Skip to main content
Heliyon logoLink to Heliyon
. 2024 Nov 28;10(23):e40794. doi: 10.1016/j.heliyon.2024.e40794

The first macrofossil record of parasitic plant flowers from an Eocene Baltic amber

Weijia Huang a, Wenzhe Liu b, Xin Wang c,
PMCID: PMC11648213  PMID: 39687097

Abstract

Parasitic plants left little trace in the macrofossil record, making their evolutionary history mysterious. Baltic amber and other fossil lagerstätts have provided plenty of angiosperm fossils, there are only three reports of fossil leaves (cf. Schoepfia republicensis and Schoepfia sp. 1) related to Schoepfiaceae until now, making many hypotheses related to its evolution untested. Here we report a fossil corolla and stamens of a probable schoepfiaceous flower (Schoepfiaceae, Santalales) from late Eocene (37.8–33.9 Ma ago) of Kaliningrad, Russia. Unlike previously reported flowers, the new fossil is characterized by its five fused petals bearing adnate stamens. This character assemblage points to an affinity of Schoepfiaceae. This is the debut of schoepfiaceous flower in the macrofossil record, shedding a new light on the evolution of this poorly understood family. Its unexpected occurrence in Russia adds information to the discussion on the history of Schoepfiaceae.

Keywords: Flower, Corolla, Schoepfiaceae, Amber, Eocene, Kaliningrad, Russia


Although early angiosperms have been abundantly documented [[1], [2], [3], [4], [5], [6], [7], [8], [9], [10], [11], [12], [13], [14], [15], [16], [17]], there are still many lacunae in our understanding of angiosperm evolution. For example, due to their special habit, parasitic plants (especially their flowers) are rarely reported in the fossil record. Schoepfiaceae, a family now restricted to the Neotropical (20 species) [18] and southeast Asia (4 species) [18,19], have very limited macrofossil record: only 9 pieces of leaves from the Eocene (38–55.8 Ma) of Northwest USA (cf. Schoepfia republicensis) [20,21] and 1 piece of leaf (Schoepfia sp. 1) from the Miocene-Pliocene (5.3–11.6 Ma) of Southwest China [22] have been reported until now, while their flowers are completely lacking in the fossil record. Such a lack of macrofossil data makes the evolution and history of Schoepfiaceae elusive. Here we report a new fossil taxon, Schoepfioides kaliningradensis gen. et sp. nov (including corolla and adnate stamens), from the late Eocene (37.8–33.9 Ma ago) of Kaliningrad, Russia. The unique morphology of Schoepfioides compares itself best with Schoepfia, a genus in the parasitic family Schoepfiaceae (Santalales). Thus it can be determined that our fossil represents the debut of schoepfiaceous flower in the current macrofossil record, and will add much to our understanding of this poorly understood family.

The fossil material was uncovered from an outcrop of the Blue Earth near Yantarny Village, Samland Peninsula, Kaliningrad, Russia (54°52´22″N, 19°56´26″E) in 2015. The studied specimen was preserved three dimensionally in a brownish amber. Various works [[23], [24], [25], [26], [27], [28], [29], [30]] suggest a late Eocene age (37.8–33.9 Ma) for the amber enclosing the fossil. It was observed and photographed using a Nikon SMZ1500 stereomicroscope with a DS-Fi1 digital camera housed at the Nanjing Institute of Geology and Palaeontology, Nanjing, China. Micro-CT observation was performed using a Zeiss Xradia 520 versa X-ray microscope housed at the Nanjing Institute of Geology and Palaeontology, Nanjing, China. The three dimensional reconstruction and virtual sections were generated using VG Studio MAX 3.0. All figures were organized for publication using a Photoshop 7.0.

Eudicots

Santalales

Schoepfiaceae

Schoepfioides gen. nov

Diagnosis: Corolla tubular, campanulate, with 5 triangular reflexing lobes. Five epipetalous stamens, dorsifixed, bilocular, with a hair tuft between stame and petal, adnated to the middle of the petals. Filament short.

Type species: Schoepfioides kaliningradensis gen. et sp. nov.

Etymology: Schoepfioides-for its close resmblance to extant plant Schoepfia.

Type horizon: The Priabonian, late Eocene (37.8–33.9 Ma).

Type locality: Yantarny Village, Samland Peninsula, Kaliningrad, Russia (54°52´22″N, 19°56´26″E).

Schoepfioides kaliningradensis gen. et sp. nov

Fig. 1, Fig. 2

Fig. 1.

Fig. 1

General view and details of Schoepfioides kaliningradensis gen. et sp. nov.

a. Top view of the corolla. Note one (arrow) of the stamens. Scale bar = 1 mm

b. An oblique top view of the corolla, showing five relfexing lobes. Scale bar = 1 mm.

c. Adaxial view of a petal and its epipetalous stamen (arrow). Note the post-staminal hair tuft. Scale bar = 1 mm

d. A reflexing lobe and its epipetalous stamen (arrow). Scale bar = 1 mm.

e. Acuicular epidermal trichomes on a petal surface. Scale bar = 0.5 mm.

f. A hair tuft associated with a stamen (fallen off). Scale bar = 0.5 mm.

Fig. 2.

Fig. 2

Micro-CT virtual sections of the corolla.

a. Side view of the corolla, showing four preserved epipetalous stamens, each of which is supported by a vein running through the whole length of the petal (arrow). Scale bar = 1 mm

b. Bottom view of the corolla, showing the deployment of five petal lobes and an elongated oval hole (central) at the corolla bottom. Scale bar = 1 mm.

c. Adaxial view of petal lobe and its epipetalous stamen (arrow). Scale bar = 1 mm

d. Cross view of the epipetalous stamen in Fig. 2e–f, showing its dorsal short filament (arrow) and two locules. Scale bar = 0.2 mm.

e. Side view of the epipetalous stamen in Fig. 2h, showing its short dorsal filament (arrow). Scale bar = 1 mm.

f. Adaixal view of the stamen shown in Fig. 2h, showing its apical connective and two locules. Scale bar = 1 mm

g. Adaxial view of petal and its epipetalous stamen (arrow). Scale bar = 0.2 mm

h. Side view of a petal, showing reflexing lobe and its epipetalous stamen (arrow). Scale bar = 0.2 mm.

i. Oval cross view of the corolla (near the top), showing fused petals and two reflexing petal lobes (top). Scale bar = 1 mm.

j. Cross view of the corolla (near the bottom), showing five fused petals (arrows). Scale bar = 1 mm

k. A reflexed petal tip. Scale bar = 0.5 mm

l. Side view of a petal lobe, showing reflexed tip and epipetalous stamen (arrow). Scale bar = 0.2 mm

m. Cross view of a petal, showing epipetaous stamen (arrow) adnated to the petal. Scale bar = 0.5 mm.

Diagnosis: the same as the genus.

Description: A single flower corolla is preserved (Fig. 1, Fig. 2a-b). The corolla is campanulate in form, 5.7 mm long (Fig. 1, Fig. 2a-b). Oval in cross view, 4.5 mm × 4 mm (Fig. 2b–i). There are five triangular lobes on the top of the corolla tube (Fig. 1, Fig. 2g-h, k). The lobes are triangular in shape, reflexing, measuring 2.6 mm long and 1.7 mm wide at the base (Fig. 1, Fig. 2a-b). On the middle of each lobe there is an epipetalous stamen, behind which is a tuft of hairs (Fig. 1, Fig. 2a-b, g-h, l-m). Each stamen has a 0.17 mm-long filament, two locules, and a pointed connective (Fig. 1, Fig. 2a-h, l-m). Each anther is 1.4 mm long, 0.48 mm wide, 0.37 mm thick, and the connective is about 0.2 mm long (Fig. 1, Fig. 2c-f, l-m).

Etymology: kaliningradensis for the fossil locality Kaliningrad, Russia.

Holotype: BMM5586.

Depository: the Blue Miracle Museum Science Research Studio, Guangzhou, China.

Remarks: Corolla with epipetalous stamens, especially those with a post-staminal hair tuft, are present in families of Santalales. For example, stamens adnate to the corolla base in Loranthaceae [31]. However, stamens in Loranthaceae lack an associated hair tuft, adnate to the base (rather than top) of the corolla, and have basifixed anther [31]. These constitute a strong contrast against Schoepfiaceae, stamens of which have an associated tuft of hairs, adnate to the top (rather than base) of the corolla, and have dorsalifixed anther [31]. These characters support the identification of the fossil flower as an extinct member of Schoepfiaceae.

Discussion

Comparison of Schoepfioides kaliningradensis with extant species of Schoepfia The Schoepfiaceae (Santalales) is a small family of parasitic angiosperms, consisting of about 50 species endemic to South America and Asia, living in moist habitat such as high elevation cloud forests [18,19]. This family was named after Dr. David Schoepf, a German botanist. This small family is a sister of two more diverse, widespread, parasitic families, Misodendraceae and Loranthaceae [[31], [32], [33]]. Flowers in Misodendraceae have apetalous or 3 petals, while flowers of Loranthaceae have a connate perianth of 3 or 5 lobes with adnate slender-filamented anthers [31,32], and thus both are distinct from Schoepfiaceae, in which the flowers have 5-lobeed perianth with adnate stout-filamented stamens opposite to petals. As a parasitic family, plants in Schoepfiaceae rely on other plants to obtain nutrients, thus having little potential to be fossilized. Until now there are only three reports of total ten pieces of leaves related to Schoepfiaceae [[20], [21], [22]], making the evolution and history of Schoepfiaceae poorly understood.

The post-staminal hair tuft in Schoepfioides kaliningradensis (Fig. 1c) is a feature never seen in the fossil record. The occurrence of this feature appears to be very informative as hairs behind the anthers are commonly considered a feature characteristic of Santalaceae, although they occur elsewhere infrequently [32]. According to the diagnosis of Schoepfiaceae, “petals (4)5(6), united for most of their length to form a cylindrical to subcampanulate corolla, the limbs spreading or recurved at anthesis; stamens as many as the petals and connate with them at the latter's middle, opposite the petals, each associated with a post-staminal hair tuft; filaments as long as the ovoid, dorsifixed, biloculate anthers that are placed at the flower's mouth” [32], and they can be verified in extant Schoepfia flowers (Fig. 3a–c). Almost all these features occur in the fossil specimen of Schoepfioides kaliningradensis (Fig. 1, Fig. 2a-m). This observation suggests that Schoepfioides kaliningradensis represents a flower of Schoepfiaceae, which has never been seen in the macrofossil record so far, especially at this early age (late Eocene). Although there are two other genera (Arjona and Quinchamalium), frequently placed in the Schoepfiaceae, these two genera distinguish themselves from the fossil flower by their different corolla forms and longer petal lobes [18,33].

Fig. 3.

Fig. 3

Flowers of Schoepfia jasminodora Sieb. & Zucc. and their details.

a. Several flowers of various developmental stages in an infructescence.

b. Side view of a flower showing connate petals and reflexing lobes.

c. Oblique top view of a flower showing five stamens (dark dots) adnate to the petals and a hair tuft (black triangle) asscoaited with a stamen.

Palaeogeography and Evolution Extant Schoepfiaceae is a poorly understood family restricted to America (20 species in Mesoamerica, Caribbean, Argentina, Bolivia, and Peru) and Asia (4 species in India, Malesia, China) (Fig. 4) [18,19,32,34]. The family is frequently regarded as related to Misodendroaceae and Loranthaceae [[31], [32], [33]]. Although there are some fossil of Santalales, most of them are restricted to pollen records the significance of which is “compromised by intrageneric polymorphism and convergence” [33]. Fortunately, some macrofossil records are found related to Schoepfia, leaves from the Eocene (38–55.8 Ma) of Northwest USA [20,21] and from the Miocene-Pliocene of Southwest China [22] (Fig. 4). Such extant and past geographical distributions are debatable topics for botanists: While extant center of diversity (Fig. 4) appears to suggest a southern hemisphere origin for the family, which was also favored by molecular analysis [33], the present reported occurrence of flower corolla and stamens indicate that Schoepfiaceae have existed in Kaliningrad, Russia by the late Eocene. It is possible Schoepfiaceae may migrate from their Eocene center of diversity in North America and west Europe, to their extant diversity center in South America and Asia (the latter has their Miocene fossil record [22] and a few extant species). Although we have limited fossils of Schoepfiaceae currently, it appears that the Southern hemisphere origin of Schoepfiaceae suggested previously [33] should be reconsidered, especially when more fossil information is available in the future.

Fig. 4.

Fig. 4

Global distribution of Schoepfia (red) and the fossil locality of Schoepfioides kaliningradensis gen. et sp. nov. in Kaliningrad, Russia (blue dot), two previous fossil localities in NW USA and SW China (blue squares).

Origin of Parasitism The occurrence of Schoepfioides kaliningradensis raises new questions concerning the origin and evolution of parasitism. Haustorial parasitism occurs in 270 genera (>4500 species) of angiosperms [33]. Extant Schoepfiaceae is known to be root parasitic [33]. However, it is unknown when they became parasitic, before or after the age of Schoepfioides kaliningradensis, which we now compare with Schoepfiaceae. Considering the relatively longer history of Schoepfiaceae among Santatales [33], it is possible that Schoepfioides kaliningradensis was not parasitic yet. If really so, then parasitism in Schoepfiaceae should occur after the age of Schoepfioides kaliningradensis (late Eocene), but one question rises, exactly when it occurred. In the meanwhile, if Schoepfioides kaliningradensis were parasitic, then parasitism in Schoepfiaceae should have occurred before the age of Schoepfioides kaliningradensis (late Eocene), and again we will face exactly the same question. We hope future fossil discoveries will help to answer this question.

CRediT authorship contribution statement

Weijia Huang: Writing – review & editing, Writing – original draft. Wenzhe Liu: Writing – review & editing, Writing – original draft. Xin Wang: Writing – review & editing, Writing – original draft.

Data availability

Data included in article is referenced in the article.

Ethics declaration

Review and approval by an ethics committee or informed consent was not required for this study because it did not involve human subjects or laboratory experiments.

Funding

This research was supported by the National Natural Science Foundation of China (42288201).

Declaration of competing interest

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Acknowledgments

We thank Mr. Suping Wu for her help with Micro-CT.

References

  • 1.Wang X. second ed. Springer; Cham, Switzerland: 2018. The Dawn Angiosperms; p. 407. [Google Scholar]
  • 2.Wang X. In: Evolutionary Biology: Concept, Modeling and Application. Pontarotti P., editor. Springer-Verlag; Berlin: 2009. New fossils and new hope for the origin of angiosperms; pp. 51–70. [Google Scholar]
  • 3.Wang X. Schmeissneria: an angiosperm from the early jurassic. J. Systemat. Evol. 2010;48(5):326–335. [Google Scholar]
  • 4.Wang X., et al. Schmeissneria: a missing link to angiosperms? BMC Evol. Biol. 2007;7:14. doi: 10.1186/1471-2148-7-14. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 5.Fu Q., et al. An unexpected noncarpellate epigynous flower from the Jurassic of China. Elife. 2018;7 doi: 10.7554/eLife.38827. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 6.Fu Q., et al. Nanjinganthus is an angiosperm, isn't it? China Geology. 2020;3(3):359–361. [Google Scholar]
  • 7.Han G., et al. A whole plant herbaceous angiosperm from the Middle Jurassic of China. Acta Geol. Sin. 2016;90(1):19–29. [Google Scholar]
  • 8.Liu Z.-J., Wang X. A perfect flower from the Jurassic of China. Hist. Biol. 2016;28(5):707–719. doi: 10.1080/08912963.2015.1020423. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 9.Liu Z.-J., Wang X. Yuhania: a unique angiosperm from the middle jurassic of inner Mongolia, China. Hist. Biol. 2017;29(4):431–441. doi: 10.1080/08912963.2016.1178740. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 10.Hochuli P.A., Feist-Burkhardt S. A boreal early cradle of angiosperms? angiosperm-like pollen from the Middle Triassic of the Barents Sea (Norway) J. Micropalaeontol. 2004;23:97–104. [Google Scholar]
  • 11.Hochuli P.A., Feist-Burkhardt S. Angiosperm-like pollen and afropollis from the middle triassic (Anisian) of the germanic basin (Northern Switzerland) Front. Plant Sci. 2013;4:344. doi: 10.3389/fpls.2013.00344. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 12.Prasad V., et al. Late Cretaceous origin of the rice tribe provides evidence for early diversification in Poaceae. Nat. Commun. 2011;2:480. doi: 10.1038/ncomms1482. [DOI] [PubMed] [Google Scholar]
  • 13.Wu Y., You H.-L., Li X.-Q. Dinosaur-associated poaceae epidermis and phytoliths from the early cretaceous of China. Natl. Sci. Rev. 2018;5:721–727. [Google Scholar]
  • 14.Friis E.M., Crane P.R., Pedersen K.R. Cambridge University Press; Cambridge: 2011. The Early Flowers and Angiosperm Evolution; p. 596. [Google Scholar]
  • 15.Fu Q., et al. Micro-CT results exhibit ovules enclosed in the ovaries of Nanjinganthus. Sci. Rep. 2023;13:426. doi: 10.1038/s41598-022-27334-0. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 16.Han L., et al. New fossil evidence suggests that angiosperms flourished in the Middle Jurassic. Life. 2023;13(3):819. doi: 10.3390/life13030819. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 17.Wang X., Fu Q. Taiyuanostachya: an abominable angiosperm from the early permian of China. Journal of Biotechnology and Biomedicine. 2023;6(3):371–379. [Google Scholar]
  • 18.Farroñay F., et al. A new record and emended description of a rare Amazonian white-sand species: Schoepfia clarkii (Schoepfiaceae) Brittonia. 2019;71:312–317. [Google Scholar]
  • 19.Wu Z.-Y., et al. Science Press; Beijing: 2003. The Families and Genera of Angiosperms in China, A Comprehensive Analysis; p. 1209. [Google Scholar]
  • 20.Wolfe J.A., Wehr W.C. vol. 1597. U.S. Geological Survey Bulletin; 1987. pp. 1–25. (Middle Eocene Dicotyledonous Plants from Republic, Northeastern Washington). [Google Scholar]
  • 21.Wilf P. Late Paleocene-ealry Eocene climate climate changes in southwestern Wyoming: paleobotanical analysis. GSA Bulletin. 2000;112(2):292–307. [Google Scholar]
  • 22.Jacques F.M.B., et al. Quantitative reconstruction of the Late Miocene monsoon climates of southwest China: a case study of the Lincang flora from Yunnan Province. Palaeogeogr. Palaeoclimatol. Palaeoecol. 2011;304:318–327. [Google Scholar]
  • 23.Sivkov V.V., Zhamoida V.A. In: Terrestrial and Inland Water Environment of the Kaliningrad Region. Gritsenko V.A., et al., editors. 2017. Amber deposits in the Kaliningrad region; pp. 33–44. [Google Scholar]
  • 24.Sadowski E.-M., Hammel J.U., Denk T. Synchrotron X-ray imaging of a dichasium cupule of Castanopsis from Eocene Baltic amber. Am. J. Bot. 2018;105(12):2025–2036. doi: 10.1002/ajb2.1202. [DOI] [PubMed] [Google Scholar]
  • 25.Cai C., et al. First fossil jacobsoniid beetle (Coleoptera): derolathrus groehni n. sp. from Eocene Baltic amber. J. Paleontol. 2016;89(5):762–767. [Google Scholar]
  • 26.Weitschat W., Wichard W. In: Biodiversity of Fossils in Amber from the Major World Deposits. Penny D., editor. 2010. Baltic amber; pp. 80–115. [Google Scholar]
  • 27.Seyfullah L.J., et al. The Carnian Pluvial Episode and the first global appearance of amber. J. Geol. Soc. 2018;93(3):1684–1714. [Google Scholar]
  • 28.Bukejs A., Moseyko A.G., Alekseev V.I. Morphological and organic spectroscopic studies of a 44-million-year-old leaf beetle (Coleoptera: Chrysomelidae) in amber with endogenous remains of chitin. Sci. Rep. 2023;35(10):1771–1777. doi: 10.1038/s41598-023-32557-w. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 29.Sadowski E.-M., et al. Sciadopotys cladodes from Eocene baltic amber. Bot. J. Linn. Soc. 2016;180(2):258–268. [Google Scholar]
  • 30.Sadowski E.-M., et al. Carnivorous leaves from Baltic amber. Proc. Natl. Acad. Sci. USA. 2014;112(1):190–195. doi: 10.1073/pnas.1414777111. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 31.Apg A.P.G.I.V. An update of the Angiosperm Phylogeny Group classification for the orders and families of flowering plants. Bot. J. Linn. Soc. 2016;181(1):1–20. [Google Scholar]
  • 32.Kuijt J., Hansen B. In: Kubitzki K., editor. vol. XII. Springer-Verlag; Berlin: 2014. Flowering plants. Eudicots, Santalales, balanophorales; p. 213. (The Families and Genera of Vascular Plants). [Google Scholar]
  • 33.Vidal-Russell R., Nickrent D.L. The first mistletoes: origins of aerial parasitism in Santalales. Mol. Phylogenet. Evol. 2008;47(2):523–537. doi: 10.1016/j.ympev.2008.01.016. [DOI] [PubMed] [Google Scholar]
  • 34.Wu Z.-Y., et al. Science Press; Beijing: 2003. The Families and Genera of Angiosperms in China, A Comprehensive Analysis. [Google Scholar]

Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Data Availability Statement

Data included in article is referenced in the article.


Articles from Heliyon are provided here courtesy of Elsevier

RESOURCES