Many plant genera in the tropical West Pacific are survivors from the paleo-rainforests of Gondwana. For example, the oldest fossils of the Malesian and Australasian conifer Agathis (Araucariaceae) come from the early Paleocene and possibly latest Cretaceous of Patagonia, Argentina (West Gondwana). However, it is unknown whether dependent ecological guilds or lineages of associated insects and fungi persisted on Gondwanan host plants like Agathis through time and space. We report insect-feeding and fungal damage on Patagonian Agathis fossils from four latest Cretaceous to middle Eocene floras spanning ca. 18 Myr and compare it with damage on extant Agathis. Very similar damage was found on fossil and modern Agathis, including blotch mines representing the first known Cretaceous–Paleogene boundary crossing leaf-mine association, external foliage feeding, galls, possible armored scale insect (Diaspididae) covers, and a rust fungus (Pucciniales). The similar suite of damage, unique to fossil and extant Agathis, suggests persistence of ecological guilds and possibly the component communities associated with Agathis since the late Mesozoic, implying host tracking of the genus across major plate movements that led to survival at great distances. The living associations, mostly made by still-unknown culprits, point to previously unrecognized biodiversity and evolutionary history in threatened rainforest ecosystems.
Terminal Cretaceous to Eocene floras from Patagonia, Argentina show affinities with fossil floras from Australia and other southern land masses, as well as living subtropical and tropical montane rainforest floras from Australasia to Southeast Asia1,2,3,4,5,6,7,8. These biogeographic connections derive from the former presence of mesic austral rainforests toward the end of Gondwana, which were nearly exterminated following the final separation of South America, Antarctica, and Australia starting from the middle Eocene. Many of the survivor lineages were sheltered in Australia as the continent moved northward to its eventual, late Oligocene collision with Asia, initiating new biotic interchanges4,5,9,10,11. A number of angiosperm12,13,14,15,16,17,18,19, fern20, and conifer21,22,23 genera with latest Cretaceous to Eocene fossil records in Patagonia exhibit this pattern of Old World survival5. The early Paleogene floras of Gondwanan Patagonia hosted diverse insect-herbivore communities based on the richness of insect feeding damage on fossil leaves24,25,26 and body fossils27,28,29, but whether the ancient insect communities or ecological associations tracked their host plants across later range shifts has been unknown.
Recently, the first South American members of the Old World broadleaved conifer genus Agathis (kauris, dammars; Araucariaceae), including its oldest known representatives, were recognized from multiple vegetative and reproductive organs found in early Paleocene7, early and middle Eocene22, and probably in terminal Cretaceous7 floras of central Patagonia, Argentina. The fossils document the evolution of the genus from an early Paleocene stem lineage to an Eocene member of the Agathis crown7. Older fossils of the agathioid clade belong to extinct taxa that lack distinctive characters of its two living genera, Wollemia and Agathis7,30,31,32. All previous Agathis fossils had come from the late Paleocene to early Miocene of Australia and the late Oligocene–Miocene of New Zealand, with no reports of unequivocal associated insect damage33,34,35. The separation of South America and Antarctica and associated cooling and aridification36,37 presumably led to the loss of suitable habitat and the extinction of Agathis in South America along with other paleo-Antarctic genera5, but the genus persists today with ca. 17 species in lowland to upper montane rainforests in Australasia and across Wallace’s Line to Sumatra in Malesia38. Agathis trees are large-statured keystone species38, often emerging prominently above angiosperms in the canopy, and they host diverse animal and fungal communities39,40. The genus faces immense logging pressure through much of its modern range38.
The Patagonian Agathis material includes abundant, well-preserved leaf-compression fossils7,22, which we observed to be associated with diverse insect herbivore damage types (DTs), including distinctive blotch mines (Fig. 1a–i and Supplementary Figs. 1–4), that resemble those we have seen on extant Agathis species (Fig. 1j–m and Supplementary Fig. 5). Although some extant Agathis insect associations have been studied (Supplementary Data 1), most extant associations that resemble the fossils are undocumented, indicating undiscovered biodiversity and evolutionary history that may exist as ancient herbivore and fungal associations surviving on modern Agathis hosts. The high relative abundances of the fossils studied here7,11,22 indicate that Agathis was a dominant genus in the past like it is today41; thus, the fossils represent ecologically important component communities that were present during the early evolution of the genus. To address the possibilities of the persistence of insect herbivore and fungal ecological guilds and the possible tracking of Agathis through time and space by component communities, we compare insect and fungal damage on fossil Agathis from Patagonia with damage on extant herbarium collections and living, wild Agathis trees.
We examined leafy branches, isolated leaves, and male and female reproductive organs of the well-preserved Argentine fossils Agathis immortalis7, a stem-group Agathis from the early Paleocene Palacio de los Loros 2 locality (PL2; Salamanca Formation; geomagnetic polarity chron C28n, which has an age range of 64.47–63.49 Ma)7,42,43,44; and Agathis zamunerae22, a crown-group Agathis7 from the early Eocene Laguna del Hunco (LH; Huitrera Formation; ca. 52.2 Ma) and middle Eocene Río Pichileufú (RP; Huitrera Formation; ca. 47.7 Ma) localities11,21. In addition, we examined cf. Agathis sp. leaves7 from the latest Cretaceous (Maastrichtian; 67–66 Ma) portion of the Lefipán Formation45,46. The Cretaceous specimens, only known from isolated leaves, exhibit morphological characters consistent with Agathis, although no cuticle or reproductive organs have been recovered7. All sites are located in Patagonian Argentina, in Chubut (Lefipán, PL2, LH) and Río Negro (RP) provinces. Together, these localities represent four time slices spanning ca. 18 million years of the early evolution of Agathis and its component communities, which are defined as assemblages of ecologically dependent component species occurring on a particular plant-host species47. We found a suite of diverse biotic associations never before seen on fossil Agathis, and we erect a new leaf mining ichnogenus and two ichnospecies; discuss other damage, including external foliage feeding, galling, possible armored scale insect (Hemiptera: Diaspididae) covers, and epiphyllous fungi (Pucciniales); and compare the damage from Patagonia with its modern analogs on extant Agathis. From the survey of modern material, we also report a rich, largely undocumented array of modern insect herbivory on living Agathis across its range that is similar to the new fossil exemplars.
Frondicuniculum ichnogen. nov.
Etymology. Classical Latin: frons -dis, a leaf, leafy twig or foliage; and cuniculum-i, meaning a mine, underground passage, hole or pit.
Type ichnospecies. Frondicuniculum lineacurvum ichnosp. nov.
Diagnosis. Elongate-ellipsoidal blotch mines occurring on broadleaved, parallel veined conifer leaves. Long axes of the mines are parallel to leaf venation. Frass, when present, is densely packed, composed of spheroidal pellets surrounded by amorphous matter, often positioned along one margin of the mine. Leaf veins within mines are distorted.
Frondicuniculum lineacurvum ichnosp. nov.
Etymology. Classical Latin: linea-e, a string, linen thread, or drawn line; and curvus–a –um, bent, bowed, arched, or curved.
Diagnosis. As for the genus, with smooth, linear to gently curving mine margins.
Description. An elongate-ellipsoidal blotch mine positioned along leaf margin, long axis parallel to leaf veins, mine margins well defined, linear to gently curving. Mine dimensions 7.2–50.0 mm long by 2.0–10.0 mm wide. Frass, when present, composed of spherical or hemispherical pellets measuring 0.04–0.12 mm in diameter and surrounded by dark, amorphous matter. Frass pellets mostly positioned near mine margin and may be replaced by surrounding amber with original frass material not preserved. Reaction rim 0.1–0.3 mm wide present at contact between mine margins and surrounding leaf tissue. Individual specimen descriptions of holotype and paratypes provided in Supplementary Note 1.
Occurrence. Huitrera Formation, Laguna del Hunco (early Eocene, Chubut Province, Argentina) and Río Pichileufú (middle Eocene, Río Negro Province, Argentina), on host plant Agathis zamunerae Wilf.
Repositories. Museo Paleontológico Egidio Feruglio, Trelew, Chubut, Argentina (MPEF-Pb), and Smithsonian Institution, National Museum of Natural History (USNM).
Frondicuniculum flexuosum ichnosp. nov.
Etymology. Classical Latin: flexuosus –a –um, full of winding turns, bent, or crooked.
Diagnosis. As for the genus, with wavy mine margins.
Description. An elongate-ellipsoidal blotch mine with gentle to strongly undulatory margins having a raised, wrinkly appearance. Mine positioned along leaf margin, long axis of the mine parallel to leaf veins. Mine dimensions 11.4–35.2 mm long by 1.2–9.4 mm wide. Frass, when present, composed of spheroidal pellets measuring ca. 0.1 mm in diameter and surrounded by smaller fragments of amorphous frass. Frass distributed throughout mine or positioned laterally near one margin of the mine. Mine margins 0.2–8.0 mm wide. Individual specimen descriptions of holotype and paratypes provided in Supplementary Note 1.
Occurrence. Palacio de los Loros 2 locality; Salamanca Formation, early Paleocene; Chubut Province, Argentina, on host plant Agathis immortalis Escapa, Iglesias, Wilf, Catalano, Caraballo et Cúneo.
Repository. Museo Paleontológico Egidio Feruglio, Trelew, Chubut, Argentina (MPEF-Pb).
For clarity, we note that the new zoological typifications and identifications assigned here refer only to the insect-damaged areas (i.e., trace fossils) of the cited fossil material, which often has separate botanical typification and identification under the same repository numbers as defined by Wilf et al.22 for Agathis zamunerae and Escapa et al.7 for Agathis immortalis. Morphologically similar, elongate-ellipsoidal blotch mines are associated with Agathis at PL2 (early Paleocene, 4 specimens), LH (early Eocene, 2 specimens), and RP (early/middle Eocene, 1 specimen), as well as Cretaceous cf. Agathis (see next paragraph), with minor differences in their margin structure. Frondicuniculum flexuosum mines have undulatory, wrinkled margins (Fig. 1a, c, and Supplementary Fig. 2a–j), whereas F. lineacurvum mines (Fig. 1d–h and Supplementary Figs. 3a–f, 4a, b) have smooth, gently curving margins. However, the overall shape, position on leaves, frass characters, and persistence through ca. 18 myr on the same host genus from the same region suggest that the mines were made by similar, probably closely related leaf-mining insects.
A blotch mine positioned along the central axis of a cf. Agathis leaf from the Maastrichtian Lefipán Formation is characterized by an elongate-ellipsoidal shape with its long axis parallel to the leaf veins and smooth, gently curved margins (Fig. 1i and Supplementary Fig. 1a–c). The mine lacks frass, which may be a preservational effect, and otherwise could be the same as Frondicuniculum lineacurvum. Because of the preservation and because there is only one specimen, or possibly two (Supplementary Fig. 1d), we did not assign a formal name to this specimen. However, the overall similarity of Cretaceous and Paleocene blotch mines on Agathis (elongate-elliposidal shape, smooth margins, distorted leaf veins) is noteworthy as the first likely evidence of a Cretaceous-Paleogene (K-Pg) boundary crossing leaf-mine association on closely related plants. Until now, no evidence has been found of surviving K-Pg leaf-mine associations within regional Maastrichtian and Danian floras anywhere in the world46,49,50.
Another probable blotch-mine type from LH and RP (Eocene) has a linear trajectory and is oriented parallel to the leaf veins, exhibiting breached epidermal tissue (DT251; Fig. 2a, b and see Supplementary Note 1 for detailed descriptions). The putative mines have a similar appearance to slot feeding characterized by elongate holes, although their smooth, gently curving margins suggest a leaf-mining origin. Some of these mine-like structures are flanked by flaps of epidermal tissue, attributable to breaching of the tissue due to environmental factors such as in vivo abrasion (Fig. 2a). The margins along the field of damage are smooth and sometimes influenced by leaf veins. We found similar damage as possible mines on modern Australian Agathis robusta (Fig. 2c and Supplementary Fig. 5m, Supplementary Note 1), featuring an elongate-ellipsoidal shape oriented parallel to the leaf veins. Like the fossils, the epidermal tissue of the extant mines is often breached (Fig. 2c and Supplementary Fig. 5m), leaving flaps of unconsumed tissue surrounded by a thin, darkened rim of reaction tissue.
Only two extant leaf-mining insects have been documented in association with Agathis (Supplementary Data 1), both on A. australis of New Zealand, although their mines are not similar to the fossils. Larvae of the leaf blotch-miner moth Parectopa leucocyma (Lepidoptera: Gracillariidae) initially form small blotch mines that transition to linear epidermal mines and then galls39. Microlamia pygmaea, a longhorn beetle (Coleoptera: Cerambycidae), mines dead leaves on fallen branches51. In our survey of extant Agathis, we found numerous examples of blotch mines similar to our fossils on six host species that span much of the modern range of the genus (Fig. 1j–m, Supplementary Fig. 5a–f, Supplementary Note 1). The extant blotch mines, previously undocumented to our knowledge, are typically elongate-ellipsoidal and exhibit many similarities to the fossils, suggesting geologically long-term behaviors with origins in the late Mesozoic and early Cenozoic. Most mine trajectories occur along the leaf margins (Fig. 1j–m), although some course along the central axes of leaves (Supplementary Fig. 5c). The long axes of the extant blotch mines are parallel to leaf venation (Fig. 1j–m) as in the fossils. Margins of the mines are smooth to wavy.
In order to assess potential convergence of leaf mine morphologies associated with related conifers that have similar leaf architecture to Agathis, we also compared extant mines on Araucaria (Araucariaceae) and members of the Podocarpaceae family, including Nageia, Afrocarpus, Sundacarpus, and Podocarpus. Araucarivora gentilii Hodges (Elachistidae) caterpillars mine leaves of Araucaria araucana in Argentina and Chile52. Mines begin with a short serpentine phase and then expand into a raised, circular to polylobate blotch mine. A circular exit hole is typically positioned near the margin of the blotch mine. The fossil Agathis blotch mines (Fig. 1a–i and Supplementary Figs. 1–4) differ in that they are elongate and lack a serpentine phase. We did not find any other blotch mine morphologies on Araucaria herbarium specimens throughout the range of the genus (parts of South America and Australasia). Three leaf-mining taxa have been described on Podocarpus. Phyllocnistis podocarpa (Lepidoptera: Gracillariidae) larvae mine Podocarpus macrophyllus leaves in Japan, creating serpentine mines with overlapping paths that often form into a blotch, although their zigzag frass trail is distinct from the fossil Agathis blotch mines53. In New Zealand, Podocarpus totara hosts two leaf miners, including Chrysorthenches polita (Lepidoptera: Glyphipterigidae), whose mines have not been described54, and Peristoreus flavitarsis (Coleoptera: Curculionidae)55. The mines of Peristoreus flavitarsis are a possible extant analog to the fossil Agathis mines, in addition to similar mines we found on extant Agathis (Fig. 1j–m and Supplementary Fig. 5). The mines are full depth and typically span the width of the leaf. Frass pellets are often deposited along portions of the mine margin at the edge of the leaf. Individual larvae make mines on multiple leaves. Before pupating in the soil or litter, the larva chews a circular hole through the epidermis on the abaxial side of the leaf55. We found other putative blotch mines on herbarium sheets of Podocarpus with similar morphologies to those on extant and fossil Agathis, including on Podocarpus ingensis from Bolivia, Podocarpus oleifolius from Colombia, and Podocarpus urbanii from Jamaica. We did not find any comparable mines on herbarium specimens of Afrocarpus, Nageia, or Sundacarpus.
Leaf mines have been recognized on other broadleaved, parallel-veined gymnosperms from the Mesozoic, although Frondicuniculum is distinguished from all the Mesozoic examples by its blotch morphology and lack of a serpentine phase. Similar to our Cretaceous specimens (Fig. 2d, e, and Supplementary Fig. 1e, f), unnamed mines on the voltzialean conifer Heidiphyllum elongatum, from the Late Triassic (Carnian) of the Karoo Basin in South Africa56,57, exhibit an elongate, parallel-sided, rectilinear path with spheroidal pellets often deposited in an approximate meniscate pattern. Triassohyponomus dinmorensis mines, also on H. elongatum but from the Blackstone Formation (Middle Triassic) in Australia58, are serpentine and have an extensive, tightly sinusoidal to meniscate pattern. Fossafolia offae on Liaoningocladus boii from the Early Cretaceous Yixian Formation of northeast China begins as a serpentine mine with an intestiniform frass trail and transitions to a blotch phase59. The blotch mines on Patagonian fossil and living Old World Agathis therefore appear to represent part of a suite of leaf mining insects of uncertain interrelationships that has colonized parallel-veined, broadleaved seed plants since the Mesozoic, but which nevertheless are distinct from the Mesozoic examples in producing the blotch-mine morphology with no serpentine phase.
Additional damage diversity
In addition to leaf mines, fossil and extant Agathis are associated with a variety of other insect feeding types (Table 1), which we sketch here while details are being prepared separately. External foliage feeding includes small circular holes (DT1, DT2; Table 1), semicircular excisions into leaf margins (DT12; Fig. 2f–h), and swaths of surface feeding (DT29). A similar spectrum of damage is found on extant Agathis throughout its range (Fig. 2i). However, many types of external foliage-feeding damage can be made by a variety of insects with mandibulate mouthparts across several taxonomic orders60, and their presence at multiple fossil and modern sites does not necessarily indicate that the same suite of closely-related insect groups produced the damage.
Four gall DTs are associated with fossil Agathis in Patagonia, including nondiagnostic, dark circular galls (DT32; Lef and LH), circular galls with a nonhardened center surrounded by a thickened outer rim (DT11; PL2), and columnar galls (DT116; PL2). Moreover, at PL2, A. immortalis is associated with ellipsoidal galls bearing a thickened outer wall surrounding epidermal tissue with files of cells. The center of each gall is marked by a circular dot representing the central chamber or exit hole (Fig. 2j). The fossils resemble undescribed ellipsoidal galls on A. ovata from New Caledonia, which are characterized by a raised rim of thickened tissue surrounding a flat, epidermal surface with a circular exit hole (Fig. 2k). The only previously documented galling insect on extant Agathis is Conifericoccus agathidis (Hemiptera: Margarodidae), the kauri coccid, whose second-instar nymphs induce blister galls that have caused extensive defoliation of Agathis robusta in Australia61. Nevertheless, we found abundant and diverse gall morphologies on extant Agathis (Fig. 2k and Table 1).
Possible covers of female armored scale insects (Diaspididae) occur on Agathis at PL2 (Fig. 2l), LH (Fig. 2m), and RP (Fig. 2n, o). At PL2, the covers are found on leaves and a cone scale7. The dorsal covers are characterized by concentric growth rings made during the construction of the cover through two instars and an adult phase (Fig. 2l–o). Ventral covers surround the dorsal covers (Fig. 2m) and, in some cases, appear to be deeply set in the leaf tissue and leave a columnar or circular pit when detached. We caution that other interpretations of these structures remain possible because some of their features are not present on extant diaspidid covers (off-center indent or hole on dorsal covers) or are atypical (ventral cover structure surrounding dorsal cover; only adult female covers are present). The possible scale covers, including the-off center indent, are very similar to structures assigned to Diaspididae from the Late Cretaceous of New Zealand and Australia62, and comparable scale covers are associated with angiosperm leaves from the Eocene of Germany63 and Miocene of New Zealand64. On extant Agathis, diaspidid scales previously have been documented on three species in New Zealand and Australia (Supplementary Data 1). We found diaspidids on Agathis herbarium specimens from New Caledonia and Fiji, including an unidentified diaspidid species that induced pit galls on A. macrophylla from Fiji (Fig. 2p).
A probable rust fungus (Pucciniales), characterized by rings of circular to oval aecia on a circular gall, is associated with Agathis zamunerae at LH (Fig. 2q). Two species of rust fungi in the genus Aecidium parasitize extant Agathis: Aecidium fragiforme from Oceania and Malesia and Aecidium balansae in New Caledonia (Fig. 2r)40,65. Aecidium on extant Agathis produces galls covered in yellow aecia (Fig. 2p). The very similar morphologies of the fossil and extant rust on Agathis suggest long-term, persistent associations reaching back to at least the early Eocene.
The persistence of multiple, nearly identical insect herbivore and fungal associations for tens of millions of years on the same host genus, Agathis (Table 1), provides insights into the evolution of insect-herbivore component communities in deep time66,67,68. The first occurrences of some of these associations were on the early Paleocene stem-group species A. immortalis and continued onto the early Eocene crown group A. zamunerae from ca. 12 million years later, suggesting an evolving co-association dating to the earliest history of the host genus67. For example, the mine margins of Frondicuniculum flexuosum on A. immortalis are wavy, but the margins of F. lineacurvum on A. zamunerae are linear to gently curving, suggesting evolutionary changes in leaf-miner behavior from the Paleocene to the Eocene. Besides minor morphological changes, however, the component communities of the Paleocene stem group and Eocene crown-group Agathis species remained remarkably similar (Table 1). The presence of crown-group Agathis in Gondwanan rainforests by the early Eocene22 and the established pattern of rainforest biome tracking among the survivor taxa from the fossil Patagonian floras5,69 provide evidence for niche conservatism70,71. Extant Agathis has accessory xylem tissues adjacent to leaf veins72 that can collapse during drought conditions73, highlighting the importance of everwet rainforest environments for the genus. The inferred presence of rainforest environments throughout the history of Agathis5,22 may have provided stable conditions for insect and fungal associations to establish geologically long-term, conservative relationships with their host genus, even as the rainforest habitats relocated across vast distances in response to global change.
Another possible explanation for reoccurrences of similar associations on Agathis through time is the convergence of insect and fungal damage morphologies and tissue usage. In this scenario, some or all the culprit lineages that made the damage on Agathis in ancient South America went extinct, even as the host persisted, and were replaced by unrelated but ecomorphically convergent lineages that recolonized the same host at a later time. The presumed stability of environmental pressures on potential herbivores as a result of habitat tracking by Agathis may have led to a convergence in damage type morphologies and diversity through time. In addition, the leaf morphology of Agathis has remained relatively unchanged since at least the latest Cretaceous7, and leaf mining behavior in particular can be influenced by leaf architecture74. Podocarpus was the only Gondwanan conifer genus that we found with similar blotch mines to Agathis, which may represent an example of convergence of leaf mine morphology as a result of similar leaf structure. However, we did not find analogs on Podocarpus to other distinct associations on fossil Agathis from Patagonia, such as the second blotch mine type, pit galls, and a distinctive rust fungus. Thus, although Podocarpus hosts morphologically similar blotch mines to Agathis, the full suite of associations on fossil Agathis presented here persists only on living Agathis.
The convergence scenario is possible and in all likelihood occurred for at least some of the fossil examples we report here that also occur on living Agathis. Because the modern and ancient culprits discovered here, are by definition, largely unknown, it is not yet possible to distinguish definitively between lineage persistence and convergence, and we present this contrast as a question for future work. However, persistence is more parsimonious and plausible than convergence on first principles, given that the host lineage clearly survived and maintains a remarkably similar suite of biotic associations today as in the deep past that is not known to occur on any other living genus.
In summary, we found a similar suite of insect damage on Cretaceous, Paleocene, and Eocene Agathis fossils from Patagonia as well as on extant Agathis throughout its modern range (Table 1). This persistent damage included leaf mines as well as external foliage feeding, galling, possible diaspidid scale-insect covers, and a rust fungus. The repeated occurrences of compositionally and morphologically similar types of herbivory on Agathis throughout its history suggest, at least, that functionally conservative ecological guilds of insects and fungi have persisted on Agathis since the end of the Mesozoic or early Cenozoic. A further possibility, and a likely one because of the demonstrated survival of the host genus, is that living Agathis component communities include the legacy of long-term, ecologically conservative lineage associations that originated in Mesozoic Gondwana, survived the end-Cretaceous extinction, and tracked the host–plant genus Agathis as its crown lineage evolved. In this scenario, the host and its communities then shifted their ranges together slowly but massively in response to major plate movements and environmental changes. These associations persist today at great temporal and spatial distances in Australasia and Southeast Asia, but they are now critically threatened by human impacts, including logging38 and climate change75. Most of the living culprits of Agathis herbivory that we observed are unknown to the best of our knowledge, suggesting potential for evolutionary and biogeographic study of novel associations.
Fossil Agathis data collection
We compared insect feeding damage on Patagonian fossil Agathis leaves, branches, and cone scales (Supplementary Data 2) from well-studied localities of the latest Cretaceous (cf. Agathis sp., Lefipán Formation, localities LefE, LefL and, LefW, 10 specimens)45,46, early Paleocene (A. immortalis, Salamanca Formation, locality PL2, 319 specimens)7,42,43,44, early Eocene (A. zamunerae, LH, 121 specimens)11,21,22, and middle Eocene (A. zamunerae, RP, 32 specimens)11,21,22 with damage on extant Agathis species. The Lefipán localities and LH are located in northwest Chubut, Argentina; PL2 is in the western San Jorge Basin near Sarmiento in southern Chubut; and RP is located in western Río Negro, Argentina. The fossil plant collections examined from Lefipán, PL2, and LH are curated at the Museo Paleontológico Egidio Feruglio (MPEF-Pb) in Trelew, Chubut. The RP collections are curated at the Museo de Paleontológico de Bariloche (BAR), San Carlos de Bariloche, Río Negro, and E.W. Berry’s historical Río Pichileufú collection48 is housed at the Smithsonian Institution, National Museum of Natural History (USNM), Washington, D.C., United States. We assigned damage-type numbers (DTs) to all insect and fungal damage using the standard reference76 and subsequent addenda. Due to the small sample sizes of rare fossil conifer-leaf mines, we did not attempt quantitative analyses comparing time periods.
Fossil locality information
The Lefipán formation was deposited in the Maastrichtian to early Danian in a tide-dominated delta environment45. The macrofloras studied here are from the terminal Maastrichtian portion of the formation (67–66 Ma), based on biostratigraphy of marine invertebrates45, dinoflagellates, and palynomorphs77,78. The three fossil plant localites (LefE, LefL, and LefW) are located in close proximity in the San Ramón section of the Lefipán Formation45, as previously detailed46. The cf. Agathis leaves from the Lefipán Formation display typical Agathis characters (symmetrical blade, lanceolate shape, parallel venation, short constricted petiole), but no reproductive parts have been found, and the specimens lack cuticular remains7. Nevertheless, they are only ca. 2–3 m.y. older than the Danian Agathis immortalis fossils, come from the same region and general depositional setting, and quite possibly represent A. immortalis or a close relative7.
Early Danian A. immortalis fossils were collected from locality Palacio de los Loros 2 (PL2) in the estuarine Salamanca Formation44. The strata at PL242 were deposited during geomagnetic polarity chron C28n (64.67–63.49 Ma)43,44,79. Specimens of A. immortalis include leaves, both isolated and on leafy branches, and many cone scales, winged seeds, and pollen cones with in situ Dilwynites pollen, including juvenile pollen cones attached to a leafy branch7.
Eocene Agathis zamunerae fossils come from Laguna del Hunco (12 quarries) and Río Pichileufú (specimens are from quarries RP3, near RP1, or imprecisely known localities from older collections), both of these caldera-lake deposits in La Huitrera Formation22. At Laguna del Hunco, 40Ar/39Ar dating of sanidine crystals in a tuff within a fossiliferous layer yielded an age of 52.22 ± 0.22 Ma10,11,21, and 40Ar/39Ar dating of tuffs located directly over the fossiliferous layers at Río Pichileufú provided an age of 47.74 ± 0.05 Ma11,21.
Extant Agathis data collection
We examined herbarium specimens of 15 species of Agathis for insect damage (Supplementary Note 1), including the complete collections of Agathis at the Arnold Arboretum (A) and Gray Herbarium (GH) of the Harvard University Herbaria, Royal Botanic Garden Edinburgh (E), Royal Botanic Gardens Kew (K), United States National Herbarium (US), Australian National Herbarium (CANB), National Herbarium of New South Wales (NSW), and the Singapore Botanic Gardens Herbarium (SING). Field examinations of Agathis were done in the Atherton Tablelands region, Queensland, Australia (A. robusta, A. atropurpurea, and A. microstachya) and on Mt. Kinabalu, Sabah, Malaysian Borneo (A. lenticula, A. borneensis, and A. kinabaluensis). We also examined the digitized (data.rbge.org.uk/search/herbarium) collections of Afrocarpus, Podocarpus, and Sundacarpus (Podocarpaceae) and Araucaria (Araucariaceae) from E and physical collections of Nageia (Podocarpaceae) from E and K to assess convergence in leaf mine morphology with Agathis mines.
We took macrophotographs with a Nikon D90 camera at the repositories listed above and at the Paleobotany Laboratory, Pennsylvania State University. For microphotography, we used a Nikon SMZ 1500 binocular microscope with a Nikon DS-Ri1 camera at the Paleobotany Laboratory, Pennsylvania State University. We processed images with Nikon NIS Elements v. 3 software, used Photoshop CC 2017 to vertically composite photographs of fossils when necessary, and Adobe Camera Raw Editor to adjust contrast, white balance, etc. on entire images.
This published work and the nomenclatural acts it contains have been registered in ZooBank, the proposed online registration system for the International Code of Zoological Nomenclature (ICZN). The ZooBank LSIDs (Life Science Identifiers) can be resolved and the associated information viewed through any standard web browser by appending the LSID to the prefix “http://zoobank.org/”. The LSIDs for this publication are: 12D2484C-3DEF-4B47-B307-E79EA61E8C4E for the new ichnogenus Frondicuniculum; 31540A57-B065-4BFD-8F67-021943A29F43 for the new ichnospecies F. flexuosum; and E8C206D0-22F5-4A2F-8183-F4AC51B3DA54 for the new ichnospecies F. lineacurvum.
Further information on research design is available in the Nature Research Reporting Summary linked to this article.
All data generated during this study are included in this published article and its supplementary information files. All material cited in this study is housed and permanently available in the repositories named in this article. Full repository information for all fossil specimens studied is listed in Supplementary Data 2.
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The authors thank E. Pinheiro and two anonymous reviewers for their constructive comments; I. Escapa, P. Puerta, L. Reiner, and E. Ruigómez and many others from Museo Paleontológico Egidio Feruglio and elsewhere for field and laboratory assistance; the staff at E (L. Scott), A and GH (J. Shapiro and E. Wood), K (S. Dawson, A. Farjon), US (E. Gardner, A. Clark, I. Lin, K. Rankin, R. Russell), CANB (B. Lepschi, C. Cargill), NSW (L. L. Lee and L. Murray), SING (N. Karim, S. Lee), USNM (F. Marsh and J. Wingerath), and CMNH (P. Fox and D. Su) for help with their collections; S. Bellgard, T. Bralower, D. Hughes, Y. Imada, N. Martin, M. Padamsee, and M. Patzkowsky for discussions; R. Kooyman for fieldwork with PW in Queensland and Sabah and related collaboration; and D. Crayn for further assistance with Australian material. This study was supported by grants to M.P.D. from the CIC/Smithsonian Fellowship, the Evolving Earth Foundation, the Geological Society of America, Sigma Xi, the Paleontological Society and the P. D. Krynine Memorial Fund of the Penn State Department of Geosciences; and to P.W., A.I., and N.R.C. from NSF awards DEB-0345750, DEB-0919071, DEB-1556666, and EAR-1925755. This research partly fulfilled requirements for a PhD degree in Geosciences from Pennsylvania State University by MPD.
The authors declare no competing interests.
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Donovan, M.P., Wilf, P., Iglesias, A. et al. Persistent biotic interactions of a Gondwanan conifer from Cretaceous Patagonia to modern Malesia. Commun Biol 3, 708 (2020). https://doi.org/10.1038/s42003-020-01428-9