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Unravelling the palaeobiogeographical history of the living fossil genus Rehderodendron (Styracaceae) with fossil and extant pollen and fruit data



The relict genus Rehderodendron (Styracaceae), the species of which are restricted to mostly warm temperate to tropical climate in East Asia today, is known from fossil fruits and pollen in Europe during warmer periods from the lower Eocene to Pliocene. To infer which extant species are most closely related to the fossils, new data of pollen and fruit morphologiesy of six extant species, and additional new data of fossil pollen and previously described fossil fruits of Rehderodendron, are compared.


Both fossil pollen and fruits resemble a morphological mixture of the extant species R. indochinense, R. kwantungense, R. macrocarpum, and R. microcarpum, thus implying that these extant taxa and the fossil European taxa represent an old Eurasian lineage, whereas the pollen and fruit morphology of the extant R. kweichowense and R. truongsonense differ considerably from the fossils and other extant species investigated, and are considered to have evolved independently.


The palaeobiogeographical history of Rehderodendron reveals that its fossil members of the European lineage were most prominent during climatic optima such as the Palaeocene–Eocene Thermal Maximum (PETM), Early Eocene Climate Optimum (EECO) and Middle Miocene Thermal Maximum (MMTM). However, when during the Pliocene the climate changed to colder and less humid conditions, the genus went extinct in Europe but migrated eastwards, most likely in two dispersal events along the Tethys Sea prior to extinction. One of the former most westerly stepping stones is suggested by the refugial occurrence of R. microcarpum in the southeastern Himalaya, whereas R. macrocarpum and R. kwangtungense, the taxa distributed more to the east, might have migrated eastwards already before the Miocene.

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The current flora of eastern Asia and southeastern Europe is assumed to be a relict of an ancient Cenozoic flora that thrived along the warm and humid northern margin of the Tethys Sea. The palaeoflora in Eurasia was characterized by a high degree of uniformity [e.g., [15] and underwent changes from the Palaeocene to Miocene and Pliocene in response to climatic changes [6, 7] and the closing of the Tethys. After the Pliocene, the thermophilic elements disappeared completely from Europe either prior or during Quaternary glaciation, but many of them still persist in eastern Asia [5]. Manchester et al. [3] considered that some of the extant genera exhibit morphological stasis and therefore can be considered “living fossils” traced back to early Cenozoic times. Rehderodendron appears to be one such fossil, because it was reduced from a widespread geographic distribution during the Cenozoic to only eastern Asia in modern times in response to environmental and climatic changes. Comparable examples are Carya Nuttall (Juglandaceae), which was more diverse in Europe than in North America and Asia during the Neogene, but now has disappeared completely from the modern European flora [8, 9], and Styrax Linnaeus (Styracaceae), whose evolutionary history can be traced the through the Cenozoic relictual flora in Europe [10] but today is only present with one species in south east Europe, whereas although it is diverse today in Asia and the Americas.

The Styracaceae family comprises 12 genera and ca. 160–180 woody plant species occurring in warm temperate to tropical climates in the Americas, south Europe, east and south east Asia and Malesia [11, 12]. The family forms a well supported clade [10, 12], and most of the genera are monotypic or oligotypic with limited geographic distribution, except Styrax, the largest genus [10, 13]. Rehderodendron Hu comprises 6–8 species that occur as trees in China, Vietnam and, Myanmar (Fig. 1; Table 1; [10, 11, 1417]). Most of the Rehderodendron species are deciduous trees and flower before their leaves develop (R. burmanicum (W.W. Sm. & Farrer) W.Y. Zhao, P.W. Fritsch & W.B. Liao, R. indochinense H.L. Li, R. kwangtungense Chun, R. kweichowense Hu, R. macrocarpum Hu, R. microcarpum K.M. Feng ex T.L. Ming) and grow in montane evergreen and mixed deciduous broadleaved forests. Two species (R. truongsonense P.W. Fritsch, W.B. Liao & W.Y. Zhao and R. macrophyllum (C.W. Wu & K.M. Feng) W.Y. Zhao, P.W. Fritsch & W.B. Liao; [17]) are considered evergreen and occur in ravine seasonal rain forests or broadleaved montane evergreen forests (Table 1). The fruit of Rehderodendron is distinguished from those of the other Styracaceae genera by its large size and cylindrical shape, harbouring an endocarp with many irregular rays intruding into the mesocarp [15, 17].

Fig. 1
figure 1

Map of Asia showing geographic distribution distribution of the extant species of Rehderodendron

Table 1 List of extant species investigated (p = pollen; f = fruits), their collection sites, general occurrences and climate according to Köppen-Geiger [4445] and Köppen-Trewartha [46]

The earliest recognizable fossil occurrences of Rehderodendon are fruits of Rehderodendron stonei (Reid & Chandler) Mai from the lower Eocene of England [18, 19] and from the middle Eocene of France [20]. Other Styracaceae fossils are fruits of Styrax spp. from the upper Eocene of England [21] and pollen of Styrax from the lower Eocene of Austria [22]. However, because of their characteristic fruit morphology, fossil Rehderodendron fruits have been recognized subsequently from other fossil localities in Europe ranging from Miocene to Pliocene in age. Leaf morphology is of limited utility in distinguishing among Styracaceae genera. No fossil leaves of Rehderodendron have been described.

The overall pollen morphology of Rehderodendron is typical for Styracaceae in general, but until now only a few meagre descriptions and images of extant Rehderodendron pollen exist, mainly in a broader context circumscribing the pollen morphology of the family Styracaceae [23, 24]. The pollen often are depicted with scanning electron microscopy (SEM), light microscopy (LM) or transmission electron microscopy (TEM); however, the information from these images is often limited, mainly because of low magnification or insufficient printing techniques. Despite the fact that the endemic distribution of Rehderodendron today is mainly in China, Vietnam and Myanmar, and the fact that fossil Rehderodendron diaspores have been recorded only from Europe since the lower Eocene to the Pliocene [3, 18, 2528], with few exceptions fossil pollen of Rehderodendron is pretty scarce in the literature [e.g. 29, 30]. Here we present original LM, SEM images and descriptions of pollen from six extant species of Rehderodendron (R. indochinense, R. kwangtungense, R. kweichowense, R. macrocarpum, R. microcarpum, and R. truongsonense) and compare them with LM and SEM images of three fossil Rehderodendron pollen from lower Eocene and middle Miocene strata of England, Austria and Germany. Additionally we provide new images and descriptions of extant fruit morphology of Rehderodendron and all these results are used to reconstruct the palaeobiogeographical history and evolution of this living fossil.

Methods and material

Flower and fruit material of Rehderodendron kwangtungense R. kweichowense, R. macrocarpum, R microcarpum and R. indochinense from China was collected by Zhao W.Y. and his Chinese and International colleagues in 2018 and 2020, and identified by him. Rehderodendron truongsonense from Vietnam was collected by U. Swenson and colleagues in October 2018 (Table 1). All plants are housed in Sun Yat-sen University, State Key Laboratory and Guangdong Key Laboratory of Plant Resources (Guangzhou China).

Anther material of Rehderodendron species was soaked in a drop of acetolysis mixture (9:1 acetic acid anhydride: concentrated sulphuric acid) on a glass slide under a binocular and manipulated with a needle to release the pollen from the anthers. The anthers in the acetolysis mixture were repeatedly heated for several seconds over a candle flame to colour the pollen wall and extrude the cell contents. Then the pollen grains were fished out with a micro-manipulator (eyebrow hair mounted on a needle) and transferred to a clean drop of glycerol for LM photography together with a micrometer (Nikon). After photography, the pollen grains were transferred to SEM stubs with a micro-manipulator into minute drops of alcohol to wash off the remaining glycerol, then the stubs were sputter-coated with gold (BIO-RAD) under argon atmosphere and investigated in high vacuum with a FEI Inspect S 500 scanning electron microscope.

The fossil pollen grains were recovered from sediment samples covering the Palaeocene–Eocene-Thermal Maximum (PETM) from England and the Middle-Miocene-Thermal Maximum (MMTM) from Austria and Germany [22, 29, 31] by treating the sediments with HF and HCL with subsequent acetolysis [e.g., 32, 33]. The remaining extracts were mixed with glycerol and smeared onto a glass slides. The manipulation, photography and SEM investigation of fossil pollen followed the same procedures as for the extant pollen. SEM stubs of the fossil pollen are housed in the Department of Palaeontology, University of Vienna under IPUW number 7838a, 7841, 7843. The morphological characters of fossil Rehderodendron fruits were modeled on descriptions in previous studies [18, 20, 2628].


Pollen grains of six extant Rehderodendron species were photographed under LM and SEM and their sizes measured (Table 2, Figs. 2, 3). Depending on the length of heating during the acetolysation process, the pollen changed shape from originally suboblate (unacetolysed state) to subspheroidal and then to more subprolate (fully acetolysed state; Fig. 2). Pollen measurements displayed considerable differences: LM photographs of pollen in glycerol with a micrometer scale yielded larger sizes than the measurements of pollen photographed with SEM (more-or-less desiccated state of pollen after being washed in alcohol, partly desiccated and sputter-coated under argon atmosphere; Table 2, Fig. 2). The measurements of the width and height of the endopori was only possible under LM. However, all measured sizes fall within the size ranges of previously measured Rehderodendron pollen in [23 page 87: R. kwangtungense, R. kweichowense and R. indochinense, the last = is R. macrocarpum according to the junior author] and [24 Table 1: R. macrocarpum]. The same is true for the fossil Rehderodendron pollen (see descriptions below).

Table 2 Pollen size measurements of extant species
Fig. 2
figure 2

LM and SEM overview images of extant Rehderodendron pollen. Scale bar in the LM images 10 µm, scale bar in the SEM overview images 10 µm

Fig. 3
figure 3

SEM detail images of extant and fossil Rehderodendron pollen: Scale bar = 2 µm

Description of extant pollen

Ericales Dumortier

Styracaceae Dumortier

Rehderodendron Hu

R. kwangtungense Chun (Figs. 2A, A1, 3A)

Pollen grains tricolporate (rarely tetracolporate), spheroidal to subprolate, triangular to circular in polar view and angular, elliptical to subcircular in equatorial view; measurements under LM: polar axes 32.4–38.7 µm, equatorial axes 34.5–42.7 µm; under SEM: polar axes 27.8–29.0 µm, equatorial axes 26.2–31.2 µm; endoporus rectangular to quadrangular: 7.2–11.8 µm × 5.4–7.4 µm (Figs. 1, 2). Tectum: tectate, perforate, shallowly fossulate, and faintly rugulate with rugulae bordered by faint fossulae or perforations (comparable to R. indochinense, but less pronounced), towards the colpi more micro-verrucate; ectexine in polar areas and mesocolpi regularly ornamented with supratectal blunt micro-echini (or micro-gemmae), colpus membrane, when visible, micro-verrucate; pollen wall 1.2–1.3 µm thick with sexine (0.7–0.8 µm) thicker than nexine (0.4–0.5 µm), endexine columellar to granular (columellae max. 0.3 µm high).

R. kweichowense Hu (Figs. 2B, B1, 3B)

Pollen grains tricolporate, suboblate, subspheroidal to prolate, triangular to circular in polar view and angular, elliptical to subcircular in equatorial view (Figs. 1, 2); measurements under LM: polar axes 27.3–34.9 µm, equatorial axes 17.8–39.6 µm; under SEM: polar axes 25.0–27.2 µm, equatorial axes 20.9–29.7 µm; endoporus rectangular to quadrangular 3.2–8.4 µm × 2.7–9.8 µm. Tectum: tectate, micro-verrucate to occasionally micro-rugulate, perforate, diameter of micro-verrucae ca. 0.2 µm, several micro-verrucae and micro-rugulae locally fused to produce areolae of 0.5–0.8 µm in diameter; colpus membrane, when visible, micro-verrucate; pollen wall thickness 1.1–1.3 µm with sexine thicker than nexine.

R. macrocarpum Hu (Figs. 2C, C1, 3C)

Pollen grain tricolporate, suboblate, subspheroidal, triangular to circular in polar view and angular, elliptical to subcircular in equatorial view (Figs. 1, 2); measurements under LM: polar axes 28.2–34.2 µm, equatorial axes 32–44.2 µm; under SEM: polar axes 24.3–26.3 µm, equatorial axes 24.3–33.6 µm; endoporus shape rectangular to quadrangular 4.9–11.8 µm × 6.4–10.4 µm. Tectum: tectate, perforate fossulate, fossulae border ± elongated, occasionally curved, angular rugulae (or areolae) of 0.3–0.8 µm width and 1.2–2.8 µm length; rugulae flat, with regularly spaced rows composed of occasionally fused supratectal micro-echini (or micro-gemmae) arranged perpendicularly to rugulae; colpus membrane, when visible micro-verrucate; pollen wall thickness 1.4–1.7 µm with sexine (1–1.2 µm, visible columellae max. 0.3 µm long) thicker than nexine 0.3–0.5 µm).

R. microcarpum K.M Feng ex. T.L. Ming (Figs. 2D, D1, 3D)

Pollen grains tricolporate, suboblate to subprolate, triangular to circular in polar view and angular, elliptical to subcircular in equatorial view (Figs. 1, 2); measurements under LM: polar axes 31.8–32.7 µm, equatorial axes 37.3–42.4 µm; under SEM: polar axes 26.2 to 28.8 µm, equatorial axes 26.6–31.2 µm; endoporus rectangular to quadrangular 10.4–11.9 µm × 5.9–9.1 µm. Tectum: tectate, perforate, fossulate, micro-verrucate to micro-rugulate, mesocolpium areas more pronounced perforate and micro-verrucate and colpus margins and polar areas more micro-rugulate and fossulate; micro-verrucae and micro-rugulae regularly covered by supratectal micro-echini (or micro-gemmae), occasionally arranged in rows and fused (the micro-rugulae considerably smaller than micro-rugulae of R. macrocarpum); colpus membrane when visible loosely micro-verrucate; pollen wall thickness 1.0–1.3 µm with sexine (0.7–0.9 µm, visible columellae max. 0.2 µm long) thicker than nexine (0.3–0.4 µm).

R. indochinense H.L. Li (Figs. 2E, E1, 3E)

Pollen grains tricolporate, subspheroidal to suboblate or subprolate, triangular to circular in polar view and angular, elliptical to subcircular in equatorial view (Figs. 1, 2); measurements under LM: polar axes 26.9–29.1 µm, equatorial axis 30.1–38.2 µm; and under SEM: polar axes 23.5–27.1 µm, equatorial axes 23.1–37.5 µm; endoporus shape rectangular to quadrangular, 5.4–9.1 × 5.4–6.7 µm. Tectum: tectate, perforate, rugulate, shallow fossulate, rugulae generally angular, irregularly shaped and bordered by shallow fossulae (grooves) and perforations; rugulae 1–2 µm long, generally < 1 µm wide, regularly ornamented with supratectal blunt micro-echini (or micro-gemmae), decreasing considerably in size towards colpus margins; perforations most prominent in polar areas, diminishing towards colpus margins; colpus membrane micro-verrucate; pollen wall thickness 1.4–1.5 µm with sexine (0.8–1 µm, visible columellae max. 0.3 µm long) thicker than nexine (ca. 0.4 µm).

R. truongsonense P.W. Fritsch, W.B. Liao & W.Y. Zhao (Figs. 2F, F1, 3F)

Pollen grains tricolporate, suboblate to spheroidal, triangular to circular in polar view and angular, elliptical to subcircular in equatorial view (Figs. 1, 2); measurements under LM: polar axes 30.5–32.7 µm, equatorial axes 36.4–40.0 µm; and under SEM: polar axes 26.1–28.2 µm, equatorial axes 28.3–32.1 µm; endoporus rectangular 6.3–12.7 µm × 4.3–7.4 µm. Tectum: tectate, covered with regularly arranged micro-gemmae and fused micro-gemmae producing short, rod-like structures, perforate to foveolate, tectum becoming more pronounced micro-rugulate to micro-verrucate and fossulate towards colpus margins; colpus membrane, when visible loosely micro-verrucate; pollen wall thickness 1.0–1.4 µm with sexine (0.8–0.9 µm, visible columellae max. 0.3 µm long) thicker than nexine (ca. 0.5 µm).

Description of fossil pollen

Rehderodendron sp. 1 (Figs. 3G, 4A).

Fig. 4
figure 4

LM and SEM overview images of three examples of fossil Rehderodendron pollen. R. sp. 1 from the lower Eocene of England, R. sp. 2 from the middle Miocene in Austria (Schaßbach), R. sp. 3 from the middle Miocene in German, (Entrischenbrunn)

Pollen grains tricolporate, prolate; polar axis ca. 30.5 µm and equatorial axis ca. 22.3 µm (SEM); endoporus ± quadrangular to rectangular, ca. 7.2 µm × ca. 5.7 µm (compressed fossilized state). Tectum: rugulate, fossulate, perforate, covered with supratectal micro-gemmae, the rugulae ± angular, occasionally curving 0.6–1.7 µm long and 0.4–0.8 µm wide; micro-gemmae regularly arranged in rows perpendicular to the rugulae lengths; wall thickness 1.2–1.4 µm with sexine thicker than nexine (Figs. 2, 3).

Remarks: This pollen type comes from the PETM section recovered in exploration drill cores of the London tube in Brixton (England). It was originally affiliated with Ebenaceae (Diospyros in [22]) but clearly is Rehderodendron. It most closely resembles R. kwangtungense and R. macrocarpum.

Rehderodendron sp. 2 (Figs. 3H, 4B)

Pollen grains tricolporate, prolate; polar axis 30.8–34 µm and equatorial axis 23.2 –24.4 µm; endoporus more-or-less quadrangular to rectangular, 3.8–4.9 × 3.8–4.6 µm (compressed fossilized state). Tectum: irregularly shaped, rugulate to micro-rugulate to irregularly shaped verrucate, fossulate, perforate, rugulae ± angular, occasionally curving (0.7–2.5 × 0.2–0.8 µm) and ornamented with striae or linearly fused supratectal micro-gemmae arranged perpendicular to the length of the rugulae; wall thickness 1.2–1.3 µm with sexine thicker than nexine (Figs. 2, 3).

Remarks: This pollen type has been reported [29 Fig. 3G–I] from the middle Miocene Schaßbach clay pit (Austria; MMTM). It resembles a mixture of R. kwangtungense, R. microcarpum and R. indochinense.

Rehderodendron sp. 3 (Figs. 3I, 4C)

Pollen grains tricolporate, prolate; polar axis 31–34.6 µm and equatorial axis 23.2–24.5 µm; endoporus more-or-less quadrangular to rectangular ca. 4.8–6.7 µm × 4.1–5.6 µm (compressed fossilized state). Tectum: rugulate, fossulate, perforate, rugulae are more-or-less angular, occasionally curving ca. 0.8–1.8 µm long and ca. 0.3–0.8 µm wide and ornamented with striae arranged diagonally or perpendicular to the length of the rugulae; wall thickness ca. 1.1–1.3 µm with sexine thicker than nexine (Figs. 2, 3).

Remarks: This pollen type has been reported from Hofmann and Sachse [31] middle Miocene (end of the MMTM) sand pit in Entrischenbrunn (Germany). It most closely resembles a mixture of R. macrocarpum, R. microcarpum and R. indochinense.

Summarized results of pollen descriptions

The sexine sculpture and ornamentation of R. macrocarpum and R. microcarpum exhibit fluent continuous transitions in the rugulae sizes (larger to smaller); however, R. macrocarpum is more fossulate and less perforate whereas R. microcarpum displays more perforations (Fig. 3). In comparing the sexine of R. microcarpum with R. kwangtungense and R. indochinense the rugulae sizes are also transitional (towards smaller and less pronounced rugulae and more obvious perforations); however R. kwangtungense has more pronounced supratectal micro-gemmae (Fig. 3). Separation among these four taxa is indistinct. Conversely, R. truongsonense, which is conspicuously perforate with supratectal micro-gemmae or echini, and R. kweichowense, which is micro-verrucate to areolate (Fig. 2), can be easily differentiated from each other and the rest of the extant species, and the fossil pollen, which are neither conspicuously perforate and micro-gemmate, nor micro-verrucate to areolate.

Brief descriptions of extant fruits

In general all investigated species develop a thick spongy mesocarp and differ mostly in the rib number and complexity of the endocarp ray system (Fig. 5, Table 3).

Fig. 5
figure 5

Images of the six extant Rehderodendron fruits: A, B R. indochinense; C, D R. kwangtungense; EF R. macrocarpum; G, H R. microcarpum; I, J R. kweichowense; K, L R. truongsonense. Scale bar 2 cm

Table 3 Fossil occurrences of fossil Rehderodendron fruits (f) and pollen (p) in Europe

The fruits of R. indochinense (Fig. 5A, B) have a characteristic long cylindrical shape with five obvious ribs, and the fruit surface usually has large brown spots, a unique feature among extant Rehderodendron species. The styles are persistent, the stigma is beaked, and the endocarp rays are irregular.

Rehderodendron kwangtungense (Fig. 5C, D) generally is characterized by columnar fruits that are conspicuously ribbed, and the styles are inconspicuous and persistent. The endocarp ray system is complex and displays irregular rays.

The fruits of R. microcarpum (Fig. 5E, F) are more narrower and smaller than all other Rehderodendron fruits with usually an ovoid, cylindrical to fusiform shape and an inconspicuously ribbed surface (5 ribs usually visible). The styles are persistent (conical coracoid). The endocarp has simple, thickened rays.

Rehderodendron macrocarpum (Fig. 5G, H) is characterized by its oblong to elliptic fruits that are conspicuously ribbed (8–12 ribs); persistent styles are very short. The endocarp rays are thick and its rays display irregular thicknesses and lengths.

As mentioned above, the pollen morphology of R. kweichowense and R. truongsonense differ substantially from those of the other four species investigated. This difference is also reflected in their fruits: the fruits of R. kweichowense (Fig. 5I, J) are densely covered with stellate hairs. The fruits also have 10 to12 ribs and irregular endocarp rays. The fruits of R. truongsonense (Fig. 5K, L) are short-terete and inconspicuously ribbed; the endocarp is thickened and comprises an even more complex endocarp ray system than R. macrocarpum.


Comparison of extant and fossil pollen of Rehderodendron

The comparison of LM and SEM images of the three fossil and six extant Rehderodendron pollen described here revealed that the fossil pollen resemble overall four extant Rehderodendron taxa: the lower Eocene Rehderodendron sp. 1 from the PETM (Figs. 3G, 4A) resembles a mixture of mostly R. kwangtungense and R. macrocarpum (Figs. 2A,C, 3A, C), the middle Miocene Rehderodendron sp. 2 from the MMTM (Figs. 3H, 4B) resembles a mixture of R. kwangtungense, R. microcarpum, and R. indochinense (Figs. 2A, D, E, 3A, D, E), and sp. 3 from the end of the MMTM (Figs. 3I, 4C) resembles a mixture of R. macrocarpum, R. indochinense and R. microcarpum (Figs. 2C, E, D, 3C, E, D). However, there are two differences:

  1. 1.

    The fossil pollen are always prolate (Fig. 3A–C), which is only the case in extant Rehderodendron pollen when acetolysed for a longer time. The influence of acetolysation under heat is therefore assumed to mimic the fossilization process and the pollen shape can change from suboblate to prolate (Fig. 2A1–F1).

  2. 2.

    As compared to the extant species R. indochinense, R. kwangtungense, R. macrocarpum and R. microcarpum, the rugulae of the fossil Rehderodendron sp. 2 and sp. 3 display a much wider variation in size, and the supratectal arrangement of micro-gemmae on the rugulae in the fossil specimens of Rehderodendron sp. 2 and sp. 3 is generally more diagonally arranged and the individual micro-echini/micro-gemmae are mostly fused into rows (Figs. 2, 3).

However, rugulae size and the degree of fusion of supratectal echini is also various within extant and fossil species. Both, extant and fossil pollen grains show a decrease in rugulae size towards the colpus margo (Fig. 3). There are more than those above: fossil pollen grains were found in Austria and Germany and are of late Oligocene to middle Miocene age [30, 3439] (summary Table 3). They all appear similar to Rehderodendron species sp. 2 and sp. 3 described here and display the same variation of rugulae size and fusion of supratectal micro-gemmae. The resemblance of fossil pollen and fruits to R. indochinense begins in the Miocene. We suggest that all fossils were members of a lineage leading to the extant species.

No records of fossil Rehderodendron pollen resembling the extant taxa R. kweichowense and R. truongsonense exist. Our assessment of the fossil Rehderodendron pollen type in Grímsson et al. [30: Fig. 20D-F] affiliated with R. kweichowense and R. macrocarpum was hampered by a mix-up of taxa and insufficient images in [23]: their R. macrocarpum is actually R. indochinense and our new images show that R. kweichowense has a completely different tectum ornamentation than the fossil pollen in [30]. Consequently, similar to the other fossil pollen taxa, their pollen taxon resembles a mixture of R. indochinense and R. microcarpum.

Distribution of fossil Rehderodendron fruits and comparison with extant species

Manchester et al. [3, 18, 2628] provided a brief summary of Rehderodendron fossil diaspores. There are additional fossil diaspore occurrences in the literature [e.g., 20, 25, 4042] that are listed in Table 4. Five fossil taxa have been recorded from Europe [3, 18, 27]: R. stonei (Reid & Chandler) Mai from the lower Eocene to mid-Eocene of England [19] and France (near the EECO, R. ehrenbergii (Kirchheimer) Mai, R. wisaense Mai and R. custodum Holý from the Miocene in Germany and the Czech Republic (often near the MMTM), R. ehrenbergii from the Pliocene in Italy, and R. dacium Mai & Petrescu from the Pliocene in Romania. According to Manchester et al. [3], who reinterpreted the findings of Miki [43], Rehderodendron diaspores probably also were present during the Pliocene in Japan, but this material has not been re-investigated. The fossil fruits have generally been compared with R. kwangtungense (= R. hui in [18 page 489; 24 page 67]), perhaps because the material of of R. kwangtungense was the easiest to access and the only one available in European herbaria.

Table 4 Measurements and descriptions of fossil and extant Rehderodendron fruits

In comparing fruit morphology of fossil Rehderodendron with extant species it can be seen that the fossil fruits do not resemble only R. kwangtungense (Fig. 5C, D) as suggested by Mai [18] and Gregor [24], but other species as well. The smallest fruit is that of R. stonei [3, Figs. 50–51 and in 18, Fig. 17j-l], displaying as well characters of R. microcarpum (Fig. 5G, H), whereas the medium-sized R. ehrenbergii [e.g., 3, Figs. 45–49; 18, Fig. 17 g-h] more closely resembles R. macrocarpum (Fig. 5E, F), and R. microcarpum (Fig. 5G, H). The largest fruit is that of R. wisaense [18, Fig. 17 m, plate 69 Figs. 15–17] and resembles a poorly developed fruit of R. indochinense (Fig. 5A, B); the same is most likely true for R. dacium and R. custodum (Table 3). We conclude that, like the pollen data, the fossil fruits display the same variation and mixture of morphological characteristics as in extant R. kwangtungense, R. microcarpum, R. macrocarpum, and R. indochinense, and the resemblance to R. indochinense occurs in fossil fruits from the Miocene to Pliocene.

Eurasian distribution of extant and fossil Rehderodendron

The geographic distribution of extant Rehderodendron and its fossil fruits and pollen shows a disjunction up to the Late Miocene (or Pliocene):

  1. 1.

    The extant species occur solely in Asia (mainly China, Vietnam and Myanmar, Laos, NE India; Tables 1, 5, Fig. 1) and grow generally in Cwa, Cwb, Cfa climates of the Köppen-Geiger classification ([44, 45]: warm-temperate climate with dry winters and hot or warm summers or fully humid with hot summers) or Cw and Cf climates of the Köppen-Trewartha classification ([46]: subtropical climate with dry winters or fully humid). The exception is the Vietnamese R. truongsonense [15], which thrives as well under Am climate of the Köppen-Geiger classification ([44, 45]: tropical to subtropical monsoon climate). Fossils similar to R. truongsonense and R. kweichowense are not represented in the fossil record and therefore will be not discussed further. In comparing temperature and rainfall ranges extracted from the climate information based on extant Rehderodendron distribution from WorldClim website (; [47], see Table 5), many of the modern species of Rehderodendron appear to easily adapt to subtropical monsoon climate (the annual mean temperature of Rehderodendron ranges from 7.08–19.5 ℃ and annual precipitation range from 893–3856 mm; Table 5).

  2. 2.

    The fossil occurrences of pollen and fruits that all resemble extant R. kwangtungense, R. macrocarpum, R. microcarpum, and R. indochinense are restricted to Europe (England, France, Czech Republic, Germany, Austria, Italy and Romania; Table 4, Fig. 6) and until now have not been found in other regions. Rehderodendron fossils are often recorded from exceptionally warm periods during the early Eocene around the PETM in England [4851, 51] and EECO in France [20], these are periods characterized by A and C climates of Köppen-Geiger [44, 45; warm temperate to tropical climate] and C climates of Köppen-Trewartha classification [46; subtropical climate]. Further, fossil pollen occur at the Oligocene/Miocene transition, during the lower and middle Miocene (MMTM), periods that are characterized by mostly C and less A climates of Köppen-Geiger (Köppen-Geiger data of the MMTM in Germany Entrischenbrunn [31], Köppen-Geiger data of the MMTM in Austria Lavanttal [30], and CLAMP and Köppen-Geiger data of Schaßbach, Austria [52, 53]). Fossil fruits occurred at the Miocene/Pliocene transition and during the Pliocene in southern Europe in refugial “warm and moist niches” [54, 42 for Italy; 27 for Romania]. The palaeoclimate conditions can be summarized as sufficient warmth [42, 54] and either evenly distributed precipitation/humidity (Cfa climate), or unevenly distributed precipitation during the year (= Cwa/Cwb climate = drier winter and warm or hot summers) to grow, flower, set seed and propagate. During the Pliocene, the early lineage of Rehderodendron went extinct in Europe because of cooling and drying during the Pleistocene [6, 7]. Consequently, the European early Rehderodendron was likely an ancestral lineage leading to the extant species (R. indochinense, R. kwangtungense, Rehderodendron macrocarpum and R. microcarpum) that currently occur in China, Myanmar and Vietnam, whereas R. kweichowense and R. truongsonense likely evolved separately.

Table 5 Temperature and rainfall ranges of extant Rehderodendron species extracted from WorldClim website (; [47])
Fig. 6
figure 6

Map of Europe showing geographic distribution of Rehderodendron fossils in Table 3

The dispersal from Europe to Asia

Fruit dispersal of several taxa by animals and water and the west–east migration during the Eocene from Europe to China and vice versa has been mentioned, amongst other fossil taxa, for Juglans Linnaeus of section Cardiocaryon, Cornus Linnaeus of the blue and white fruited clade, Nyssa sinensis Olivier type, and Symplocos Jacquin subgenus Palura from middle Eocene strata of Hainan [33]. Additionally, a “boreotropical” origin of the entire family of Juglandaceae has been implied by [55], who suggested that Europe played a critical role in the migration and distribution of taxa but also exhibited high extinction of Juglandaceae taxa [55, Fig. 4]. Fitting also into this scheme is Symplocos, with its well known fossil record in Europe [summarized in 56] ranging from Paleogene to late Pliocene. The relationship of European Symplocos fossils with Asian Symplocos taxa and a Eurasian origin for the Symplocaceae has been demonstrated by Manchester and Fritsch [57, 58]. The family was known also from a few Eocene and Miocene localities in North America and now has a disjunct east Asian-American distribution [59, 60]. There are more examples of taxa with a “circumboreal connection” [2, Fig. 2] which were distributed from the Paleogene onwards up to Miocene or Pliocene in Eurasia and North America and nowadays are present in east Asia only: examples are Torricellia De Candolle [58, 6163], Gordonia J. Ellis (= Polyspora Sweet [24, 29, 63,64,65]), and Mastixiaceae [e.g., 1, 19, 59, 66,67,68]. Our data from Rehderodendron are consistent with the idea that this European-Asian connection must have been still active during the Miocene across the then-closed Turgai Strait [1, 18, 42, 57, 69].

The modern species of Rehderodendron generally grow along streams and stream valley slopes (such as R. kweichowense, R. macrophyllum, R. microcarpum, R. truongsonense), or on the gentle slopes in mountain cloud forests (R. indochinense, R. kwangtungense, R. macrocarpum). This indicates that water and gravity are important propagation forces for the fruits of this genus and that their thick spongy mesocarp helps them to float in water. Based on field observations, fruits of Rehderodendron should not float in water for a long time, or else they will rot. Additionally, it has been observed that some rodents (such as squirrels) collect fruits of Rehderodendron for consumption and storage (dyszoochory behaviour), but often destroy the seeds in the fruits and therefore only a small fraction of seeds might be able to germinate in the (forgotten) storage. We therefore suggest that water (and gravity) are the main driving vectors for the lateral fruit distribution and migration of Rehderodendron downslope whereas animals might be responsible for the fruit distribution within the mountain areas.

The dispersal of Rehderodendron to the east may have occurred in three stages.

The existence of a continuous zone of maritime-influenced vegetation along the Tethys during the Cenozoic and the concept of a “boreotropical flora” proposed by Wolfe [5, see also 1, 70] may have played a role in the early dispersal events of Rehderodendron species and many other taxa characteristic of the Eurasian relict flora (see above) (1.) The lower Eocene pollen and fruits from England and the Miocene fossils from Germany and Austria all show similarities, amongst others, with R. kwangtungense. Rehderodendron kwangtungense could be interpreted to represent the oldest developed extant species (Zhao, unpublished data) and might have dispersed eastwards already during middle Eocene times; it therefore can be found today in the easternmost part of China (see Fig. 1).

(2.) The ongoing Tethys closure and subsequent uplift of the Tibetan Plateau likely hampered the dispersal of Rehderodendron between Europe and East Asia. Additionally, the disappearing Tethys must have shifted the former Eurasian maritime-influenced climate to a more continental monsoonal climate [6, Fig. 2; 7], resulting in the evolution from the Eocene Rehderodendron stonei and Rehderodendron pollen sp. 1 to Rehderodendron ehrenbergii and R. wisaense etc. and to Rehderodendron pollen sp. 2 and sp. 3 during the Miocene (these taxa resemble in part R. indochinense) (3.) The cooling during the Pliocene [6 Fig. 2; 7] caused the extirpation of European Rehderodendron (the extant species of Rehderodendron require annual mean temperatures > 7.08 ℃, and annual precipitation > 893 mm; Table 5). Although the fruits of Rehderodendron are highly variable, it is apparent that fruits of R. ehrenbergii are similar to extant fruits of R. microcarpum, which mostly is distributed in the western part of the distribution of the range of the genus (southern eastern Himalaya; Yunnan and Xizang in China, and Kachin in Myanmar, Fig. 1). If so, then this refugium represents the end of the eastward migration of R. ehrenbergii, however, there is no evidence that the fossil R. ehrenbergii and the extant R. microcarpum belong to the same species. Never-the-less, the southeastern Himalaya was warmer than southeastern Europe during the Pleistocene ice age, which could explain why R. microcarpum survived while R. ehrenbergii perished in Europe. A comparable migration route can be assumed for the Miocene and Pliocene R. wiesaense, R. dacium, and R. custodum the fruits of which resemble mostly the extant R. indochinense, which is distributed slightly farther south of R. microcarpum (Fig. 1).

A somewhat comparable fossil (Eocene and Miocene) and modern distribution pattern to Rehderodendron can be found in Torricellia De Candolle (Torricelliaceae (Wangenheim) H.H. Hu) [2, 6163]: one extant species (T. tiliifolia De Candolle) lives in the eastern Himalaya and the other one (T. angulata Oliver) in central China [63 page 317].


Fossil pollen grains of Rehderodendron occurred in Europe from the lower Eocene to Miocene and resembles a mixture of characters of the extant R. indochinense, R. kwangtungense, R. macrocarpum, and R. microcarpum. Fossil fruit of Rehderodendron occurred only in Europe from the lower Eocene to the Pliocene (southern Europe) and resemble a mixture of characters of the same species. Fossil pollen grains and fruits with the morphology of R. kweichowense and R. truongsonense are not known and appear to represent a different lineage within Rehderodendron.

Fossil Rehderodendron in Europe grew under warm-temperate to subtropical climate conditions, generally A and C climates of Köppen-Geiger, which is also true for the extant species (China, Vietnam and Myanmar). Fossil Rehderodendron was frequently found in warm and humid periods of the Cenozoic (PETM, EECO, MMTM) and the last warm moist periods of the Pliocene in southern Europe.

Today Rehderodendron is suggested to be an element of the Eurasian “boreotropical” relictual flora which dispersed from Europe to Asia along the Tethys Sea (most probably via water) from the middle Eocene onwards and became extinct in Europe after the Pliocene.

Availability of data and materials

All specimens are available at the listed repositories: stubs with pollen at the University of Vienna, Department of Palaeontology and herbarium specimens at Sun Yat-sen University State Key Laboratory and Guangdong Key Laboratory of Plant Resources.


  1. Mai DH. Tertiäre Vegetationsgeschichte Europas. Jena: Gustav Fischer Verlag; 1995. p. 691.

    Google Scholar 

  2. Manchester SR. Biogeographical relationships of North American Tertiary floras. Ann Miss Bot Gard. 1999;86:472–522.

    Article  Google Scholar 

  3. Manchester SR, Chen Z-D, Lu A-M, Uemura K. Eastern Asian endemic seed plant genera and their paleogeographic history throughout the northern hemisphere. J Syst Evol. 2009;47:1–42.

    Article  Google Scholar 

  4. Tiffney BH. Perspectives on the origin of the floristic similarity between eastern Asia and eastern North America. J Arnold Arboretum. 1985;66:73–94.

    Article  Google Scholar 

  5. Wolfe JA. Some aspects of plant geography of the Northern Hemisphere during the late Cretaceous and Tertiary. Ann Mo Bot Gard. 1975;62:264–79.

    Article  Google Scholar 

  6. Zachos J, Pagani M, Sloan L, Thomas E, Billups K. Trends, rhythms, and aberrations in global climate 65 ma to Present. Science. 2001;292:686–93.

    Article  CAS  Google Scholar 

  7. Zachos JC, Dickens GR, Zeebe RE. An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics. Nature. 2008;451:279–83.

    Article  CAS  Google Scholar 

  8. Mai DH. Der Formenkreis der Vietnam-Nuß (Carya poilanei (Chev.) Leroy) in Europa. Feddes Repert. 1981;92:339–85.

    Article  Google Scholar 

  9. Manchester SR. The fossil history of Juglandaceae. Monogr Syst Bot Missouri Bot Gard. 1987;21:1–137.

    Google Scholar 

  10. Fritsch PW, Morton CM, Chen T, Meldrum C. Phylogeny and biogeography of the Styracaceae. Intern J Plant Sci. 2001;162:S95–116.

    Article  Google Scholar 

  11. Fritsch PW. Styracaceae. In: Kubitzky K, editor. The families and genera of vascular plants, vol. 6. Berlin: Springer Verlag; 2004. p. 434–42.

    Google Scholar 

  12. Yan M-H, Fritsch PW, Moore MJ, Feng T, Meng A-P, Yang J, Deng T, Zhao C-X, Yao X-H, Sun H, Wang H-C. Plastid phylogenomics resolves infrafamilial relationships of the Styracaceae and sheds light on the backbone relationships of the Ericales. Mol Phylogenet Evol. 2018;121:198–211.

    Article  Google Scholar 

  13. Fritsch PW. Phylogeny and biogeography of the flowering plant genus Styrax (Styraceae) based on chloroplast DNA restriction sites and DNA sequences of the internal transcribed spacer region. Mol Phylogenet Evol. 2001;19:387–408.

    Article  CAS  Google Scholar 

  14. Hwang S-M, Grimes J. Styracaceae. In: Wu Z-Y, Raven PH, editors. Flora of China, vol. 15. Beijing and St Louis: Science Press and Missouri Botanical Gardens Press; 1996. p. 53–271.

    Google Scholar 

  15. Zhao W-Y, Fritsch PW, Do VT, Fan Q, Yin Q-Y, Penneys DS, Swenson U, Liao W-B. Rehderodendron truongsonense (Styracaceae) a new species from Vietnam. J Bot Res Inst Texas. 2019;13:157–71.

    Article  Google Scholar 

  16. Zhao W-Y, Fritsch PW, Fan Q, Liao W-B. Taxonomic reassessment of Rehderodendron gongshangense (Styracaceae) based on herbarium specimens and field observations. Phytotaxa. 2020;450:001–7.

    Article  Google Scholar 

  17. Zhao W-Y, Fritsch PW, Liu Z-C, Fan Q, Jin J-H, Liao W-B. New combinations and synonyms in Rehderodendron (Styracaceae). PhytoKeys. 2020;161:79–88.

    Article  Google Scholar 

  18. Mai DH. Subtropische Elemente im europäischen Tertiär I. Die Gattungen Gironniera, Sarcococca, Illicium, Evodia, Ilex, Mastixia, Alangium, Symplocos and Rehderodendron. Paläont Abh Abt B. 1970;3:441–503.

    Google Scholar 

  19. Reid EM, Chandler MEJ. The London clay flora. London, UK: British Museum (Natural History); 1933.

    Book  Google Scholar 

  20. Vaudois-Mieja N. Extension paleogeographique en Europe de l'actuel genre asiatique Rehderodendron Hu (Styracacees). Comptes-Rendus des Seances de l'Academie des Sciences, Serie 2 Mecanique-Physique, Chimie, Sciences de l'Univers, Sciences de la Terre. 1983; 296(1): 125–130.

  21. Chandler MEJ. The upper Eocene flora of Hordle Hands, 1. London: Palaeontological Society; 1925. p. 32.

    Google Scholar 

  22. Hofmann C-C. Light and scanning electron microscopic investigations of pollen of Ericales (Ericaceae, Sapotaceae, Ebenaceae, Styracaceae and Theaceae) from five lower and mid-Eocene localities. Bot J Linn Soc. 2018;187:550–78.

    Article  Google Scholar 

  23. Liang Y-H, Yu C-H. Pollen morphology of Styracaceae and its taxonomic significance. Acta Phytotax Sinica. 1985;23:81–90.

    Google Scholar 

  24. Morton CM, Dickison WC. Comparative pollen morphology of the Styracaceae. Grana. 1992;31:1–15.

    Article  Google Scholar 

  25. Gregor HJ. Neue Pflanzenfossilien aus der niederrheinischen Braunkohle. II Polyspora kilpperi nova. Spec. (Theaceae) aus dem Ober-Miozän des Tagebaus Zukunft-West bei Eschweiler/Rhld. Paläontol Zeitschr. 1978;52:198–204.

    Article  Google Scholar 

  26. Geissert G, Gregor H-J. Einige interessante und neue sommergrüne Pflanzenelemente (Fruktifikationen) aus dem Elsäßer Pliozän (Genera Sabia Colebr., Wikstroemia Endl., Alangium Lam., Nyssa L., Halesia Ellis, Rehderodendron Hu). Mitt. Badischen Landesver. Naturk. Naturs. e.V. Freiburg Breisgau. 1981;12:233–9.

    Google Scholar 

  27. Mai DH, Petrescu I. Eine neue Rehderodendron-Art (Styracaceae) aus dem oberen Pliozän des Baraolt Beckens (Sozialistische Republik Rumänien). Zeitschr für Geol Wissensch Berlin. 1983;11:915–25.

    Google Scholar 

  28. Martinetto E. East Asian plant elements in the Plio-Pleistocene floras of Italy. In: Zhang A-L, Wu S-G, editors. Floristic characteristics and diversity of East Asian plants: proceeding of the first international symposium on floristic characteristics and diversity of East Asian Plants. Beijing and Berlin Heidelberg: China Higher Education Press and Springer-Verlag; 1998. p. 71–87.

    Google Scholar 

  29. Hofmann C-C, Lichtenwagner S. First palynological results of accessorial elements from the Langhian Schaßbach clay pit, Lavanttal Basin (Austria)—LM and SEM investigations of Cornales and Ericales. Grana. 2020;59:33–43.

    Article  Google Scholar 

  30. Grímsson F, Bouchal JM, Xafis A, Zetter R. Combined LM and SEM study of the middle Miocene (Sarmatian) palynoflora from the Laventtal Basin, Ausztria: Part V. Magnoliophyta 3—Myrtales to Ericales. Grana. 2020;59:127–93.

    Article  Google Scholar 

  31. Hofmann Ch-Ch, Sachse M. SEM pollen analysis of mid-Miocene deposits of Entrischenbrunn (Bavaria, Germany) revealing considerable amounts of pollen of subhumid and sclerophyllous plants together with intrazonal water plants. Rev Palaeobot Palyn. 2023. submitted.

  32. Hofmann C-C, Gregor HJ. Scanning electron microscope and light microscope investigations of pollen from an atypical mid-Eocene coal facies in Stolzenbach mine (PreußenElektra) near Borken (Kassel, Lower Hesse, Germany). Rev Palaeobot Palyn. 2018;252:41–63.

    Article  Google Scholar 

  33. Hofmann C-C, Kodrul TM, Liu X-Y, Jin J-H. Scanning electron microscopy investigations of middle to late Eocene pollen from the Chanchang Basin (Hainan Island, South China)—insights into the paleobiogeography and fossil history of Juglans, Fagus, Lagerstroemia, Mortoniodendron, Cornus, Nyssa, Symplocos and some Icacinaceae in SE Asia. Rev Palaeobot Palyn. 2019;265:41–61.

    Article  Google Scholar 

  34. Ferguson DK, Zetter R, Pingen M, Hofmann C-C. Advances in our knowledge of the Miocene plant assemblage from Kreuzau. Germany Rev Palaeobot Palyn. 1998;101:147–77.

    Article  Google Scholar 

  35. Filek T. Pollenmorphologische Untersuchungen (LM, REM) ausgewählter Gattungen aus „Phosphoritkonkretionen“ der Fundstelle Hinzenbach, Oligozän, Österreich. Master thesis, University Vienna; 2019, p. 78.

  36. Hofmann C-C, Zetter R, Draxler I. Pollen- und Sporenvergesellschaften aus dem Karpatium des Korneuburger Beckens (Niederösterreich). Beitr Paläont. 2002;27:17–43.

    Google Scholar 

  37. Kottik S. Die Palynologie des Randecker Maars (Miozän, Baden Württemberg). Master thesis of the University of Vienna, 2002, p.96.

  38. Kovar-Eder J, Meller B, Zetter R. Comparative investigations of the basal fossiliferous layers of the opencast mine Oberdorf (Köflach-Voitsberg lignite deposit, Styria, Austria; Early Miocene). Rev Palaeobot Palyn. 1998;101:125–45.

    Article  Google Scholar 

  39. Vomela S. Die Mikroflora der untermiozänen Fundstelle Wiesa bei Kamenz, Deutschland. Master thesis, University of Vienna, 2016, p. 167.

  40. Geissert F, Gregor H-J, Mai DH. Die “Saugbaggerflora” eine Früchte- und Samenflora aus dem Grenzbereich Mio-Pliozän von Sessenheim im Elsass (Frankreich). Docum Natur. 1990;57:1–208.

    Google Scholar 

  41. Gregor HJ, Oberli U, Sachse M. Neue paläophytologische Befunde zu den mio-oligozänen Floren von Wattwil und Ebnat-Kappel (Kanton St. Gallen, Schweiz) und ihre palökologischen-klimastratigraphischen Aussagen. Docum. Natur. In prep.

  42. Martinetto E, Momohara A, Bizzarri R, Baldanza A, Delfino M, Esu D, Sardella R. Late persistence and deterministic extinction of “humid thermophilous plant taxa of East Asian affinity” (HUTEA) in southern Europe. Palaeogeogr Palaeoclimatol Palaeoecol. 2015;467:211–31.

    Article  Google Scholar 

  43. Miki S. Paleodavidia, synonym of Melliodendron and fossil remains in Japan. Bull Mukogawa Women’s Univ. 1968;16:287–91.

    Google Scholar 

  44. Kottek M, Grieser J, Beck C, Rudolf B, Rubel F. World Map of the Köppen-Geiger climate classification updated. Meteorol Zeitschr. 2006;15:259–63.

    Article  Google Scholar 

  45. Rubel F, Brugger K, Haslinger K, Auer I. The climate of the European Alps: shift of very high resolution Köppen-Geiger climate zones 1800–2100. Meteorol Zeitschr. 2017;25:115–25.

    Article  Google Scholar 

  46. Belda M, Holtanová E, Halenka T, Kalová J. Climate classification revisited: from Köppen to Trewartha. Clim Res. 2014;59:1–13.

    Article  Google Scholar 

  47. Hijmans RJ, Cameron SE, Parra JL, Jones PG, Jarvis A. Very high resolution interpolated climate surfaces for global land areas. Int J Climat. 2005;25:1965–78.

    Article  Google Scholar 

  48. Collinson ME, Steart DC, Harrington GJ, Hooker JJ, Scott AC, Allen LO, Glasspool IJ, Gibbons SJ. Palynological evidence of vegetation dynamics in response to palaeoenvironmental change across the onset of the Palaeogene-Eocene Thermal Maximum at Cobham, Southern England. Grana. 2009;48:38–66.

    Article  Google Scholar 

  49. Hofmann C-C, Mohamed O, Egger H. A new terrestrial palynoflora from the Palaeocene/Eocene boundary in the northwestern Tethyan realm (St. Pankraz, Austria). Rev Palaeobot Palynol. 2011;166:295–310.

    Article  Google Scholar 

  50. Hofmann C-C, Pancost R, Ottner F, Egger H, Taylor K, Zetter R. Palynology, biomarker and clay mineralogy of the Early Eocene Climate Optimum (EECO) in the transgressive Krappfeld succession (Eastern Alps, Austria). Austrian J Earth Sci. 2012;105:224–39.

    Google Scholar 

  51. Hofmann C-C, Egger H, King C. LM and SEM investigations of pollen from the PETM and EECO localities of Austria and Great Britain: new findings of Atherospermataceae, Annonaceae, Araceae, and Arecaceae from the lower Eocene. Plant Syst Evol. 2015;301:773–93.

    Article  CAS  Google Scholar 

  52. Braunstein N. Leaf margin analyse und CLAMP analyse einer sarmatischen Blattflora aus dem Lavanttal. Master thesis of the University of Vienna, 2014, p 112.

  53. Dörrer J. CLAMP analyse und leaf margin analyse einer Sarmatischen Blattflora aus dem Lavanttal (Teil 2). Master thesis of the University of Vienna, 2014, p 119.

  54. Martinetto E. The role of central Italy as a centre of refuge for thermophilous plants in the Late Cenozoic. Acta Palaeobot. 2001;41:299–319.

    Google Scholar 

  55. Zhang Q-Y, Ree RH, Salamin N, Xing Y-W, Silvestro D. Fossil-informed models reveal a boreotropical origin and divergent evolutionary trajectories in the walnut family (Juglandaceae). Syst Biol. 2022;71:242–58.

    Article  Google Scholar 

  56. Mai DH, Martinetto E. A reconsideration of the diversity of Symplocos in the European Neogene on the basis of fruit morphology. Rev Palaeobot Palynol. 2006;140:1–26.

    Article  Google Scholar 

  57. Manchester SR, Fritsch PW. European fossil fruits of Sphenotheca related to Asian species of Symplocos. J Syst Evol. 2014;52:68–74.

    Article  Google Scholar 

  58. Fritsch PW, Manchester SR, Stone RD, Cruz BC, Almeda F. Northern hemisphere origins of the amphi-Pacific tropical plant family Symplocaceae. J Biogeogr. 2015;42:891–901.

    Article  Google Scholar 

  59. Manchester SR. Fruits and seeds of the Middle Eocene Nut Beds flora, Clarno Formation, North Central Oregon. Palaeontogr Am. 1994;58:1–205.

    Google Scholar 

  60. Tiffney BH. Part 8. Fossil fruit and seed flora from early Eocene Fisher/Sullivan site. In: Reems RE, Grimsly GJ, editors. Early Eocene vertebrates and plants from the Fisher/Sullivan site (Nanjemoy Formation) Stafford County, Virginia. Virginia Div. Min. Res. Publication; 1999, 152, pp 139–159.

  61. Collinson ME, Manchester SR, Wilde V. Fossil fruits and seeds of the Middle Eocene Messel biota, Germany. Abh Senckenberg Naturforsch Ges. 2012;570:1–251.

    Google Scholar 

  62. Manchester SR, Collinson ME, Soriana C, Sykes D. Homologous fruit characters in geographical separated genera of extant and fossil Torricelliaceae (Apiales). Int J Plant Sci. 2017;178:567–79.

    Article  Google Scholar 

  63. Meller B. Comparative investigation of modern and fossil Torricellia fruits—a disjunctive element in the Miocene and Eocene of Central Europe and the USA. Beitr Paläont. 2006;30:315–27.

    Google Scholar 

  64. Kovar-Eder MB. Plant assemblages from the hanging wall sequence of the opencast mine Oberdorf N. Voitsberg, Styria (Austria, Early Miocene, Ottnangian). Palaeontogr B. 2001;259:65–112.

    Google Scholar 

  65. Grote PJ, Dilcher DL. Investigations of angiosperms from the Eocene of North America: a new genus of Theaceae based on fruit and seed remains. Bot Gaz. 1989;150:190–206.

    Article  Google Scholar 

  66. Eyde RH. The fossil record and ecology of Nyssa (Cornaceae). Botan Rev. 1997;63:97–123.

    Article  Google Scholar 

  67. Eyde RH, Xiang Q-Y. Fossil mastixoid (Cornaceae) alive in eastern Asia. Am J Bot. 1990;77:689–92.

    Article  Google Scholar 

  68. Kirchheimer F. Die Laubgewächse der Braunkohlezeit in einem kritischen Katalog ihrer Früchte und Samen. W. Knapp Verlag, Halle/Saale; 1957, p.783.

  69. Tiffney BH, Manchester SR. The use of geological and palaeontological evidence in evaluation plant phylogeographic hypotheses in the Northern Hemisphere Tertiary. Intern J Plant Sci. 2001;162:S3–17.

    Article  Google Scholar 

  70. Pearson PN, van Dongen BE, Nicholas CJ, Pancost RD, Schouten S, Singano JM, Wade BS. Stable warm tropical climate through the Eocene Epoch. Geology. 2007;35:211–4.

    Article  Google Scholar 

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We are grateful for collection help from staffers of Gaoligong Mountain National Nature Reserve, Shenzhen Dapeng Peninsula National Geopark, Nanling National Nature Reserve, and Yunnan Daweishan National Nature Reserve. This work was supported by the National Natural Science Foundation of China-Natural Science Foundation of Guangdong Province (2021A1515110425). We greatly appreciate the comments of Eduardo Martinetto and an anonymous reviewer that helped a lot to improve the manuscript. All authors read and approved the final manuscript.


Open access funding provided by University of Vienna. The contribution of ZWY was partly funded by National Natural Science Foundation of China—Natural Science Foundation of Guangdong Province (2021A1515110425) in combination with the fourth Survey of Chinese Traditional Medicine Resources (2018-523-001) with permission to collect species of Rehderodendron.

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Authors and Affiliations



CCH originated the concept of the study, prepared the extant and fossil pollen, summarized the fossil climate data, wrote most of the manuscript. Plant material was collected by ZWY and Chinese and International colleagues and identified by ZWY. This material was the PhD dissertation of ZWY (Styracaceae and Rehderodendron; see citations 1517) and all material used in the study is therefore deposited University Sun Yat-sen. ZWY provided the pollen and fruit material, described the fruits and compared them with the fossil occurrences, summarized the climate data and contributed to the manuscript.

Corresponding author

Correspondence to Christa-Charlotte Hofmann.

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Confirmation that collection of plant material complied with institutional, national, and international guidelines and legislation. All the plant material was collected under permit within the project 2021A1515110425 funded by the Natural Science Foundation of Guangdong Province. The vouchered samples are housed in Sun Yat-sen University, State Key Laboratory and Guangdong Key Laboratory of Plant Resources, Guangzhou, and numbers given in Table 1. No molecular data was generated so no permits are required under the Nagoya Protocol. The species are not listed under CITES appendices.

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Hofmann, CC., Zhao, WY. Unravelling the palaeobiogeographical history of the living fossil genus Rehderodendron (Styracaceae) with fossil and extant pollen and fruit data. BMC Ecol Evo 22, 145 (2022).

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