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Artykuły w czasopismach na temat „Palaeoecology”

Autor: Grafiati
Data publikacji: 4 czerwca 2021
Data aktualizacji: 9 marca 2023

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1

Hart, S. Fraser. "Archaeocyath palaeoecology". Paleontological Society Special Publications 6 (1992): 122. http://dx.doi.org/10.1017/s2475262200006821.

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A well preserved archaeocyath fauna occurs in the Forteau Formation in Southern Labrador, Canada. Following on from the confirmation that archaeocyatha are aspiculate calcified sponges, detailed ecological work is now being undertaken on this fauna, a representative of the first reefal ecosystem in the fossil record.One species, Metaldetes profundus, shows considerable variability in growth form, from open bowl-shaped forms in lagoonal settings, to a branching morphology in biohermal habitats. This species also appears to colonise a variety of substrate types and for this purpose often uses exothecal structures and holdfasts. M. profundus is also the dominant species numerically, comprising 80% of the fauna, except at the top of the bioherm horizon, where Archaeocyathus atlanticus becomes dominant. In contrast to previous studies' findings, bowl-shaped Metaldetes at the top of the bioherm horizon occupy the basal region of the bioherms, not the upper areas and provide a surface on which the bioherms can develop.The unique form of Retilamina amourensis endows it with the ability to stabilise substrates so facilitating the colonization of a substrate. It is more common at the base of bioherms, providing a surface on which other archaeocyaths can settle. The calcimicrobes Renalcis and Epiphyton also appear to have played a major role in the initiation of the bioherms, occurring as 3–5cm thick layers on erosion surfaces, within which small, juvenile, upright M. profundus sticks, <1cm in diameter, are found, surrounded and supported by the dense calcimicrobe aggregate.Digital 3-D analysis is being used to document the behaviour of the archaeocyaths, together with vertical and lateral zonation within the bioherms, especially with regard to the timing of calcimicrobe encrustation. Volumetric abundances of the archaeocyaths are also being calculated.There are small faunal composition changes over the area: Archaeosycon billingsi, a solitary stick-like form is more abundant in the west than in the east and Archaeocyathus atlanticus, another stick-like form occurs in dense clusters in lagoonal environments, elsewhere being solitary.
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2

Thorn, Vanessa. "Phytoliths in palaeoecology". Geology Today 23, nr 4 (lipiec 2007): 153–57. http://dx.doi.org/10.1111/j.1365-2451.2007.00624.x.

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3

Donovan, Stephen K. "Beachcombing and palaeoecology". Geology Today 27, nr 1 (styczeń 2011): 25–33. http://dx.doi.org/10.1111/j.1365-2451.2011.00779.x.

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4

Hicks, Sheila. "Aerobiology and palaeoecology". Aerobiologia 8, nr 2 (sierpień 1992): 220–30. http://dx.doi.org/10.1007/bf02071630.

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5

Andrews, P. J. "Palaeoecology of Laetoli". Journal of Human Evolution 18, nr 2 (kwiecień 1989): 173–81. http://dx.doi.org/10.1016/0047-2484(89)90071-7.

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6

May, Robert M. "Palaeoecology and ecology". Trends in Ecology & Evolution 9, nr 9 (wrzesień 1994): 345. http://dx.doi.org/10.1016/0169-5347(94)90160-0.

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7

McDonald, H. Gregory. "Yukon to the Yucatan: Habitat partitioning in North American Late Pleistocene ground sloths (Xenarthra, Pilosa)". Journal of Palaeosciences 70, nr (1-2) (10.09.2021): 237–52. http://dx.doi.org/10.54991/jop.2021.17.

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The late Pleistocene mammalian fauna of North America included seven genera of ground sloth, representing four families. This cohort of megaherbivores had an extensive geographic range in North America from the Yukon in Canada to the Yucatan Peninsula in Mexico and inhabited a variety of biomes. Within this latitudinal range there are taxa with a distribution limited to temperate latitudes while others have a distribution restricted to tropical latitudes. Some taxa are better documented than others and more is known about their palaeoecology and habitat preferences, while our knowledge of the palaeoecology of taxa more recently discovered remains limited. In order to better understand what aspects of their palaeoecology allowed their dispersal from South America, long–term success in North America and ultimately the underlying causes for their extinction at the end of the Pleistocene more information is needed. A summary overview of the differences in the palaeoecology of the late Pleistocene sloths in North America and their preferred habitats is presented based on different data sources.
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8

Edwards, Kevin J., H. R. Delcourt i P. A. Delcourt. "For Palaeoecology Read Palynology". Journal of Biogeography 19, nr 2 (marzec 1992): 231. http://dx.doi.org/10.2307/2845511.

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9

Fortey, R. "The palaeoecology of trilobites". Journal of Zoology 292, nr 4 (kwiecień 2014): 250–59. http://dx.doi.org/10.1111/jzo.12108.

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10

ANDREWS, PETER. "PALAEOECOLOGY AND HOMINOID PALAEOENVIRONMENTS". Biological Reviews 71, nr 2 (maj 1996): 257–300. http://dx.doi.org/10.1111/j.1469-185x.1996.tb00749.x.

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11

Moore, Peter D. "Palaeoecology: Unravelling human effects". Nature 321, nr 6067 (maj 1986): 204. http://dx.doi.org/10.1038/321204a0.

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12

YOUNG, J. R., H. R. THIERSTEIN i A. WINTER. "Nannoplankton ecology and palaeoecology". Marine Micropaleontology 39, nr 1-4 (czerwiec 2000): vii—ix. http://dx.doi.org/10.1016/s0377-8398(00)00009-8.

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13

Pickford, Martin. "Fort Ternan (Kenya) palaeoecology". Journal of Human Evolution 16, nr 3 (marzec 1987): 305–9. http://dx.doi.org/10.1016/0047-2484(87)90006-6.

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14

ANDERSEN, SVEND TH. "Palaeoecology of the Quaternary". Boreas 10, nr 1 (16.01.2008): 132. http://dx.doi.org/10.1111/j.1502-3885.1981.tb00476.x.

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15

SIMOLA, HEIKKI. "Aspects of Quaternary Palaeoecology". Boreas 14, nr 1 (16.01.2008): 96. http://dx.doi.org/10.1111/j.1502-3885.1985.tb00893.x.

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16

BERGLUND, BJÖRN E. "Tropical palynology and palaeoecology". Boreas 18, nr 2 (16.01.2008): 126. http://dx.doi.org/10.1111/j.1502-3885.1989.tb00382.x.

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17

Huntley, B. "Quaternary palaeoecology and ecology". Quaternary Science Reviews 15, nr 5-6 (1996): 591–606. http://dx.doi.org/10.1016/0277-3791(96)00015-7.

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18

Cooper, R. A., S. Rigby, D. K. Loydell i D. E. B. Bates. "Palaeoecology of the Graptoloidea". Earth-Science Reviews 112, nr 1-2 (kwiecień 2012): 23–41. http://dx.doi.org/10.1016/j.earscirev.2012.01.001.

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19

PATZKOWSKY, M. E. "Palaeoecology: Ecosystems, Environments, and Evolution". PALAIOS 15, nr 3 (1.06.2000): 255. http://dx.doi.org/10.1669/0883-1351(2000)015<0255:br>2.0.co;2.

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20

Gałka, Mariusz, Łukasz Lamentowicz i Mariusz Lamentowicz. "Palaeoecology ofSphagnum obtusumin NE Poland". Bryologist 116, nr 3 (sierpień 2013): 238–47. http://dx.doi.org/10.1639/0007-2745-116.3.238.

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21

Andrews, Peter, i Sylvia Hixson. "Taxon-Free Methods of Palaeoecology". Annales Zoologici Fennici 51, nr 1-2 (kwiecień 2014): 269–84. http://dx.doi.org/10.5735/086.051.0225.

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22

Donovan, S. Kenneth. "H.H. Swinnerton and crinoid palaeoecology". Proceedings of the Geologists' Association 133, nr 1 (luty 2022): 112–13. http://dx.doi.org/10.1016/j.pgeola.2021.11.004.

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23

Wood, Rachel. "Palaeoecology of Ediacaran metazoan reefs". Geological Society, London, Special Publications 448, nr 1 (15.09.2016): 195–210. http://dx.doi.org/10.1144/sp448.1.

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24

Keighley, Dave. "Trace Fossils in Evolutionary Palaeoecology". Ichnos 15, nr 1 (25.12.2007): 44–45. http://dx.doi.org/10.1080/10420940600864993.

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25

Moore, Peter D. "Palaeoecology: Distributions of desert plants". Nature 317, nr 6039 (październik 1985): 672. http://dx.doi.org/10.1038/317672a0.

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26

Hofreiter, Michael, Matthew Collins i John R. Stewart. "Ancient biomolecules in Quaternary palaeoecology". Quaternary Science Reviews 33 (luty 2012): 1–13. http://dx.doi.org/10.1016/j.quascirev.2011.11.018.

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27

Gaillard, Christian. "Palaeoecology: Ecosystems, environments and evolution". Geobios 31, nr 5 (styczeń 1998): 620. http://dx.doi.org/10.1016/s0016-6995(98)80047-8.

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28

Gasse, F., i E. Fourtanier. "African diatom palaeoecology and biostratigraphy". Journal of African Earth Sciences (and the Middle East) 12, nr 1-2 (styczeń 1991): 325–34. http://dx.doi.org/10.1016/0899-5362(91)90081-9.

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29

Abrams, Marc D., i Gregory J. Nowacki. "Native American imprint in palaeoecology". Nature Sustainability 3, nr 11 (20.07.2020): 896–97. http://dx.doi.org/10.1038/s41893-020-0578-6.

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30

Worsley, Peter. "Pleistocene palaeoecology of Central Norfolk". Quaternary Science Reviews 11, nr 7-8 (1992): 821. http://dx.doi.org/10.1016/0277-3791(92)90085-m.

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31

Colin Prentice, I. "Palaeoecology and plant population dynamics". Trends in Ecology & Evolution 3, nr 12 (grudzień 1988): 343–45. http://dx.doi.org/10.1016/0169-5347(88)90092-4.

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32

Davies, Althea L., Richard Streeter, Ian T. Lawson, Katherine H. Roucoux i William Hiles. "The application of resilience concepts in palaeoecology". Holocene 28, nr 9 (12.06.2018): 1523–34. http://dx.doi.org/10.1177/0959683618777077.

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The concept of resilience has become increasingly important in ecological and socio-ecological literature. With its focus on the temporal behaviour of ecosystems, palaeoecology has an important role to play in developing a scientific understanding of ecological resilience. We provide a critical review of the ways in which resilience is being addressed by palaeoecologists. We review ~180 papers, identifying the definitions or conceptualisations of ‘resilience’ that they use, and analysing the ways in which palaeoecology is contributing to our understanding of ecological resilience. We identify three key areas for further development. First, the term ‘resilience’ is frequently defined too broadly to be meaningful without further qualification. In particular, palaeoecologists need to distinguish between ‘press’ vs ‘pulse’ disturbances, and ‘ecological’ vs ‘engineering’ resilience. Palaeoecologists are well placed to critically assess the extent to which these dichotomies apply in real (rather than theoretical) ecosystems, where climate and other environmental parameters are constantly changing. Second, defining a formal ‘response model’ – a statement of the anticipated relationships between proxies, disturbances and resilience properties – can help to clarify arguments, especially inferred causal links, since the difficulty of proving causation is a fundamental limitation of palaeoecology for understanding ecosystem drivers and responses. Third, there is a need for critical analysis of the role of scale in ecosystem resilience. Different palaeoenvironmental proxies are differently able to address the various temporal and spatial scales of ecological change, and these limitations, as well as methodological constraints on inherently noisy proxy data, need to be explored and addressed.
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33

Shuang-Xing, Guo. "Evolution, palaeobiogeography and palaeoecology of Eucommiaceae". Journal of Palaeosciences 49, nr (1-3) (31.12.2000): 65–84. http://dx.doi.org/10.54991/jop.2000.133.

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A comprehensive treatise incorporating morphology, ecology, stratigraphy and systematics of Eucommia belonging to family Eucommiaceae, based on extant and extinct records, is presented. Fifteen species of megafossil leaves and fruits of Eucommia and about one hundred localities from the northern hemisphere are known. Pollen of Eucommiidites troedssonii Erdtman was widely distributed in the Mesozoic sediments of Europe. Authentic pollen reocrds of Eucommia, Eucommiaceaopollenites eucommides Sun and E. minor Sun are known from China. They first appeared in East China in the Paleocene. The validity of Eucommia leaves known from the Paleocene of the western United States is doubtful. Other records include Eucommia brevirostria from south China, Eucommia kobayashi from northern Japan, Eucommia sp. from Alaska. United States, E. brownie, E. Montana from the Oligocene of United States, E. sibirica from the Miocene and Oligocene of Siberia. During the Miocene Eucommia species has widest distribution – E. japonica from Japan, E. caucasica from Caucasus, E. kryshtofovichii from Moldovia and Poland, E. palaeoulmoides from Caucasus, Ukraine, the Netherlands, Kazakhastan and western Russia and Eucommia sp. from Mexico are known. Eucommia europaea is known from the Mio-Pliocene of Siberia, Germany, Poland, France, Italy, the Netherlands and Hungary, Some fossil specimens assigned to the living E. ulmoides were found from the Miocene and Pliocene of Germany, Poland, Romania. Several indeterminable species of Eucommia were recorded from the Neogene of Poland, Germany, France and Italy. One species of Eucommia was found in the Pleistocene of Italy. An evaluation of these records, their geographical distribution, endemism and environmental impact have been discussed.
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34

Moss, Brian, i B. E. Berglund. "Handbook of Holocene Palaeoecology and Palaeohydrology." Journal of Ecology 75, nr 2 (czerwiec 1987): 577. http://dx.doi.org/10.2307/2260436.

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35

HABERLE, SIMON G., HERMANN BEHLING, LYDIE DUPONT i WIEBKE KIRLEIS. "Introduction: Tropical palaeoecology and global change". Global Change Biology 16, nr 6 (9.07.2009): 1645–46. http://dx.doi.org/10.1111/j.1365-2486.2010.02231.x.

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36

Scrutton, Colin. "Palaeozoic corals: their evolution and palaeoecology". Geology Today 15, nr 5 (październik 1999): 184–93. http://dx.doi.org/10.1046/j.1365-2451.1999.1505005.x.

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37

Morris, Simon Conway. "Palaeoecology: Polar forests of the past". Nature 313, nr 6005 (luty 1985): 739. http://dx.doi.org/10.1038/313739a0.

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38

Battarbee, Richard W., Henry Lamb, Keith Bennett, Mary Edwards, Anne E. Bjune, Peter E. Kaland, Björn E. Berglund i in. "John Birks: Pioneer in quantitative palaeoecology". Holocene 25, nr 1 (9.12.2014): 3–16. http://dx.doi.org/10.1177/0959683614556390.

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39

Austin, Bill. "Ecology and Palaeoecology of Benthic Foraminifera". Holocene 2, nr 2 (lipiec 1992): 185–86. http://dx.doi.org/10.1177/095968369200200213.

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40

Brinkkemper, Otto. "Book review: Handbook of Plant Palaeoecology". Holocene 24, nr 1 (23.12.2013): 130–31. http://dx.doi.org/10.1177/0959683613507663.

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41

Scanlon, J. D., M. S. Y. Lee, M. W. Caldwell i R. Shine. "The palaeoecology of the primitive snakePachyrhachis". Historical Biology 13, nr 2-3 (styczeń 1999): 127–52. http://dx.doi.org/10.1080/08912969909386578.

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42

Donovan, Stephen K., i David N. Lewis. "Palaeoecology in the museum gift shop". Proceedings of the Geologists' Association 115, nr 4 (styczeń 2004): 367–70. http://dx.doi.org/10.1016/s0016-7878(04)80016-6.

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43

Canfield, D. E. "Palaeoecology A breath of fresh air". Nature 400, nr 6744 (sierpień 1999): 503–5. http://dx.doi.org/10.1038/22872.

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44

Guérin, C. "Handbook of holocene palaeoecology and palaeohydrology". Geobios 19, nr 3 (styczeń 1986): 402. http://dx.doi.org/10.1016/s0016-6995(86)80028-6.

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45

Villa, Giuliana, Jackie A. Lees i Paul R. Bown. "Calcareous nannofossil palaeoecology and palaeoceanographic reconstruction". Marine Micropaleontology 52, nr 1-4 (sierpień 2004): 1–3. http://dx.doi.org/10.1016/j.marmicro.2004.05.001.

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46

Jorissen, Frans J. "Ecology and palaeoecology of benthic foraminifera". Palaeogeography, Palaeoclimatology, Palaeoecology 95, nr 3-4 (wrzesień 1992): 349–50. http://dx.doi.org/10.1016/0031-0182(92)90153-v.

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47

Huntley, B. "The lessons of palaeoecology re-taught". Trends in Ecology & Evolution 13, nr 10 (1.10.1998): 424. http://dx.doi.org/10.1016/s0169-5347(98)01477-3.

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48

Berggren, William A. "Ecology and Palaeoecology of Benthic Foraminifera." Journal of Protozoology 39, nr 4 (lipiec 1992): 537. http://dx.doi.org/10.1111/j.1550-7408.1992.tb04846.x.

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49

Wiltshire, Patricia E. J. "Mycology in palaeoecology and forensic science". Fungal Biology 120, nr 11 (listopad 2016): 1272–90. http://dx.doi.org/10.1016/j.funbio.2016.07.005.

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50

Lowe, J. John. "Handbook of holocene palaeoecology and palaeohydrology". Quaternary Science Reviews 4, nr 4 (1985): xv—xviii. http://dx.doi.org/10.1016/0277-3791(85)90013-7.

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