The Early History of the Proteaceae in Australia: the Pollen Record

1998 ◽  
Vol 11 (4) ◽  
pp. 401 ◽  
Author(s):  
Mary E. Dettmann ◽  
David M. Jarzen

The early history of the Proteaceae in Australia is traced from the record of fossil pollen that possess characters having taxonomic resolution among extant members of the family. Pollen characters useful for segregating subfamilies and generic groups are apertural number and form together with exine stratification and structure. When considered in conjunction with pollen shape, polarity, and size and exine sculpturing, they may be used to discriminate generic and/or species groups. The fossil pollen record suggests that the family originated in northern Gondwana during the late Cenomanian and radiated by as yet unidentified routes into southern high latitudes during the Turonian. There the family underwent substantial differentiation and expansion during Santonian–Maastrichtian times when at least four of the seven extant subfamilies evolved. Although diversification in Australia principally involved rainforest lineages (e.g. Macadamia–Helicia, Carnarvonia, Gevuina) ancestors of some sclerophyllous taxa (e.g. Adenanthos) also differentiated; this occurred in a regionalised vegetation of mesotherm open-forests in which podocarps and araucarians were important. Subsequent (Paleocene–Eocene) diversification and consolidation of the family may have focused on introduction and expansion of sclerophyllous lineages (e.g. Isopogon, Petrophile), but rainforest elements (e.g. Embothrium) were also involved. The associated vegetation, which was regionalised, experienced considerable floristic modifications during this time with introductions and/or expansion of an array of angiosperm taxa, notably Casuarinaceae, Myrtaceae and Nothofagus. In southern regions a marked decline in proteaceous pollen diversity and abundance occurred near the end of the Eocene, whereas in north-eastern regions the decline may have been later, during the Miocene.

2014 ◽  
Vol 41 (4) ◽  
pp. 673-686 ◽  
Author(s):  
Natácia Evangelista de Lima ◽  
Matheus S. Lima-Ribeiro ◽  
Carla Faleiro Tinoco ◽  
Levi Carina Terribile ◽  
Rosane G. Collevatti

Paleobiology ◽  
2002 ◽  
Vol 28 (3) ◽  
pp. 304-307
Author(s):  
Stephen Jay Gould

Kepler famously remarked of his great Florentine friend that he could never keep sufficiently straight a man whose first name so resembled his last: Galileo Galilei. Others have labored under (or benefited from) this duality, and this third essay of my series tells a tale of the most obscure, yet highly significant, character that I have ever encountered from the early history of our science: the Neapolitan scholar (1461–1523) who called himself Alessandro ab Alessandro, or Alexander de Alexander, or Alessandro degli Alessandro—all meaning (roughly) Alexander from the family of Alexander.


1994 ◽  
Vol 31 (2) ◽  
pp. 418-425 ◽  
Author(s):  
M. J. Hutton ◽  
G. M. MacDonald ◽  
R. J. Mott

A fossil pollen record extending from 11 300 BP to the present was recovered from Mariana Lake, Alberta (55°57′N, 112°01′W). Initially, the region had a sparse vegetation dominated by forbs and graminoids, which at approximately 10 500 BP succeeded to Picea glauca forest. Picea mariana – Sphagnum peatlands began to develop between 10 000 and 9500 BP. After 9000 BP Sphagnum-dominated sites decreased; P. glauca declined while Betula increased. From 7500 to 5500 BP Populus reached its maximum Holocene representation in the vegetation. Sphagnum-dominated peatlands almost disappeared. The changes following 9000 BP were likely caused by increased aridity. However, the presence of P. mariana, Abies, and Larix in the pollen record suggests that mesic sites remained. Beginning at 6500–6000 BP the extent of Sphagnum peatlands began to increase. Abies declined in importance following 5000 BP, possibly due to paludification of mesic sites. The expansion of parkland into central Alberta during the mid-Holocene did not extend to Mariana Lake. However, Mariana Lake records changes in vegetation resulting from increased aridity in the early to mid-Holocene which are not apparent at more northerly sites in Alberta.


1963 ◽  
Vol 9 ◽  
pp. 69-85 ◽  

Charles Galton Darwin, born 19 December 1887, was the eldest son of Sir George Darwin, F.R.S., Plumian Professor of Astronomy at Cambridge, whose best known work was on the early history of the moon. His mother, whose maiden name was Maud du Puy, was an American lady. A grandson of the great scientist whose first name he bore, two of Darwin’s uncles were Fellows of the Society and his ancestors included Erasmus Darwin, author of the Loves of the plants in verse, as well as of more conventional scientific writings, and the first Josiah Wedgwood. Among his cousins was Francis Galton who with Lord Kelvin was his godfather. The life of his family when he was a child has been recorded by his elder sister Gwen Raverat in her admirable Period piece which describes inimitably their life interwoven with that of the other Darwin families then in Cambridge and to a lesser extent with a few other Cambridge children. One of the latter recalls Charles as ‘a big cheerful energetic boy, humorous and scornful of nonsense’. He impressed his young contemporaries by discussing prime numbers and electricity with his father, he is also remembered as being pursued furiously by a sister round the garden with a fork! Newnham Grange, which since Charles’s death is to become Darwin College for postgraduate students, is a charming but rather rambling house on the banks of the branch of the Cam leading from Newnham Mill. There are bridges across from the garden leading to two islands; with a boat and a canoe and a tree house, it made an ideal home for a young and energetic family. Until he was about 10 years old, when his grandmother died, the family spent some time each year at Down House


2019 ◽  
Author(s):  
Florian Muthreich ◽  
Boris Zimmermann ◽  
H. John B. Birks ◽  
Carlos M. Vila-Viçosa ◽  
Alistair W.R Seddon

vi.AbstractAimFossil pollen is an important tool for understanding biogeographic patterns in the past, but the taxonomic resolution of the fossil-pollen record may be limited to genus or even family level. Chemical analysis of pollen grains has the potential to increase the taxonomic resolution of pollen, but present-day chemical variability is poorly understood. This study aims to investigate whether a phylogenetic signal is present in the chemical variations of Quercus L. pollen and to assess the prospects of chemical techniques for identification in biogeographic research.LocationPortugalTaxonSix taxa (five species, one subspecies) of Quercus L., Q. faginea, Q. robur, Q. robur ssp. estremadurensis, Q. coccifera, Q. rotundifolia and Q. suber belonging to three sections: Cerris, Ilex, and Quercus (Denk, Grimm, Manos, Deng, & Hipp, 2017)MethodsWe collected pollen samples from 297 individual Quercus trees across a 4° (∼450 km) latitudinal gradient and determined chemical differences using Fourier-transform infrared spectroscopy (FTIR). We used canonical powered partial least-squares regression (CPPLS) and discriminant analysis to describe within- and between-species chemical variability.ResultsWe find clear differences in the FTIR spectra from Quercus pollen at the section level (Cerris: ∼98%; Ilex: ∼100%; Quercus: ∼97%). Successful discrimination is based on spectral signals related to lipids and sporopollenins. However, discrimination of species within individual Quercus sections is more difficult: overall, species recall is ∼76% and species misidentifications within sections lie between 18% and 31% of the test-set.Main ConclusionsOur results demonstrate that subgenus level differentiation of Quercus pollen is possible using FTIR methods, with successful classification at the section level. This indicates that operator-independent FTIR approaches can surpass traditional morphological techniques using the light microscope. Our results have implications both for providing new insights into past colonisation pathways of Quercus, and likewise for forecasting future responses to climate change. However, before FTIR techniques can be applied more broadly across palaeoecology and biogeography, our results also highlight a number of research challenges that still need to be addressed, including developing sporopollenin-specific taxonomic discriminators and determining a more complete understanding of the effects of environmental variation on pollen-chemical signatures in Quercus.


Author(s):  
Simon Morgan Wortham

This chapter examines phobia as a question of psychoanalysis itself, a means to assess its complex and problematic conditions of possibility. In 1929, Alfred Adler produced a case study of ‘Miss R.’ in which he analysed her lupus phobia. Lupus is an auto-immune disease that reached its heights during the nineteenth century. Found at the crossroads between the sprawl of the city and the birth of the clinic, lupus’s historic arc reflects the early history of psychoanalysis. Adler associates Miss R.’s phobias with a desire to avoid her own inferiorization within the family and a fear about life on the outside. The case study offers a clue to the relationship between analyst and analysand: Adler interprets the young girl’s behaviour in terms of an egotistic desire to hold centre-stage; yet the case history is constructed out of extemporized remarks made before a captive audience, presumably to show off Adler’s analytic brilliance (in contrast to Freud’s, whom he takes every opportunity to disparage). We wonder whether Adler might be talking about himself as much as Miss R., and the case study begins to offer some insights not only into the split with Freud in 1911 but indeed the resistances of psychoanalysis itself.


2007 ◽  
Vol 45 (4) ◽  
pp. 605-610 ◽  
Author(s):  
Liliana Katinas ◽  
Jorge V. Crisci ◽  
María Cristina Tellería ◽  
Viviana Barreda ◽  
Luis Palazzesi

2019 ◽  
Vol 7 ◽  
pp. 111-128
Author(s):  
Sinjini Sinha ◽  
Don B Brinkman ◽  
Alison M. Murray

            Isolated centra of members of the Esocidae occur frequently in vertebrate microfossil localities of Late Cretaceous and early Paleocene age and are an important source of data on the early history of the family. However, morphological variation along the vertebral column can lead to incorrect interpretations of diversity if they are not recognized. To facilitate the use of centra for interpreting the diversity and distribution of esocids in Cretaceous vertebrate microfossil localities, the variation along the column in five extant species of esocids is described. Comparison with Cretaceous centra referred to the Esocidae allows identification of a series of features in which species of Esox differ from basal members of the family. These include the presence of a mid-ventral groove bordered by a pair of low budges on centra in the anterior end of the column, and antero-lateral processes on the posterior abdominal and anterior caudal centra. These differences provide a basis for recognizing early occurrences of the genus Esox in the fossil record and thus will allow centra to be used to document the timing of origin of the genus.


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