a conifer cone, and that it represents a flower bud in the Early Cretaceous.
Due to intensive palaeobotanical studies [3,4,5,6,7,8,9,10,11,12,13,14,15], the great diversity of angiosperms in the Yixian Formation has been repeatedly underscored as various reproductive organs of angiosperms have been reported [3,4,5,69]. According to common sense in palaeontology, fragile parts of organisms have less potential to be preserved as fossils. This understanding has been a cornerstone of paleontological practice over past centuries. An implication of this is that fragile parts of plants, such as flowers, flower buds, and cytoplasm, are not expected in the fossil world. However, as palaeontology has developed, exceptions to this rule have frequently occurred. For example, reproductive organs of angiosperms (flowers) have been documented in the Yixian Formation [3,4,5,6,9,69], cellular ultrastructures and chloroplasts have been seen in Eocene Metasequoia [70], and even exocytosis snapshots have been observed in a Miocene conifer [71,72]. These exceptions remind us that, theoretically, fragile parts of plants can also be preserved in fossils. However, the reality is that fragile flower buds have been a rarity in the fossil record [73], especially in the Yixian Formation, which is famous worldwide for its diversity of angiosperms [3,4,5,6,7,8,9,10,11,12,13,14,15].
The numerous reproductive organs of angiosperms reported from the Yixian Formation [3,4,5,6,7,8,9,10,11,12,13,14,15] (except for Archaefructus) differ from each other morphologically, underscoring the great diversity of angiosperms in the Yixian Formation. Despite such a great diversity of angiosperms, hitherto there was no fossil record of flower buds in the Yixian Formation. None of the previously reported angiosperms in the formation has perianth, as Arachaefructus [3,4,5,8] and Sinocarpus [11,12] indicate. The present report of Archaebuda implies that flowers with perianth (as in most angiosperm flowers) occurred 125 Ma ago. This discovery is helpful to decouple the evolutionary history of flowers from that of angiosperms. The repeated popping up of new angiosperms in the Yixian Formation implies that angiosperms in the Early Cretaceous are still under-studied.
A Jurassic peer of Archaebuda, Florigerminis [73], seems to favor an earlier origin of angiosperms. However, both fossils are not permineralized and thus prevent more detailed discussion. Perhaps future application of Micro-CT or other new technology will help to reveal more internal and crucial information in better preserved fossils that will help palaeobotanists to make robust conclusions.

5. Conclusions

Despite various angiosperms reported from the Yixian Formation, until now, none of them has been a flower bud. Archaebuda reported here represents the debut of flower buds in the Early Cretaceous, indicating that flowers with a perianth did exist 125 Ma ago. This is a key contribution to the study of flower history.

Supplementary Materials

The following are available online at https://www.mdpi.com/article/10.3390/biology11111598/s1, Figure S1. Comparison between flower bud and coniferous cone.

Author Contributions

X.W. designed the research. L.-J.C. provided the fossil specimen. X.W. and L.-J.C. analysed the data and wrote the manuscript. All authors have read and agreed to the published version of the manuscript.

Funding

This research was supported by the Strategic Priority Research Program (B) of the Chinese Academy of Sciences (XDB26000000) and the National Natural Science Foundation of China (42288201, 41688103, 91514302).

Institutional Review Board Statement

This research involves no living animal/plant material and no conserved fossil materials.

Informed Consent Statement

Not applicable.

Acknowledgments

We thank Yan Fang for helping with the photography using SEM and Mike Pole for his help with English.

Conflicts of Interest

The authors declare no conflict of interest.

References

  1. Wieland, G.R. American Fossil Cycads; The Wilkens Sheiry Printing Co.: Washington, WA, USA, 1906; Volume 34, p. 295. [Google Scholar]
  2. Arber, E.A.N.; Parkin, J. On the origin of angiosperms. J. Linn. Soc. Lond. Bot. 1907, 38, 29–80. [Google Scholar] [CrossRef] [Green Version]
  3. Sun, G.; Dilcher, D.L.; Zheng, S.; Zhou, Z. In search of the first flower: A Jurassic angiosperm, Archaefructus, from Northeast China. Science 1998, 282, 1692–1695. [Google Scholar] [CrossRef] [PubMed]
  4. Sun, G.; Ji, Q.; Dilcher, D.L.; Zheng, S.; Nixon, K.C.; Wang, X. Archaefructaceae, a new basal angiosperm family. Science 2002, 296, 899–904. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  5. Ji, Q.; Li, H.; Bowe, M.; Liu, Y.; Taylor, D.W. Early Cretaceous Archaefructus eoflora sp. nov. with bisexual flowers from Beipiao, Western Liaoning, China. Acta Geol. Sin. (Engl. Ed.) 2004, 78, 883–896. [Google Scholar]
  6. Wang, X. The Dawn Angiosperms, 2nd ed.; Springer: Cham, Switzerland, 2018; p. 407. [Google Scholar]
  7. Duan, S. The oldest angiosperm—A tricarpous female reproductive fossil from western Liaoning Province, NE China. Sci. China D 1998, 41, 14–20. [Google Scholar] [CrossRef]
  8. Wang, X.; Zheng, X.-T. Reconsiderations on two characters of early angiosperm Archaefructus. Palaeoworld 2012, 21, 193–201. [Google Scholar] [CrossRef]
  9. Wang, X.; Shih, C.; Liu, Z.-J.; Lin, L.; Singh, K.J. Reconstructing the Callianthus plant–An early aquatic angiosperm from the Lower Cretaceous of China. Cretac. Res. 2021, 128, 104983. [Google Scholar] [CrossRef]
  10. Wang, X.; Zheng, S. The earliest normal flower from Liaoning Province, China. J. Integr. Plant Biol. 2009, 51, 800–811. [Google Scholar] [CrossRef]
  11. Leng, Q.; Friis, E.M. Sinocarpus decussatus gen. et sp. nov., a new angiosperm with basally syncarpous fruits from the Yixian Formation of Northeast China. Plant Syst. Evol. 2003, 241, 77–88. [Google Scholar] [CrossRef]
  12. Leng, Q.; Friis, E.M. Angiosperm leaves associated with Sinocarpus infructescences from the Yixian Formation (Mid-Early Cretaceous) of NE China. Plant Syst. Evol. 2006, 262, 173–187. [Google Scholar] [CrossRef]
  13. Han, G.; Fu, X.; Liu, Z.-J.; Wang, X. A new angiosperm genus from the Lower Cretaceous Yixian Formation, Western Liaoning, China. Acta Geol. Sin. (Engl. Ed.) 2013, 87, 916–925. [Google Scholar]
  14. Han, G.; Liu, Z.; Wang, X. A Dichocarpum-like angiosperm from the Early Cretaceous of China. Acta Geol. Sin. (Engl. Ed.) 2017, 90, 1–8. [Google Scholar]
  15. Han, G.; Wang, X. A new infructescence of angiosperms from the Early Cretaceous of China. Acta Geol. Sin. (Engl. Ed.) 2020, 94, 1711–1713. [Google Scholar] [CrossRef]
  16. Ren, D. Flower-associated Brachycera flies as fossil evidences for Jurassic angiosperm origins. Science 1998, 280, 85–88. [Google Scholar] [CrossRef]
  17. Yao, Y.; Cai, W.; Ren, D. Fossil flower bugs (Heteroptera: Cimicomorpha: Cimicoidea) from the Late Jurassic of Northeast China, including a new family, Vetanthocoridae. Zootaxa 2006, 1360, 1–40. [Google Scholar] [CrossRef]
  18. Liu, Y.; Sinitshenkova, N.D.; Ren, D. A new genus and species of stonefly (Insecta: Plecoptera) from the Yixian Formation, Liaoning Province, China. Cretac. Res. 2007, 28, 322–326. [Google Scholar] [CrossRef]
  19. Ren, D.; Shih, C.; Gao, T.; Yao, Y.; Zhao, Y. Silent Stories; Science Press: Beijing, China, 2010; p. 322. [Google Scholar]
  20. Gao, T.; Shih, C.; Rasnitsyn, A.P.; Xu, X.; Wang, S.; Ren, D. New transitional fleas from China highlighting diversity of Early Cretaceous ectoparasitic insects. Curr. Biol. 2013, 23, 1261–1266. [Google Scholar] [CrossRef] [Green Version]
  21. Teng, F.; Lü, J.; Wei, X.; Hsiao, Y.; Pittman, M. New material of Zhenyuanopterus (Pterosauria) from the Early Cretaceous Yixian Formation of western Liaoning. Acta Geol. Sin. (Engl. Ed.) 2014, 88, 1–5. [Google Scholar] [CrossRef]
  22. Ding, Q.H. Research on fossil wood from the Yixian Formation in western Liaoning Province, China. Acta Geol. Sin. (Engl. Ed.) 2000, 39, 209–219. [Google Scholar]
  23. Gao, T.; Ren, D. Description of a new fossil Anthoxyela species (Hymenoptera, Xyelidae) from Yixian Formation of Northeast China. Zootaxa 2008, 1842, 56–62. [Google Scholar] [CrossRef]
  24. Huang, D.-Y.; Nel, A. The first Chinese Tarsophlebiidae from the Lower Cretaceous Yixian Formation, with morphological and phylogenetic implications (Odonatoptera: Panodonata). Cretac. Res. 2009, 30, 429–433. [Google Scholar] [CrossRef]
  25. Huang, J.; Ren, D.; Sinitshenkova, N.D.; Shih, C. New genus and species of Hexagenitidae (Insecta: Ephemeroptera) from Yixian Formation, China. Zootaxa 2007, 1629, 39–50. [Google Scholar] [CrossRef]
  26. Lin, Q.B.; Huang, D.Y.; Nel, A. A new family of Cavilabiata from the Lower Cretaceous Yixian Formation, China (Odonata: Anisoptera). Zootaxa 2007, 1649, 59–64. [Google Scholar] [CrossRef]
  27. Liu, M.; Lu, W.; Ren, D. A new fossil mordellid (Coleoptera: Tenebrionoidea: Mordellidae) from the Yixian Formation of Western Liaoning Province, China. Zootaxa 2007, 1415, 49–56. [Google Scholar] [CrossRef]
  28. Liu, M.; Ren, D.; Shih, C. A new fossil weevil (Coleoptera, Curculionoidea, Belidae) from the Yixian Formation of western Liaoning, China. Prog. Nat. Sci. 2006, 16, 885–888. [Google Scholar]
  29. Liu, M.; Zhao, Y.Y.; Ren, D. Discovery of three new mordellids (Coleoptera, Tenebrionoidea) from the Yixian Formation of western Liaoning, China. Cretac. Res. 2008, 29, 445–450. [Google Scholar] [CrossRef]
  30. Liu, Y.; Ren, D.; Sinitshenkova, N.D.; Shih, C. Three new stoneflies (Insecta: Plecoptera) from the Yixian Formation of Liaoning, China. Acta Geol. Sin. (Engl. Ed.) 2008, 82, 249–256. [Google Scholar]
  31. Lü, J. A new boreopterid pterodactyloid pterosaur from the Early Cretaceous Yixian Formation of Liaoning Province, Northeastern China. Acta Geol. Sin. (Engl. Ed.) 2010, 84, 241–246. [Google Scholar] [CrossRef]
  32. Lü, J.; Kobayashi, Y.; Lee, Y.-N.; Ji, Q. A new Psittacosaurus (Dinosauria: Ceratopsia) specimen from the Yixian Formation of western Liaoning, China: The first pathological psittacosaurid. Cretac. Res. 2007, 28, 272–276. [Google Scholar] [CrossRef]
  33. Wang, X.; Kellner, A.W.A.; Zhou, Z.; de Almeida Campos, D. A new pterosaur (Ctenochasmatidae, Archaeopterodactyloidea) from the Lower Cretaceous Yixian Formation of China. Cretac. Res. 2007, 28, 245–260. [Google Scholar] [CrossRef]
  34. Wang, X.; Ren, D.; Wang, Y. First discovery of angiospermous pollen from Yixian Formation. Acta Geol. Sin. (Engl. Ed.) 2000, 74, 265–272. [Google Scholar]
  35. Zhang, H.; Rasnitsyn, A.P.; Wang, D.; Zhang, Y. Some hatchet wasps (Hymenoptera, Evaniidae) from the Yixian Formation of western Liaoning, China. Cretac. Res. 2007, 28, 310–316. [Google Scholar] [CrossRef]
  36. Zheng, S.; Li, N.; Li, Y.; Zhang, W.; Bian, X. A new genus of fossil cycads Yixianophyllum gen. nov. from the Late Jurassic Yixian Formation, Western Liaoning, China. Acta Geol. Sin. (Engl. Ed. ) 2005, 79, 582–592. [Google Scholar]
  37. Ding, Q.-H.; Zhang, L.-D.; Guo, S.-Z.; Zhang, C.-J.; Peng, Y.-D.; Jia, B.; Chen, S.-W.; Xing, D.-H. The stratigraphic sequence and fossil-bearing horizon of the Yixian Formation in western Liaoning, China. Geol. Resour. 2001, 10, 193–198. [Google Scholar]
  38. Li, J.; Batten, D.J. Palynological evidence of an Early Cretaceous age for the Yixian Formation at Sihetun, western Liaoning, China. Cretac. Res. 2007, 28, 333–338. [Google Scholar] [CrossRef]
  39. Li, Y.; Sha, J.; Wang, Q.; Chen, S. Lacustrine tempestite litho- and biofacies in the Lower Cretaceous Yixian Formation, Beipiao, western Liaoning, northeast China. Cretac. Res. 2007, 28, 194–198. [Google Scholar] [CrossRef]
  40. Peng, Y.-D.; Zhang, L.-D.; Chen, W.; Zhang, C.-J.; Guo, S.-Z.; Xing, D.-H.; Jia, B.; Chen, S.-W.; Ding, Q.-H. 40Ar/39Ar and K-Ar dating of the Yixian Formation volcanic rocks, western Liaoning province, China. Geochimca 2003, 32, 427–435. [Google Scholar]
  41. Swisher, C.C.; Wang, Y.; Wang, X.; Xu, X.; Wang, Y. 40Ar/39Ar dating of the lower Yixian Fm, Liaoning Province, northeastern China. Chin. Sci. Bull. 1998, 43, 125. [Google Scholar] [CrossRef]
  42. Wang, W.; Zhang, H.; Zhang, L.; Zheng, S.; Yang, F.; Li, Z.; Zheng, Y.; Ding, Q. Standard Sections of Tuchengzi Stage and Yixian Stage and their Stratigraphy, Palaeontology and Tectonic-Volcanic Actions; Geological Publishing House: Beijing, China, 2004; p. 514. [Google Scholar]
  43. Wang, W.L.; Zhang, L.J.; Zheng, S.L.; Ren, D.; Zheng, Y.J.; Ding, Q.H.; Zhang, H.; Li, Z.T.; Yang, F.L. The age of the Yixianian stage and the boundary of Jurassic-Cretaceous, --- the establishment and study of stratotype of the Yixianian stage. Geol. Rev. 2005, 51, 234–242. [Google Scholar]
  44. Xing, D.H.; Sun, C.L.; Sun, Y.W.; Zhang, L.D.; Peng, Y.D.; Chen, S.W. New knowledge on Yixian Formation. Acta Geosci. Sin. 2005, 26, 25–30. [Google Scholar]
  45. Zhang, L.; Gong, E.; Xu, D.; Liu, X.; Li, J. Sedimentary facies of the Yixian Formation of Lower Cretaceous in Sihetun Basin of Beipiao, Liaoning Province. J. Palaeogeogr. 2005, 7, 70–78. [Google Scholar]
  46. Zhang, L.D.; Jin, C.Z.; Guo, S.Z.; Zhang, C.J.; Peng, Y.D.; Chen, S.W.; Xing, D.H.; Ding, Q.H.; Zheng, Y.J. The precious fossil-bearing beds of Yixian Formationin Beipiao-Yixian area: Their ages and corelation. Geol. Resour. 2004, 13, 193–221. [Google Scholar]
  47. Dilcher, D.L.; Sun, G.; Ji, Q.; Li, H. An early infructescence Hyrcantha decussata (comb. nov.) from the Yixian Formation in northeastern China. Proc. Natl. Acad. Sci. USA 2007, 104, 9370–9374. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  48. Taylor, T.N.; Taylor, E.L.; Krings, M. Paleobotany: The Biology and Evolution of Fossil Plants, 2nd ed.; Elsevier: Amsterdam, The Netherlands, 2009; p. 1230. [Google Scholar]
  49. Bierhorst, D.W. Morphology of Vascular Plants; Macmillan Company: New York, NY, USA, 1971. [Google Scholar]
  50. Martens, P. Les Gnetophytes; Gebrueder Borntraeger: Berlin, Germany, 1971. [Google Scholar]
  51. Chamberlain, C.J. Gymnosperms, Structure and Evolution; Johnson Reprint Corporation: New York, NY, USA, 1957. [Google Scholar]
  52. Escapa, I.H.; Gandolfo, M.A.; Crepet, W.L.; Nixon, K.C. A new species of Athrotaxites (Athrotaxoideae, Cupressaceae) from the Upper Cretaceous Raritan Formation, New Jersey, USA. Botany 2016, 94, 831–845. [Google Scholar] [CrossRef]
  53. Jagel, A.; Dörken, V.M. Morphology and morphogenesis of the seed cones of the Cupressaceae—part I: Cunninghamioideae, Athrotaxoideae, Taiwanioideae, Sequoioideae, Taxodioideae. Bull. Cupressus Conserv. Proj. 2014, 3, 117–136. [Google Scholar]
  54. Andruchow-Colombo, A.; Gandolfo, M.A.; Escapa, I.H.; Cúneo, N.R. New genus of Cupressaceae from the Upper Cretaceous of Patagonia (Argentina) fills a gap in the evolution of the ovuliferous complex in the family. J. Syst. Evol. 2022. [Google Scholar] [CrossRef]
  55. Chamberlain, C.J. The Living Cycads; Hafner Publishing Company: New York, NY, USA, 1919; p. 172. [Google Scholar]
  56. Chamberlain, C.J. The living cycads and phylogeny of seed plants. Am. J. Bot. 1920, 7, 146–153. [Google Scholar] [CrossRef]
  57. Chen, T.; Wang, D.; Liao, J.; Yang, Q.; Wu, Q.; Chen, Z. Morphology and anatomy on Cycas in China, chapter 5. In Cycads in China; Wang, D., Liang, H., Chen, T., Wang, D., Eds.; Guangdong Science AND Technology Press: Guangzhou, China, 1996; pp. 143–189. [Google Scholar]
  58. Cycads of China; Guan, Z.; Zhou, L. (Eds.) Sichuan Science and Technology Publisher: Chengdu, China, 1996; p. 242. [Google Scholar]
  59. Harris, T.M. The fossil cycads. Palaeontology 1961, 4, 313–323. [Google Scholar]
  60. Wieland, G.R. American Fossil Cycads; Carnegie Institution of Washington: Washington, WA, USA, 1916; Volume 34 (II). [Google Scholar]
  61. Rothwell, G.W.; Stockey, R.A. Independent evolution of seed enclosure in the bennettitales: Evidence from the anatomically preserved cone Foxeoidea connatum gen. et sp. nov. In Plants in the Mesozoic Time: Innovations, Phylogeny, Ecosystems; Gee, C.T., Ed.; Indiana University Press: Bloomington, IN, USA, 2010; pp. 51–64. [Google Scholar]
  62. Rothwell, G.W.; Crepet, W.L.; Stockey, R.A. Is the anthophyte hypothesis alive and well? New evidence from the reproductive structures of Bennettitales. Am. J. Bot. 2009, 96, 296–322. [Google Scholar] [CrossRef]
  63. Eckenwalder, J.E. Conifers of the World, the Complete Reference; Timber Press: Portland, OR, USA, 2009. [Google Scholar]
  64. Jagel, A.; Dörken, V.M. Morphology and morphogenesis of the seed cones of the Cupressaceae—part II: Cupressoideae. Bull. Cupressus Conserv. Proj. 2015, 4, 51–78. [Google Scholar]
  65. Farjon, A. A Monograph of Cupressaceae and Sciadopitys; Royal Botanic Gardens: Kew, Australia, 2005. [Google Scholar]
  66. Farjon, A.; Styles, B.T. Pinus (Pinaceae); New York Botanical Garden: New York, NY, USA, 1997; Volume 75. [Google Scholar]
  67. Wang, X.; Xu, X. Morphology of Juniperus cone and its implications on cone evolution. J. Morphol. Anat. 2021, 5, 1–4. [Google Scholar]
  68. Jain, K.K. Morphology of female cone in Pinaceae. Phytomorphology 1976, 26, 189–200. [Google Scholar]
  69. Wang, X. A novel Early Cretaceous flower and its implications on flower derivation. Biology 2022, 11, 1036. [Google Scholar] [CrossRef] [PubMed]
  70. Schoenhut, K.; Vann, D.R.; LePage, B.A. Cytological and ultrastructural preservations in Eocene Metasequoia leaves from the Canadian High Arctic. Am. J. Bot. 2004, 91, 816–824. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  71. Wang, X.; Liu, W.; Du, K. Palaeontological evidence of membrane relationship in step-by-step membrane fusion. Mol. Membr. Biol. 2011, 28, 115–122. [Google Scholar] [CrossRef] [Green Version]
  72. Wang, X.; Liu, W.; Cui, J.; Du, K. Palaeontological evidence for membrane fusion between a unit membrane and a half-unit membrane. Mol. Membr. Biol. 2007, 24, 496–506. [Google Scholar] [CrossRef]
  73. Cui, D.-F.; Hou, Y.; Yin, P.; Wang, X. A Jurassic flower bud from China. Geol. Soc. Lond. Spec. Publ. 2022, 521, 81–93. [Google Scholar] [CrossRef]
Figure 1. Geographical information of the fossil locality for Archaebuda gen. nov, Dawangzhangzi, Lingyuan, Liaoning, China. Reproduced from Han et al. [14], with permission and courtesy of Acta Geologica Sinica (English edition). Left. Fossil locality (black dot) in northeastern China. Right. Detailed position of fossil locality (red star) in a suburb of the city Lingyuan, Liaoning.
Figure 1. Geographical information of the fossil locality for Archaebuda gen. nov, Dawangzhangzi, Lingyuan, Liaoning, China. Reproduced from Han et al. [14], with permission and courtesy of Acta Geologica Sinica (English edition). Left. Fossil locality (black dot) in northeastern China. Right. Detailed position of fossil locality (red star) in a suburb of the city Lingyuan, Liaoning.
Biology 11 01598 g001
Figure 2. The holotype of Archaebuda gen. nov. and its details. (a) The general view of the specimen, including a stalk and a flower bud. Bar = 10 mm. (b) Detailed view of the bud composed of various overlapping patches. Bar = 5 mm. (c) Sketch of the bud in Figure 2b. Parts marked by letters (b, c, d) are shown in Figure 3a. (d) Basal portion of the flower bud. Bar = 1 mm. (e) Detailed view of the scaly leaf with cellular details on the pedicel. Bar = 1 mm. (f) SEM view of the portion in Figure 2e, showing the longitudinal arrangement of the cells. Bar = 1 mm.
Figure 2. The holotype of Archaebuda gen. nov. and its details. (a) The general view of the specimen, including a stalk and a flower bud. Bar = 10 mm. (b) Detailed view of the bud composed of various overlapping patches. Bar = 5 mm. (c) Sketch of the bud in Figure 2b. Parts marked by letters (b, c, d) are shown in Figure 3a. (d) Basal portion of the flower bud. Bar = 1 mm. (e) Detailed view of the scaly leaf with cellular details on the pedicel. Bar = 1 mm. (f) SEM view of the portion in Figure 2e, showing the longitudinal arrangement of the cells. Bar = 1 mm.
Biology 11 01598 g002
Figure 3. Details of Archaebuda gen. nov under SEM, except Figure 3c. (a) Detailed view of the tip of the flower bud, showing at least three overlapping papery foliar appendages of type II (1,2, 3, corresponding to d, c, b in Figure 2c) with differently oriented textures. Bar = 1 mm. (b) Detailed view of the rectangle in Figure 3a, showing three layers of overlapping papery foliar appendages of type II (1, 2, 3). SEM. Bar = 0.5 mm. (c) Stereomicroscopic view of a keeled foliar appendage of type I at the base of the flower bud. Bar = 1 mm. (d) SEM image of the foliar appendage of type I shown in Figure 3c, showing surface texture. Bar = 1 mm.
Figure 3. Details of Archaebuda gen. nov under SEM, except Figure 3c. (a) Detailed view of the tip of the flower bud, showing at least three overlapping papery foliar appendages of type II (1,2, 3, corresponding to d, c, b in Figure 2c) with differently oriented textures. Bar = 1 mm. (b) Detailed view of the rectangle in Figure 3a, showing three layers of overlapping papery foliar appendages of type II (1, 2, 3). SEM. Bar = 0.5 mm. (c) Stereomicroscopic view of a keeled foliar appendage of type I at the base of the flower bud. Bar = 1 mm. (d) SEM image of the foliar appendage of type I shown in Figure 3c, showing surface texture. Bar = 1 mm.
Biology 11 01598 g003
Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Share and Cite

MDPI and ACS Style

Chen, L.-J.; Wang, X. A Flower Bud from the Lower Cretaceous of China. Biology 2022, 11, 1598. https://doi.org/10.3390/biology11111598

AMA Style

Chen L-J, Wang X. A Flower Bud from the Lower Cretaceous of China. Biology. 2022; 11(11):1598. https://doi.org/10.3390/biology11111598

Chicago/Turabian Style

Chen, Li-Jun, and Xin Wang. 2022. "A Flower Bud from the Lower Cretaceous of China" Biology 11, no. 11: 1598. https://doi.org/10.3390/biology11111598

Note that from the first issue of 2016, this journal uses article numbers instead of page numbers. See further details here.

Article Metrics

Back to TopTop