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TABLE 1. Surface-sample studies.
NAME STATE LATIT. LONGIT. #SPL #TYP REFERENCE
1. ALBI* ID 42o20' 113o40' 63 42 Davis, 1984
2. ANIM CO 37o45' 107o45' 38 40 Maher, 1963
3. ARCH AZ CA (archeological) 35 54 OKD, unpubl. & West, 1977
4. BTCH# CA 38o00' 119o00' 11 15 Batchelder, 1970
5. CARS CA 38o45' 120o15' 12 33 Adam, 1967
6. CHEL*# AZ 36o15' 109o15' 20 27 Fall, 1987
7. CHSV# NM 36o15' 109o00' 36 13 Harris et al., 1967
8. CHUS NM 36o15' 109o00' 39 15 Bent and Wright, 1963
9. CJHE# WA 46o51' 121o46' 25 34 Heusser, 1973
10. CNTA# AZ 33o30' 111o30' 15 22 Schoenw. and Dorsch., 1971
11. CNTW WA 47o00' 119o00' 78 12 Mack and Bryant, 1974
12. COMO CO 37o30' 105o30' 9 12 Shafer, 1989
13. CRDY AZ 34o00' 110o00' 48 31 Rankin, 1980
14. FKIN# AZ 32o05' 111o00' 8 12 King, 1977
15. GATC# NV 38o50' 116o45' 56 9 Thompson, 1983
16. GDSR* MX 32o00' 113o00' 4 17 O.K. Davis, Unpubl.
17. HEVL# AZ 34o15' 109o50' 20 9 Hevly, 1968
18. HHLO# AZ 35o00' 110o00' 20 7 Hevly, 1968
19. HNRY# ID 43o00' 116o00' 16 18 Henry, 1984
20. HVMR* AZ 31o15' 119o50' 13 27 Hevly and Martin, 1961
21. INEL ID 43o30' 112o40' 6 26 Bright and Davis, 1982
22. KNGC AZ 36o15' 112o15' 22 42 King & Sigleo, 1973
23. KYLE# NV 36o15' 115o30' 21 26 Mehringer, 1967
24. LPLT CO 37o30' 107o45' 9 15 Petersen & Scott 87, & Mehr .76
25. MCWNS WY SD SD ND 71 43 McAndrews and Wright, 1969
26. MRTN,2* AZ 32o00' 110o00' 52 33 Martin, 1963; Tables 1 & 3
27. NMHL#! NM TX 32 4O Hall, 1990; Rogers et al. 1985
28. NVJR# AZ 36o30' 108o30' 19 14 Schoenwetter & Eddy, 1964
29. OAX1,2,3 MX 17o00' 97o00' 180 33 Schoenwetter & Smith, 1986
30. PANM CA 36o30' 117o15' 13 6 Mehringer, 1967
31. PFAL*# CO 38o50' 107o05' 34 18 Fall, 1988
32. PRCO NM 35o30' 107o30' 24 29 Pippin, 1979
33. PRKN AZ 35o00' 112o15' 5 17 Fish, unpublished
34. RUBM# NV 41o15' 115o30' 20 7 Thompson, 1984
35. SEQU CA 36o00' 120o00' 19 62 Anderson, 1990
36. SERL# CA 35o30' 117o30' 11 9 Leopold, 1967
37. SIER* CA 37o30' 119o15' 44 69 Anderson and Davis, 1988
38. SIGL AZ 36o15' 112o15' 25 28 King & Sigleo, 1973
39. SINA# MX 23o12' 106o26' 28 23 Jacobs, 1982
40. SNAG NM 34o00' 108o00' 5 31 Potter Rowley, 1960
41. SNMN NM 37o00' 104o00' 24 15 King, 1967
42. SONT AZ 31o30 110o10' 3 13 Mehringer Haynes Adam
43. STAF NM 35o45' 106o15' 6 9 Dixon, 1962
44. SWLN# ID 42o33' 112o00' 7 29 Bright, 1967
45. TIOG CA 37o45' 119o15' 21 35 Adam, 1967
46. WALH AZ 36o30' 112o15' 3 22 Schoenwetter, 1982
47. WASS AZ 32o20' 111o15' 22 31 Hevly et al., 1965
48. WHTM# AZ 34o00' 109o30' 9 18 Batchelder and Merrill, 1976
49. WORE# OR 44o50' 123o30' 55 15 Heusser, 1978
50. WTRM AZ 32o30' 111o30' 5 46 Anderson and Van Devender, 1991
* Includes lake sediment or moss polsters
! Includes Tauber samples
# Data digitized from figure.TABLE 2. Variables in surface sample database: environmental variables and pollen types.
ENVIRONMENTAL VARIABLE CODE EXAMPLE RANGE
Site Name SITEID ALBI
Site Sample Number SAMPNO 1
Latitude LATT 42.33 17 - 47
Longitude LONG 133.67 97 - 124
Mean Precip. (mm) PRCP 253 14 - 8988
Mean Annual Temp. (C) TEMP 15 -3 - 23
Elevation (m) ELEV 3000 0 - 3949
Vegetation Type VEGTYP RMSA
# OF -------- FREQUENCY > % --------- AVE.
POLLEN CODE LOC. 90 60 30 10 5 2 0 >0%
Abies ABIE 29 0 1 11 63 118 246 360 6
Alnus ALNU 27 12 32 54 68 90 237 416 11
Ambrosia AMBR 39 0 19 62 217 383 615 792 10
Arceuthobium ARCU 7 0 0 0 0 0 10 38 1
Artemisia ARTE 39 0 35 214 400 521 707 835 18
Cactaceae CACT 14 0 0 0 0 5 14 45 2
CaryophyllaceaeCARY 11 0 0 0 2 7 12 65 2
Chrysolepis CHRY 4 0 0 1 1 2 7 18 6
Celtis CELT 11 0 0 0 2 3 24 67 2
Cercocarpus CERC 10 0 0 4 8 11 46 87 4
Cheno. - Amar. CHAM 49 2 49 178 505 828 1098 1217 14
Compositae OCOM 49 1 44 167 393 678 1035 1189 13
Cruciferae CRUC 12 0 0 0 3 8 29 75 2
Cupressaceae CUPR 45 0 3 34 254 420 663 772 9
Cyperaceae CYPE 23 0 2 7 29 57 140 249 5
Ephedra EPHD 35 0 0 4 26 56 124 291 4
Eriogonum ERIO 22 0 0 0 1 9 43 127 2
Euphorbia EUPH 10 0 0 0 0 4 14 72 2
Fraxinus FRAX 8 0 0 0 0 0 0 22 1
Ferns FRNS 10 0 0 0 4 19 30 67 4
Gramineae GRAM 45 0 5 92 453 739 965 1159 11
Larrea LARR 8 0 0 0 1 3 12 43 2
Leguminosae LEGU 18 0 0 0 3 7 45 164 2
Liguliflorae LIGU 17 0 0 0 1 4 13 101 2
Malvaceae MALV 16 0 0 0 2 2 6 61 2
Nyctaginaceae NYCT 10 0 0 0 1 2 4 45 2
Picea PICE 25 0 1 17 60 85 125 273 7
Pinus PINU 50 3 142 422 921 1090 1215 1333 26
Polygonaceae POLG 16 0 0 0 0 0 7 79 1
Populus POPU 18 0 0 0 2 6 31 154 2
Prosopis PRSP 10 0 0 0 1 9 28 105 2
Pseudotsuga PSED 24 0 0 2 18 31 67 218 4
Quercus QURC 43 0 2 18 98 218 429 801 5
Rhamnaceae RHMN 11 0 0 0 3 6 14 60 3
Salix SALX 22 0 0 0 0 2 8 130 1
Sarcobatus SARC 24 0 1 3 14 25 46 210 3
Sequoiadendron SEQU 1 0 2 7 12 16 18 19 25
Tsuga heteroph.TSHT 5 0 0 0 5 15 34 56 5
T. mertensiana TSMR 2 0 0 1 4 12 28 58 4
Umbelliferae UMBL 18 0 1 1 4 14 29 139 3
[RETURN]
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Davis, O.K. 1995. Indices and tables of contents for AASP
publications: GEOSCIENCE AND MAN vols 1, 3, 4, 7, 9, 11, 13,
and 15, and PALYNOLOGY vols. 1-19. AASP Data Committee,
PALYDISK 16. This palydisk contains a table of contents and indices for the journal "PALYNOLOGY" and certain issues of "GEOSCIENCE AND MAN." Seven of the "GEOSCIENCE AND MAN" volumes are AASP publications containing palynology articles, the proceedings and abstracts of the annual meeting, and the group photograph. Volume 13 is a Pleistocene volume containing several palynology articles, but is not an official AASP volume. There are 19 "PALYNOLOGY" volumes, through 1995. The date are in 4 ASCII files: readme.txt (this file) age.txt authors.txt topics.txt volumes.txt
AGE.TXT
Each article is assigned a geological age, if possible. For this
first attempt, I used the one-letter age codes that are being
used for the SECOND WORLD DIRECTORY OF PALYNOLOGISTS (see
"PALYNOS" 1994 7:2). It appears that I must adopt a different
code for this index, and subdivide the Mesozoic (sorry to all you
Mesozoic authors.)
Each entry includes the first author, date, first line of the
title, journal, volume, and first page number. For example
PALEOZOIC
Barss, M.S. 1972 A problem in Pennsylvanian - Permian palynology
of Yukon Territory. G&M 4 67
Bunner, W.D. 1988 A new species of Dicommopalla (Acritarcha) from
the Middle Ordovician PAL 13 57
AUTHORS.TXT
A list of the authors in the G&M and PALY volumes. Name followed
by the date of the publication, journal, volume, first page, and
the position of the author's name (first (1), second (2)...).
Traverse, A. 1971 G&M 3 37 (2)
Traverse, A. 1971 G&M 3 65 (2)
Traverse, A. 1972 G&M 4 87 (1)
Traverse, A. 1973 G&M 7 39 (2)
Traverse, A. 1973 G&M 7 57 (2)
Traverse, A. 1975 G&M 11 1 (2)
Traverse, A. 1975 G&M 11 145 (1)
Traverse, A. 1976 G&M 15 141 (1)
Traverse, A. 1979 PAL 3 1 (2)
Traverse, A. 1982 PAL 6 203 (3)
Traverse, A. 1983 PAL 7 7 (1)
Traverse, A. 1986 PAL 10 225 (2)
TOPICS.TXT
Likewise the WDII codes were included for the subject matter
(Paleopalynology, Environmental Palynology, Morphology . . .) and
palynomorph types (Dinoflagellates, Spores, Pollen . . .). These
entries are hierarchical, with palynomorph subheadings within
topical headings:
MODERN DISTRIBUTION
DINOFLAGELLATES
Harland, R. Recent Dinoflagellate Cyst Assemblages from the
Southern Barents Sea PAL 6 9
McMinn, A. Recent and Late Quaternary dinoflagellate cyst
distribution on the PAL 16 13
VOLUMES.TXT
These are the tables of contents as copied from the two journals.
GEOSCIENCE & MAN VOL. 1
Jenkins, W.A.M. 1970 Chitinozoa. G&M 1 1-22
Terasme, J. 1970 Quaternary palynology -- its scope, problems and
potential uses. G&M 1 23-28
[RETURN]
Ravn, R.L. 1998. TAXON: a DOS hypertext database of 30,000 species of palynomorphs with references and annotations. AASP Data Committee, PALYDISK 17. This program uses the DOS program FIND.EXE. If you don't have "FIND.EXE" on your computer, "TAXON" will not run. TO INSTALL CREATE new subdirectory named "TAXON". COPY the Paly17.exe file to it and type Paly17 [Enter] to unzip the 5 diskettes included in the Palydisc. On DOS-only Computers: go to the "TAXON" subdirectory and type TAXON [Enter]. For Windows Computers: open a DOS window and go to the "TAXON" subdirectory. Type "Taxon32" [Enter].
- - - - - - - - - - - - - - - - - - - - | TAXON v 3.1 | | Welcome . . . Continue Y/N | R.L. Ravn . . . . - - - - - - - - - - - - - - - - - - - -Type "Y" [Enter] and the next screen should appear - - - - - - - - - - - - - - - - - - - - | | SEARCH FOR WHAT? [Enter] WHERE? | ____________________ ____ | | |- - - - - - - - - - - - - - - - - - - -| | Q [Enter] = quit, G [Enter] = Genera | I [Enter] = taxa index, S [Enter] = | stratigraphic column | A [Enter] = About TAXON - - - - - - - - - - - - - - - - - - - -Enter (for example) "Ovoid" [Enter] under "SEARCH" and "P5" under "WHERE," the screen should say "FINDING 'Ovoid' IN ___" Then produce the following printout - - - - - - - - - - - - - - - - - - - - | [10000] Ovoidites parvus (Cookson & Dettmann)Follow the instructions on the screen for other options. Thereafter, change to the appropriate directory and type "TAXON" to run the program. [RETURN]
Rochon, A., de Vernal, A., Turon, J.-L, Mattheissen, J., and Head, J.J. 1999. Distribution of Recent Dinoflagellate Cysts in Surface Sediments from the North Atlantic Ocean and Adjacent Seas in Relation to Sea-surface Parameters. Data Files and Tables from AASP Foundation Contibutions Series 35. AASP Data Committee, PALYDISK 18. This palydisk contains the following tables and data from AASP Foundation Contibutions Series 36:
Lentin, J. 2000. ANGIOASK.EXE and DINOASK.EXE Graphical Keys for Palynomorph Identification. Data Files and Tables from AASP Foundation Contibutions Series 35. AASP Data Committee, PALYDISK 19. This palydisk contains two DOS programs that are picture-keys for the identification of pollen (ANGIOASK.EXE) or dinoflagellate cysts (DINOASK.EXE). A 34 page manual, written in MS Word, is included. Operation of the programs is simple and intuitive. Unpack the "paly19.exe" zip file by "running" it from a dos prompt, windows "run," or windows "explorer." Once the palydisk is unzipped, either ANGIOASK or DINOASK can be run in a DOS window. The initial screen displays (one page at a time) the palynomorph characters. Simply click (quick tap!) one one or more of the graphical images to select each character, use [page up] or [page down] to move among the hundreds of images, then touch or click on [F1 - Select] to produce a list of the palynomorphs with all of the selected characters. Click on the letter codes of this list to read detailed bibliographic data for each palynomorph. [RETURN]
Rull, V. 2003. 'Contribution of Quantitative Ecological Methods to the Interpretation of Stratigraphically Homogeneous pre-Quaternary Sediments: A Palynological Example from the Oligocene of Venezuela.' Appendix for: Palynology 27: 75-98 AASP Data Committee PALYDISK 20. Taxa are described (no illustrations), with references. example: Bombacacidites Couper 1960 spp. Summary class including several morphologies belonging to the genus. The form-genus Bombacacidites has its botanical affinity with the family Bombacaceae, of which practically all representatives are trees growing in tropical rain forests and savannas (Fuchs, 1964). Common along rivers and creeks (Hoorn, 1994). MS Word file (.doc) [RETURN]
Rull, V. 2003. Synoptic pollen descriptions and complete bibliography. Appendix for, "An illustrated key for the identification of pollen from Pantepui and the Gran Sabana (eastern Venezuelan Guayana). Palynology 27: 99-134." AASP Data Committee, PALYDISK 21. Refers to pollen illustrated in plates in Palynology 27: 99-134. example: Alismataceae Sagittaria sp (plate 8: 263-266) - Herbarium information:VEN 86913. Det. Steyermark. Leg. J. Velásquez, feb. (1970, nº 1058. Loc. Edo. Guárico, Lag. El Burro, Sta Rita. - Acetolysis: MARAVEN s/n (1991). - Description: Monads. Spheroidal, apolar. Pantoporate (5 or more pores), pores circular/elliptical, inconspicuous, difficult to observe (grains sometimes appearing as inaperturate). Exine thin (1-2 um), intectate, microechinate (spines < 1 um); sexine and nexine difficult to distinguish. Grain size (excluding spines): 27-33 x 24-32 um. - References: Wodehouse (1936), Bogin (1955), Ikuse (1956), Huang (1970), Heuser (1971), Argue (1972, 1974, 1976), Hesse (1980, 1981), Melhem and De Abreu (1981), Payne (1981), Punt and Reumer (1981), Caccavari (1983), Rogers (1983), Zavada (1983). Andrew (1984), Majeed Kak (1984), Chanda et al. (1988), Mondal (1989), Moore et al. (1991), Roubik and Moreno (1991), Colinvaux et al. (1999), [RETURN]
Helenes, J. and Cabrera, D. 2003. Abundances and diversities of palynomorphs in wells one, two and three. Excel data tables to accompany, "Oligocene-Miocene palynomorph assemblages from eastern Venezuela. Palynology 27: 5-26. AASP Data Committee, PALYDISK 22. example:
Pardo-Trujillo, A., Jaramillo, C.A., and Oboh-Ikuenobe, F.E. 2003. Appendix 1. palynomorphs in the Uribe section. Appendix 2. palynomorphs in the Sogamoso core. Appendices for "Paleogene palynostratigraphy of the eastern Middle Magdalena Valley, Colombia (Palynology volume 27, 2003)."MS Excel file. AASP Data Committee PALYDISK 23. example:
Jaramillo, C.A., Bayona, G., Pardo-Trujillo, A., Rueda, M., Torres, V., Harrington, G.J. and Mora, G. 2007. Appendices to accompany, "The Palynology Of The Cerrejón Formation (Upper Paleocene) Of Northern Colombia." Palynology: 31: 153-189. MS zip file. AASP Data Committee PALYDISK 24. abstr: A palynological study of the Cerrejon Formation was conducted in order to date the formation and understand the floristic composition and diversity of a Paleocene tropical site. The Cerrejon Formation outcrops in the Cerrejon Coal Mine, the largest open cast coal mine in the world. Two cores (725 m) were provided by Carbones del Cerrejon LLC for study. Two hundred samples were prepared for palynology, and at least 150 palynomorphs were counted per sample where possible. Several statistical techniques including rarefaction, species accumulation curves, detrended correspondence analysis, and Anosim were used to analyze the floristic composition and diversity of the palynofloras. Palynomorph assemblages indicate that the age of the Cerrejon Formation and the overlying Tabaco Formation is Middle to Late Paleocene (ca. 60–58 Ma). Major structural repetitions were not found in the Cerrejon Formation in the Cerrejon coal mine, and there is little floral variation throughout. The floral composition, diversity, and lithofacies do not change significantly. Lithofacies associations and floral composition indicate deposition fluctuating from an estuarine-influenced coastal plain at the base to a fluvial-influenced coastal plain at the top. There are, however, significant differences in the composition and diversity of coal and siliciclastic samples. Coal palynofloras have fewer morphospecies, and a distinct and more homogeneous floral assemblage compared to assemblages from the intervening sisliciclastic strata, suggesting that tropical swampy environments supported fewer plant species and had a distinct vegetation adapted to permanently wet environments.
Jardine, P. and Harrington, G. 2008. Appendices to accompany, "The Red Hills Mine Palynoflora: A diverse swamp assemblage from the Late Paleocene of Mississippi, U.S.A." Palynology: 32: 183-204. MS Excel file. AASP Palydisk Committee PALYDISK 25. abstr: Lignites from the Red Hills Mine in Mississippi, U.S.A. contain pollen and spores derived from paratropical swamp vegetation on the U.S. Gulf Coast during the Late Paleocene. Most previous studies of the Gulf Coast sporomorph record have been limited to a restricted taxonomic group, or merely those taxa that are relevant to biostratigraphy, meaning that the true sporomorph diversity may be higher than previously appreciated. Eight samples were collected for palynological analysis from the Red Hills Lignite Mine in Ackerman, Mississippi. All the taxa observed during counting (a minimum of 300 grains per sample) were included in the sample count. Rarefaction, relative abundance distributions, and non-metric multidimensional scaling were used to analyze floral composition, richness, and evenness. The lignite samples are heterogeneous in terms of composition and relative abundances, indicating patchiness in the swamp communities. Clay horizons representing temporary marine incursions contain significantly higher proportions of bisaccate pollen, which may have originated a considerable distance inland from the swamps. These samples therefore represent a much larger source area (regional to sub-continental), compared to the local signal contained in the lignite samples. Richness in the Red Hills Mine assemblage is higher than has previously been recorded for the Late Paleocene of the eastern Gulf Coast. This, combined with the recognition of 23 previously undescribed taxa, suggests that a detailed reappraisal of the Gulf Coast Paleocene sporomorph record is needed to improve understanding of the evolution of the North American vegetation type. example:
Davis, O. K., 2010. Kounter.exe — a dos program (written 1985) for counting pollen. This program runs in a Windows (16, 32 bit) dos window and maps each keyboard key to a different pollen type. It automatically tallies the pollen sum and beeps when the set pollen sum is exceeded. Lower case and upper case keys are included in the pollen sum. Control- and Alt- keys are outside the sum. zip file. PALYDISK 26.
(comments in yellow)
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