Bibliografías temáticas / Paleoecology / Artículos de revistas

Artículos de revistas sobre el tema "Paleoecology"

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Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 29 de julio de 2024

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1

Ausich, William I. "Paleoecology Workshop". PALAIOS 7, n.º 2 (abril de 1992): 239. http://dx.doi.org/10.2307/3514935.

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2

Gavin, Daniel. "PALEOECOLOGY SECTION". Bulletin of the Ecological Society of America 84, n.º 4 (octubre de 2003): 186. http://dx.doi.org/10.1890/0012-9623(2003)84[186b:ps]2.0.co;2.

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3

Shuman, Bryan. "PALEOECOLOGY SECTION". Bulletin of the Ecological Society of America 85, n.º 4 (octubre de 2004): 186–87. http://dx.doi.org/10.1890/0012-9623(2004)85[186b:ps]2.0.co;2.

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4

Booth, Robert. "PALEOECOLOGY SECTION". Bulletin of the Ecological Society of America 86, n.º 4 (octubre de 2005): 263. http://dx.doi.org/10.1890/0012-9623(2005)86[263a:ps]2.0.co;2.

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5

Brugam, Richard. "Paleoecology Section". Bulletin of the Ecological Society of America 89, n.º 4 (octubre de 2008): 368. http://dx.doi.org/10.1890/0012-9623(2008)89[368a:ps]2.0.co;2.

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6

Bottjer, David J. "Bivalve Paleoecology". Notes for a Short Course: Studies in Geology 13 (1985): 122–37. http://dx.doi.org/10.1017/s0271164800001135.

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Bivalves are one of the major macroinvertebrate fossil groups of the Phanerozoic. Bivalves have occupied many aqueous habitats, and in doing this have undergone a steady, relatively unchecked increase in diversity (Figure 1). Thus, bivalves are one of the most useful fossil groups in paleoecology, both for environmental reconstruction as well as for deciphering patterns and processes of evolutionary paleoecology.
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7

Kohn, Alan J. "Gastropod Paleoecology". Notes for a Short Course: Studies in Geology 13 (1985): 174–89. http://dx.doi.org/10.1017/s0271164800001160.

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Paleoecology concerns the life processes and patterns of environmental relationships of groups of ancient organisms during their lifetimes. Two assumptions are fundamental to paleoecological theory: observed patterns in populations, associations, communities and ecosystems represented in the fossil record were imposed by contemporaneous physical and biological environmental factors and their interactions, and at least some past environmental conditions can be discerned from fossil assemblages and their rock matrices.
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8

Ward, Peter D. y Gerd E. G. Westermann. "Cephalopod Paleoecology". Notes for a Short Course: Studies in Geology 13 (1985): 215–29. http://dx.doi.org/10.1017/s0271164800001196.

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Studying the paleoecology of the extinct chambered cephalopods is somewhat analogous to studying a distant landscape through the wrong end of a powerful telescope: we can see very small views of what must have been great panoramic vistas. Two factors have lead to this situation. First, the extant cephalopods still utilizing the phragmocone system of density reduction are at very low standing diversity, while most of the more interesting taxa, such as ammonites and belemnites, are completely extinct. Our functional interpretations of various shell morphologies thus depend heavily on generalizations based on a small number of sometimes distantly related taxa, such as Nautilus and Sepia. Secondly, studies of fossil associations and their relationships to various facies are clouded by the possibility of extensive post-mortal drift of the cephalopod shells. Because of this, we cannot ever be sure that we are studying cephalopod biocoenoses. In spite of these constraints, however, the past two decades have witnessed a great research effort into the study of cephalopod paleoecology. Debate over various issues has been sometimes clamorous, a sign of a healthy and vigorous utilization of the scientific method by many interested students of the fossil record.
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9

Miller, Ranall F. "Chitin paleoecology". Biochemical Systematics and Ecology 19, n.º 5 (agosto de 1991): 401–11. http://dx.doi.org/10.1016/0305-1978(91)90057-7.

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10

Webb, Robert H. "Spatial and Temporal Distribution of Radiocarbon Ages on Rodent Middens from the Southwestern United States". Radiocarbon 28, n.º 1 (1986): 1–8. http://dx.doi.org/10.1017/s0033822200059981.

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The analysis of rodent middens, principally deposited by packrats (Neotoma sp), has rapidly become the most important paleoecologic and paleoclimatologic tool in the southwestern United States. The recent discovery of rodent middens created by stick-nest rats (Leporillus sp) and rock wallabies (Petrogale sp) in Australia (Green et al, 1983; P S Martin, oral commun, 1984) and by dassie rats (Petromus typicus) in South Africa (L Scott, oral commun, 1984) portends the use of midden analysis in arid regions worldwide. Several recent reviews of southwestern paleoecology (eg, Spaulding et al, 1983) rely heavily on rodent middens for ecologic and climatic reconstructions.
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11

Lamsdell, James C. y Curtis R. Congreve. "Phylogenetic paleoecology: macroecology within an evolutionary framework". Paleobiology 47, n.º 2 (marzo de 2021): 171–77. http://dx.doi.org/10.1017/pab.2020.61.

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The burgeoning field of phylogenetic paleoecology (Lamsdell et al. 2017) represents a synthesis of the related but differently focused fields of macroecology (Brown 1995) and macroevolution (Stanley 1975). Through a combination of the data and methods of both disciplines, phylogenetic paleoecology leverages phylogenetic theory and quantitative paleoecology to explain the temporal and spatial variation in species diversity, distribution, and disparity. Phylogenetic paleoecology is ideally situated to elucidate many fundamental issues in evolutionary biology, including the generation of new phenotypes and occupation of previously unexploited environments; the nature of relationships among character change, ecology, and evolutionary rates; determinants of the geographic distribution of species and clades; and the underlying phylogenetic signal of ecological selectivity in extinctions and radiations. This is because phylogenetic paleoecology explicitly recognizes and incorporates the quasi-independent nature of evolutionary and ecological data as expressed in the dual biological hierarchies (Eldredge and Salthe 1984; Congreve et al. 2018; Fig. 1), incorporating both as covarying factors rather than focusing on one and treating the other as error within the dataset.
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12

Winder, Isabelle C. "Early Hominin Paleoecology". Environmental Archaeology 19, n.º 2 (5 de mayo de 2014): 179–80. http://dx.doi.org/10.1179/1461410314z.00000000058.

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13

Erwin, D. H. "Paleoecology: A Redirection". Science 278, n.º 5339 (31 de octubre de 1997): 815–16. http://dx.doi.org/10.1126/science.278.5339.815.

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14

Babin, Claude. "Paleoecology concepts andapplications". Geobios 24, n.º 1 (1991): 112. http://dx.doi.org/10.1016/0016-6995(91)80043-y.

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15

Whiteman, C. A. "Paleoecology of Beringia". Quaternary Science Reviews 4, n.º 4 (1985): x—xiii. http://dx.doi.org/10.1016/0277-3791(85)90011-3.

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16

Schwörer, Christoph, Brigitta Ammann, Marco Conedera y Willy Tinner. "Wälder in der Zeitmaschine – Möglichkeiten und Grenzen der Paläoökologie". Schweizerische Zeitschrift fur Forstwesen 170, n.º 3 (1 de mayo de 2019): 117–24. http://dx.doi.org/10.3188/szf.2019.0117.

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Forests in a time machine – possibilities and limits of paleoecology Paleoecology allows the reconstruction of ecological processes that take place on long timescales – for example the vegetation dynamics since the last Ice Age or changes in the species composition of forests due to anthropogenic land use. This can be achieved by analyzing plant remains like pollen, spores, leaves, seeds or charcoal that have been conserved over millennia under low oxygen conditions in the sediment of lakes and mires. In this article, we outline the principals, the limits and the potential of paleoecology. It becomes clear that nowadays, this discipline is more than just a descriptive science. Thanks to quantitative methods, it can be used to test ecological hypothesis and identify causal relationships. Paleoecology can therefore contribute to assess the resilience of vegetation communities to external disturbances, and provides important information on how our forests will react to past, current and future climate change.
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17

Leighton, Lindsey R. "New Directions in the Paleoecology of Paleozoic Brachiopods". Paleontological Society Papers 7 (noviembre de 2001): 185–206. http://dx.doi.org/10.1017/s1089332600000966.

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Because of their great abundance, widespread distribution, excellent preservation potential (Foote and Sepkoski, 1999), and a tendency not to disarticulate after death, brachiopods are ideal subjects for paleoecological research involving morphometrics, population analysis, and phylogenetics. Paleoecology is a subdiscipline that demands large data sets and statistical tests, and brachiopods provide the opportunity to create such databases. I fully expect to see brachiopods play a major role in the coming years in studies on the cutting edge of paleoecology. My approach in this chapter is to provide some background and tools that hopefully will inspire many new ideas for using brachiopods in the study of paleoecology. My intent is not to convince anyone of the correctness of my ideas, but rather to encourage future research in these directions.
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18

Meldahl, Keith H., J. Robert Dodd y Robert J. Stanton. "Paleoecology: Concepts and Applications". PALAIOS 6, n.º 5 (octubre de 1991): 511. http://dx.doi.org/10.2307/3514988.

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19

Bottjer, David J. "Evolutionary Paleoecology: Diverse Approaches". PALAIOS 10, n.º 1 (febrero de 1995): 1. http://dx.doi.org/10.2307/3515003.

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20

Miller, William. "Advances in Deepsea Paleoecology". PALAIOS 9, n.º 1 (febrero de 1994): 1. http://dx.doi.org/10.2307/3515073.

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21

Hanson, B. "PALEOECOLOGY: Long-Lasting Consequences". Science 303, n.º 5659 (6 de febrero de 2004): 731a—731. http://dx.doi.org/10.1126/science.303.5659.731a.

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22

Sugden, Andrew M. "Future predictions from paleoecology". Science 361, n.º 6405 (30 de agosto de 2018): 888.13–890. http://dx.doi.org/10.1126/science.361.6405.888-m.

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23

Wang, Yigang y Gerd E. G. Westermann. "Paleoecology of Triassic ammonoids". Geobios 26 (enero de 1993): 373–92. http://dx.doi.org/10.1016/s0016-6995(06)80391-8.

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24

Reyment, Richard. "Paleoecology: Concepts and applications". Palaeogeography, Palaeoclimatology, Palaeoecology 91, n.º 1-2 (enero de 1992): 186–87. http://dx.doi.org/10.1016/0031-0182(92)90044-6.

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25

Napier, Joseph D., Guillaume de Lafontaine y Melissa L. Chipman. "The Evolution of Paleoecology". Trends in Ecology & Evolution 35, n.º 4 (abril de 2020): 293–95. http://dx.doi.org/10.1016/j.tree.2019.12.006.

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26

Sugden, A. M. "PALEOECOLOGY: Living in Harmony". Science 295, n.º 5554 (18 de enero de 2002): 409b—409. http://dx.doi.org/10.1126/science.295.5554.409b.

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27

Jackson, J. B. C. "PALEOECOLOGY: Measuring Past Biodiversity". Science 293, n.º 5539 (28 de septiembre de 2001): 2401–4. http://dx.doi.org/10.1126/science.1063789.

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28

Maas, Mary C. "Paleoecology in primate evolution". Evolutionary Anthropology: Issues, News, and Reviews 3, n.º 1 (2 de junio de 2005): 6–8. http://dx.doi.org/10.1002/evan.1360030105.

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29

Walker, Ian R. "Chironomidae (Diptera) in paleoecology". Quaternary Science Reviews 6, n.º 1 (enero de 1987): 29–40. http://dx.doi.org/10.1016/0277-3791(87)90014-x.

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30

Kitchell, Jennifer A. "Evolutionary paleoecology: recent contributions to evolutionary theory". Paleobiology 11, n.º 1 (1985): 91–104. http://dx.doi.org/10.1017/s0094837300011428.

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In the past decade, evolutionary paleoecology has shifted away from corroborative research of the “me-too-ecology” type toward its proper domain—the evolutionary consequences of ecological properties, roles, and strategies at the individual, population, community, and species levels. The science of evolutionary paleoecology tests for linkage between a species' ecology and its macroevolutionary history. Do the ecological characters of species within clades influence differential rate dynamics, particularly rates of faunal turnover and diversification? Intellectual coequality, once hampered by the misunderstanding that the role of paleoecology is to find examples of past ecology imperfectly entombed in the fossil record, is strengthened by the increasing number of evolutionary ecologists who have called for explicit paleontological contributions to resolve theoretical issues. The fossil record provides a necessary perspective to an understanding of process.
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31

Terras, Rafael, Mirian Carbonera, Guilherme Budke y Karla Janaísa Gonçalves Leite. "FAMÍLIA SPINOSAURIDAE (DINOSAURIA: THEROPODA): TAXONOMIA, PALEOBIOGEOGRAFIA E PALEOECOLOGIA (UMA REVISÃO)". PALEONTOLOGIA EM DESTAQUE - Boletim Informativo da Sociedade Brasileira de Paleontologia 37, n.º 77 (10 de julio de 2023): 14–54. http://dx.doi.org/10.4072/paleodest.2022.37.77.02.

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Spinosauridae family (Dinosauria: Theropoda): taxonomy, paleobiogeography and paleoecology (a revision). Spinosauridae is a family of Tetanuran theropod dinosaurs that was widely distributed during the Early Cretaceous. Here we revised the state of art of the family’s taxonomy, paleobiogeography and paleoecology. We compiled updated diagnosis for the holotypes of the 20 species attributed to the family since 1841, alongside with the different hypotheses related to the family’s paleobiogeography and paleoecology. We also compiled updated diagnosis for a series of indeterminate elements that are relevant in literature. We conclude that out of these 20 taxa six can be regarded as nomina dubia (Ostafrikasaurus crassiserratus, Suchosaurus girardi, Spinosaurus maroccanus, Siamosaurus suteethorni, Sinopliosaurus fusuiensis, Suchosaurus cultridens) due to the lack of diagnostic material and autapomorphies. Out of these, three were regarded as incertae sedis (Ostafrikasaurus crassiserratus, Suchosaurus girardi, Suchosaurus cultridens) for the same reasons and the possibility of belonging to previously already established taxa inside Spinosauridae and for one of these (Ostafrikasaurus crassiserratus) for possibly being a member of Ceratosauria. As for paleobiogeography, the fossil evidence suggests that the family might have originated in Laurasia (Western Europe), but the existence of a tooth older than the European taxa might indicate that the family might have originated in Gondwana (Brazil). Finally, regarding paleoecology, the most accepted hypothesis is that they were generalist predators of the margins of aquatic environments (i.e. riparian zone), and waders in shallow waters like modern herons and storks, and if necessary also resorting to terrestrial environments. They would be capable of alternating between resources and environments, in addition to sharing their habitats with theropods of the Abelisauridae and Carcharodontosauridae families and even with other spinosaurids, if the environmental conditions favored it. Keywords: Theropoda, Spinosauridae, Spinosaurinae, Baryonychinae, paleobiogeography, paleoecology.
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32

DiMichele, William A. y Robert A. Gastaldo. "Plant Paleoecology in Deep Time1". Annals of the Missouri Botanical Garden 95, n.º 1 (11 de marzo de 2008): 144–98. http://dx.doi.org/10.3417/2007016.

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33

Levin, Lisa A. "Paleoecology and Ecology of Xenophyophores". PALAIOS 9, n.º 1 (febrero de 1994): 32. http://dx.doi.org/10.2307/3515076.

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34

Wooller, Matthew. "Mangrove paleoecology and environmental change". PAGES news 16, n.º 1 (enero de 2008): 40–41. http://dx.doi.org/10.22498/pages.16.1.40.

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35

Fontana, Sonia L. y Keith D. Bennett. "Quaternary paleoecology: Reconstructing past environments". Past Global Changes Magazine 22, n.º 1 (abril de 2014): 46. http://dx.doi.org/10.22498/pages.22.1.46.

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36

Fontana, Sonia L. y Keith D. Bennett. "Quaternary paleoecology: Reconstructing past environments". Past Global Change Magazine 23, n.º 2 (diciembre de 2015): 77. http://dx.doi.org/10.22498/pages.23.2.77.

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37

Olago, Daniel O. y Eric O. Odada. "Paleoecology of Eastern Africa Mountains". PAGES news 9, n.º 3 (diciembre de 2001): 19–21. http://dx.doi.org/10.22498/pages.9.3.19.

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38

Tinner, Willy y Brigitta Ammann. "Timberline Paleoecology in the Alps". PAGES news 9, n.º 3 (diciembre de 2001): 9–11. http://dx.doi.org/10.22498/pages.9.3.9.

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39

Lovejoy, Thomas E. "Paleoecology and the path ahead". Frontiers in Ecology and the Environment 5, n.º 9 (noviembre de 2007): 456. http://dx.doi.org/10.1890/1540-9295(2007)5[456:patpa]2.0.co;2.

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40

Shipman, Pat. "Paleoecology of Fort Ternan reconsidered". Journal of Human Evolution 15, n.º 3 (marzo de 1986): 193–204. http://dx.doi.org/10.1016/s0047-2484(86)80045-8.

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41

Ekdale, A. A. "Paleoecology of the marine endobenthos". Palaeogeography, Palaeoclimatology, Palaeoecology 50, n.º 1 (enero de 1985): 63–81. http://dx.doi.org/10.1016/s0031-0182(85)80006-7.

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42

Olson, Everett C. "Vertebrate paleoecology: A current perspective". Palaeogeography, Palaeoclimatology, Palaeoecology 50, n.º 1 (enero de 1985): 83–106. http://dx.doi.org/10.1016/s0031-0182(85)80007-9.

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43

Verma, Omkar. "Paleoecology: Past, present and future". Journal of the Geological Society of India 91, n.º 1 (enero de 2018): 115–16. http://dx.doi.org/10.1007/s12594-018-0843-8.

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44

Miller, William. "Paleoecology of benthic community replacement". Lethaia 19, n.º 3 (julio de 1986): 225–31. http://dx.doi.org/10.1111/j.1502-3931.1986.tb00735.x.

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45

KOTAKE, NOBUHIRO. "Paleoecology of the Zoophycos producers". Lethaia 22, n.º 3 (julio de 1989): 327–41. http://dx.doi.org/10.1111/j.1502-3931.1989.tb01349.x.

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46

Heusser, C. J. "Quaternary paleoecology of Fuego-Patagonia". Revista do Instituto Geológico 15, n.º 1-2 (1994): 7–26. http://dx.doi.org/10.5935/0100-929x.19940002.

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47

Kumaran, Navnith K. P. y Ruta B. Limaye. "Holocene Palynology and Tropical Paleoecology". Quaternary International 325 (marzo de 2014): 1–2. http://dx.doi.org/10.1016/j.quaint.2014.02.005.

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48

Hughes, Paul. "Paleoecology and the conservation paradox". Landscape Ecology 32, n.º 1 (22 de noviembre de 2016): 227–28. http://dx.doi.org/10.1007/s10980-016-0470-y.

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49

Bartlein, P. J. y I. C. Prentice. "Orbital variations, climate and paleoecology". Trends in Ecology & Evolution 4, n.º 7 (julio de 1989): 195–99. http://dx.doi.org/10.1016/0169-5347(89)90072-4.

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50

McDougall, Kristin. "Micropaleontological Evidence of A Submarine Fan in the Lower Coaledo Formation, Southwestern Oregon, USA". Journal of Foraminiferal Research 53, n.º 4 (1 de octubre de 2023): 311–37. http://dx.doi.org/10.61551/gsjfr.53.4.311.

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Abstract The middle Eocene lower Coaledo Formation was interpreted as ten shoaling upward delta-margin cycles based on sediments and macrofauna. The strata, however, contains deep-water foraminifers. Explanations to resolve this anomaly included reworking, bathymetric range extension, or upward migration of water masses. Paleoecology analysis of foraminifers indicates that the few shelf species are poorly preserved whereas the well-preserved lower bathyal species dominate, and planktic organisms are present. Evidence for reworking, bathymetric range extension, or upward migration of water masses was not found in any of the cycles. The paleoecologic utility of hummocky cross-bedded sandstones is questioned as these features are controversial. In addition, there is no evidence of sea-level changes or tectonic activity to accommodate the bathymetric changes needed. Deposition of the lower Coaledo Formation on a submarine fan at lower bathyal depths eliminates the need to explain bathymetric anomalies or lack of tectonic movement.
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