A fossil fern indicator of epiphytism in a Tertiary flora

The first known indicator of probable fern epiphytism in the Tertiary fossil record is documented from the Eocene London Clay of southeast England. This pyritised fern rachis exhibits major deviation from the basic form of petiolar vascular trace morphology shown by the other London Clay fossil ferns and is here attributed to the Polypodiaceae. This represents the first known occurrence of this family in the London Clay macroflora, and brings the total of distinct fern rachis types from the Lower Tertiary of southeast England to six. The significance of this find is interpreted in relation to its probable origins from a tropical rainforest palaeoflora in which it is proposed that this specimen represents the first occurrence of an epiphytic component.     

Betulaceous leaves and fruits from the British Upper Palaeocene

Fossil leaves and bracteate fruits are described from a new Upper Palaeocene locality in the Reading Beds near Newbury, southern England. The leaves are assigned to Craspedodromophyllum acutum Crane and correspond in many respects to those of living Betulaceae. The bracts and fruits are assigned to Palaeocarpinus laciniata Crane, which although referable to the Coryleae exhibits a novel combination of the characters of several living genera, particularly Corylus and Carpinus. An argument is presented for the association of these organs as a reconstructed fossil plant which is an extinct member of the Betulaceae. The evolution and fossil record of the Betulaceae are discussed, the late Upper Cretaceous and Palaeocene being regarded as the time at which the characters of modern genera were beginning to differentiate. Carpinus appears to have undergone a major Eurasian diversification during the late Palaeogene and early Neogene. Dispersal in Palaeocarpinus laciniata was probably less specialized than in most extant Coryleae.     

Betulaceous leaves and fruits from the British Upper Palaeocene

Fossil leaves and bracteate fruits are described from a new Upper Palaeocene locality in the Reading Beds near Newbury, southern England. The leaves are assigned to Craspedodromophyllum acutum Crane and correspond in many respects to those of living Betulaceae. The bracts and fruits are assigned to Palaeocarpinus laciniata Crane, which although referable to the Coryleae exhibits a novel combination of the characters of several living genera, particularly Corylus and Carpinus. An argument is presented for the association of these organs as a reconstructed fossil plant which is an extinct member of the Betulaceae. The evolution and fossil record of the Betulaceae are discussed, the late Upper Cretaceous and Palaeocene being regarded as the time at which the characters of modern genera were beginning to differentiate. Carpinus appears to have undergone a major Eurasian diversification during the late Palaeogene and early Neogene. Dispersal in Palaeocarpinus laciniata was probably less specialized than in most extant Coryleae.     

A primitive ceratomorph (Perissodactyla, Mammalia) from the early Tertiary of Europe

Hyracotherium cuniculus Owen, 1842, from Palaeocene–Eocene boundary strata in NW Europe, was formerly considered to be an equoid. It is here placed in Cymbalophus gen. nov. , in the perissodactyl suborder Ceralomorpha, which comprises tapiroids and rhinocerotoids, as one of its most primitive and earliest members. This revised classification is based on an evaluation of its advanced versus primitive character states, and comparison with a variety of other primitive perissodactyls. Cheek tooth occlusal relationships in the early stages of ceratomorph evolution are discussed and contrasted with the fundamental perissodactyl morphotype as represented in Hyracotherium. It is suggested that the Lophiodontidae (formerly considered to be ceratomorphs; may be more closely related to chalicotheres; that the Isectolophidae may be the sister-group of chalicotheres and lophiodonts plus ceratomorplis; and that Cymbalophus is the most primitive known member of the newly restricted Ceratomorpha. Cymbalophus is placed tentatively in the family Helaletidae.     

Wasatchian (Early Eocene) pollen floras from the Red Hot Truck Stop, Mississippi, USA

Sediments at the Red Hot Truck Stop (RHTS), Mississippi, USA are important because they contain the lowest latitude record of both the earliest known Eocene plant and mammal fossils in North America. The RHTS contains the uppermost Tuscahoma Formation and the lowermost part of the basal Bashi and Hatchetigbee formations. The Tuscahoma Formation is composed of glauconitic sands and silts that represent estuarine to shallow marine sediments. Faunal remains indicate that the RHTS section belongs to the Wasatchian North American land mammal age and specifically to the lower Graybullian subdivision. Pollen and spore floras from the RHTS are moderately diverse (113 taxa) and contain families that today are associated with warm‐adapted vegetation types such as Annonaceae, Bombacaceae, Burseraceae and palms. Eocene first occurrences are represented by Brosipollis sp., Celtispollenites sp., Interpollis microsupplingensis, cf. Nuxpollenites psilatus, Platycarya spp., Retistephanocolporites sp. and Symplocos? contracta and by one genus of pteridophyte spore (Granulatisporites sp.). The overall composition and within‐sample diversity of the sporomorph flora is more similar to the Hatchetigbee Formation (early Eocene) than to the middle Tuscahoma Formation (late Palaeocene) but among‐sample diversity remains unchanged across the Palaeocene/Eocene boundary. The distinct composition of the RHTS demonstrates that floral change across the Palaeocene/Eocene boundary is complex and composed of several phases of floral change.     

Dispersed Fern Sporangia from the British Tertiary

Dispersed fern sporangia have been recovered from the BembridgeMarls of the Isle of Wight and from Bracklesham deposits ina borehole West of Poole, Dorset. These fern sporangia confirmthe presence of the family Polypodiaceae s.1. in the BritishTertiary flora. Previously records of this family have beenbased solely on vegetative material, usually fragmentary, forwhich taxonomic assignment is inevitably insecure. The sporangia,containing spores and with adherent paraphyses, are shown tobe most comparable with the Recent genus Acrostichum L. andare described as Acrostichum anglicumsp. nov. The distributionand occurrence of these sporangia suggests the extensive developmentof Acrostichum in the lacustrine environments of Bembridge times.     

Tertiary leaves of the tribe Banksieae (Proteaceae) from south-eastern Australia

Leaves from the tribe Banksieae of the Proteaceae are well represented in Tertiary deposits in south-eastern Australia. Four new species of Banksieaephyllum are erected, taking the total to 11, and two species are described in a new genus, with leaves with architectural similarities to the tribe Banksieae but without organic preservation. The fossil species demonstrate that the tribe was diverse by the end of the Eocene, but it is difficult to determine the ancestral type from the fossil evidence at present. The vegetation associated with some of the fossil species suggests that the tribe may have had its origins in rainforest, and became adapted to the typically dry, nutrient-poor conditions of sclerophyllous vegetation during the course of the Tertiary.     

An enigmatic fossil moss from the British Tertiary

Abstract

Patterns of variation in isozymes of peroxidase, esterase and acid phosphatase from six populations of Sphagnum pulchrnm in Britain are described. These are used to compare levels of polymorphism within and between the populations. Both are high and the implications of these fmdings are discussed in relation to the origin and maintenance of variation in populations where sexual reproduction does not take place.     

Cretaceous plant taxonomy and angiosperm ancestors: sources of difficulty

HUGHES, N. F., 1984. Cretaceous plant taxonomy and angiosperm ancestors: sources of difficulty. It is suggested that one of the primary reasons for slow progress in identifying angiosperm ancestors is restriction of investigation resulting from inappropriate and unimaginative taxonomic handling of the now much-extended available data. Because of the incomplete nature of any palynologic evidence, identification of ancestors from it can only come from a very large number of observations of fossils and from strict application of stratigraphic sequence information; quick solutions are most unlikely. The removal of any Mesozoic gymnosperm group from the list of ancestor candidates should only arise from prolonged investigation.     

British mammals in the Tertiary period

British Tertiary mammals are best represented in the Eocene and earliest Oligocene epochs. Additional occurrences are from the Miocene and Late Pliocene. The Eocene is marked by the occurrence of various extinct orders as well as the appearances of some of the earliest and must primitive artiodactyls and perissodactyls. The appearances in the Early Eocene and Early Oligocene represent major dispersal events, reflecting penecontemporaneous palaeogeographic changes. In the intervening timespan Britain was part of an European island, sharing its endemic terrestrial fauna. From the late Middle Eocene to earliest Oligocene, the British record is detailed enough to trace successive changes in the patterns of diversity and faunal turnover, which may relate to changing climate as well as to the dispersal events. It has been shown that changes in patterns of ecological diversity through the Eocene and earliest Oligocene match vegetational changes judged from plant fossils. They suggest a gradual transition from closed forest in the Early Eocene to a more open environment with reedmarsh and wooded patches by the end of the epoch.     

A new genus and species of an early Eocene primate from North Africa

A new Adapiform Primate from the locality of Chambi (Tunisia) is described and assigned toDjebelemur martinezi gen.nov., sp. nov. Holotype CBI 33, fragment of left mandible with P/3-M/3. Other material includes a lower and two upper isolated molars and one probable lower canine. This new material is assigned to the Adapidae.     

A New Damselfly Family from the Upper Palaeocene of Argentina

A new family of damselflies, based on Latibasalia elongata gen. et sp. nov. and L. quispeae gen. et sp. nov., is erected from the Upper Palaeocene Maíz Gordo Formation, north-western Argentina. Latibasaliidae fam. nov. can be included in the Zygoptera: Caloptera: Eucaloptera: Amphipterygida: Amphipterygoidea. Its phylogenetic relationships within the clade Eucaloptera Bechly, 1996 are discussed. Within Amphipterygoidea, Latibasaliidae could be closely related to Pseudolestidae or to the 'thaumatoneurid' genera Petrolestes and Congqingia because they share the absence of secondary antenodal crossveins of first and second rows and the absence of antesubnodal crossveins. These characters could be potential synapomorphies of these taxa but they are somewhat homoplastic within the Zygoptera.     

A new fossil wood from the highly diverse early Eocene equatorial forest of Gujarat (western India)

During the early Eocene (～55–52 Ma), when the Indian subcontinent relished equatorial climatic conditions, lignite was deposited along its north western margin. Lignite mines of northwestern India have proved to be an outstanding resource for palaeoenvironmental information. The Vastan lignite mine of the early Eocene age situated near Surat district (Gujarat) is one of the well-dated and fossiliferous lignite mines in western India. A fossil wood, retrieved from this mine, is systematically described and shows a strong resemblance to the modern genus Chisocheton of the family Meliaceae. Plant fossils are the best source to reconstruct the palaeoenvironment of any region, and here a luxurious, highly diverse tropical evergreen forest is interpreted in and around the fossil locality in contrast to the tropical thorn forest of the present day. This early Eocene highly diverse equatorial forest, once covered a significant portion of the Indian subcontinent, is now restricted in fringes known as Western Ghats in south India attesting to changes in climate.     

Rhododendron seeds from the Palaeocene of southern England

Seeds closely resembling those of some species of the extant genus Rhododendron L. have been recovered from the Reading Beds near Newbury, Berkshire. The fossils are assigned to Rhododendron newburyanum sp. noV. on the basis of detailed comparisons with seeds of extant Rhododendron species, other Ericaceae, and taxa with seeds of similar morphology.     

Primary domestication and early uses of the emblematic olive tree: palaeobotanical, historical and molecular evidence from the Middle East

Our knowledge of the origins of olive tree domestication in the Middle East and on the processes governing its extension and persistence in different vegetation types from prehistory through antiquity to modern times derives from diverse sources, spanning the biological sciences to the humanities. Nonetheless, it lacks a robust overview that may lead to floating interpretations. This is especially true in the Middle East, considered as the cradle of agriculture, and where the evolutionary history of this emblematic tree is intertwined with that of civilizations. Olive fruit, oil and wood have been, since Prehistoric times, characteristic products of the lands bordering the Mediterranean Sea. In the domestic economy of these countries, the olive tree gradually became a traditional tree crop since the first oil extraction, through the emergence of regional commerce that accompanied the rise and fall of early Near-Middle Eastern urbanism, until the development of modern trade, with an oil production estimated at circa 3000000 tons per year. The rising importance of the olive tree in human life has turned the tree into an endless source of fascination in the Aegean and Eastern Mediterranean, a symbol and a sacred tree, widely cited in the Bibles, the Koran, and in ancient literature. Here we argue that advances in radiocarbon chronology, palaeobotany, genetics, and archaeology-history have profoundly refined the history of olive trees in the Middle East. This review shows that the heartland of primary olive domestication must be enlarged to the Levant and not only focus on the Jordan Valley. The domestication of the olive tree is a long and ongoing process, linked to the early production of oil and the development of the olive trade. We also suggest that the olive tree became a particular icon, a sacred tree, during the Biblical period in the Levant.     

Quaternary plant fossils from the Jebel Marra volcanic complex and their palaeoclimatic interpretation

The fossil plants from the Malha Crater, previously referred to as Cyperus papyrus L. have been re-identified as Phragmites sp.; since determination to species is not possible, this record can have no phytogeographical or palaeoclimatic significance.Olea sp., probably O. laperrinei Batt. et Trab. from Jebel Marra, dated 3 500 B.P. raises interesting but so far speculative considerations regarding the inter-relationship of Mediterranean and tropical African species in the southern Sahara during the last pluvial period.Leaf impressions of the oil palm, Elaeis guineensis Jacq. from Jebel Marra, where it is no longer to be found, plus considerations regarding other surviving forest species in the gallery forests, suggest a minimum northwards climatic shift during the last pluvial in the order of 400 km.This fossil record is regarded as suggesting that the source of the oil palm kernel discovered at the Neolithic site of Esh Shaheinab, near Khartoum, is probably Jebel Marra.     

First discovery of colobine fossils from the early to middle Pleistocene of southern Taiwan

Here we report on two kinds of cercopithecid fossil monkeys (Cercopithecinae and Colobinae) from the early to middle Pleistocene sediments of the Chochen (=Tsochen) area (Tsailiao-chi or Shinhua Hill), southern Taiwan. The fossil specimens include the first fossil record of colobine monkeys from Taiwan, where only macaque monkeys now occur. All cercopithecine fossils were identified as Macaca cf. Macaca cyclopis, the extant Taiwan macaque, except for one extremely large isolated upper molar, which may belong to another macaque species. On the other hand, all colobine specimens fall within the size variation of extant and extinct Rhinopithecus, but its specific status cannot be determined because of the scantiness of the fossil material. In Taiwan, Rhinopithecus presumably became extinct in the late Pleistocene, probably owing to global cooling and vegetation change, whereas macaques, which are of almost the same body size as Rhinopithecus, survived as M. cyclopis to the present. The contrasting history of survival between the two kinds of monkeys may be due to ecological/behavioral differences between them or as a result of accidental events that occurred in the Pleistocene of Taiwan.     

A new mobergellan (small shelly fossils) from the early middle cambrian of morocco and its significance

A new mobergellan genus and species,Tateltella ranoculata, is described from the early Middle Cambrian (Agdzian Stage) of Morocco. The new taxon is characterized by only four pairs of muscle scars and is furthermore distinguished from other mobergellans by its strongly concave shape and its distally rising muscle scars. The individual specimens ofTateltella ranoculata distinctly vary in size and display different ontogenetic stages. Juvenile, intermediate, and adult stages can be distinguished by means of the development of the muscle scars that differ in Position relative to the apex, size, and distinctness between individual stages. The shell ofT. ranoculata is composed of a succession of thin phosphatic lamellae separated by interlamellar gaps, presumably originally filled by organic material. The interlamellar gaps may be divided by septum-like structures producing discrete cavities. The specimens are the youngest mobergellans known so far and correlation of their stratigraphic position suggests a correspondence with the lower part of the Amgan stage of the Siberian Platform. In addition, they are the first reported mobergellans from the present day continent Africa. Other mobergellan taxa and mobergellan-like species are briefly reviewed and the genusHippoklosma Missarzhevsky, previously assigned to the Mobergellidae, is excluded from the family due to its different shell structure. An evolutionary trend of reduction in the number of muscle scars from 14 in the early Early Cambrian to only eight in the early Middle Cambrian is apparent among mobergellans.