Knowledge (XXG)

Princeton Chert

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20: 327:) are just some of the angiosperms found both today and in the Princeton Chert. Seeds have also been found which share adaptations with living aquatics. On the other hand, terrestrial fossils have rarely been found. The few that are, are represented mainly by seeds, some of which may have been transported by birds. 182:
and during the Early Eocene Climatic Optimum. During this time the sea warmed approximately 4 °C and terrestrial temperatures were several degrees warmer than today, meaning little or no ice was present at the poles. The temperature difference between poles and equator was small. This long term
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conditions. More recent analysis of the fossil flora, however reconstructs for the Princeton Chert flora a moist warm temperate climate with mean annual temperature 13.1 ± 3.1 °C, with mild winters (cold month mean temperature 5.3 ± 2.8 °C), and mean annual precipitation 114 ± 42 cm
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into the low lying basin where the Princeton chert was located. Here, the water surrounded organisms as they grew, along with plant debris which had been accumulated. Many organisms were preserved in situ, in the lake or small pond environment in which they lived. The preservation must have been
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found, which has preserved plants and animals in minute 3D detail, with exceptional internal cellular detail. This has meant anatomical descriptions and reconstruction of whole plants from isolated parts has been possible in many species. Few plant fossils elsewhere in the world exhibit such
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lacunae surrounded by a ring of cells with thickened inner walls. Further evidence is provided by the fossils’ clear affinities with modern aquatic angiosperms. Many extant plants show these adaptations and are similar to the organisms found in the chert. For example, water lilies
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The Princeton Chert (Ashnola shale in older sources) and its fossils have been known since the 1950s, but have attracted increased attention in the late 1970 and on. This may be due to the rare type of silica permineralized fossil
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rapid, due to the minute cellular detail which has been conserved. This sequence of events is thought to have been replicated up to 50 times, as the basin allowed peat to re-accumulate each time, producing the multiple layers.
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Greenwood, DR; Archibald, SB; Mathewes, RW; Moss, PT (2005). "Fossil biotas from the Okanagan Highlands, southern British Columbia and northeastern Washington State: climates and ecosystems across an Eocene landscape".
140:. 49 chert layers, ranging in thickness from 1 to 55 cm (0.39 to 21.65 in) have been recognized and described, though each is not unique in organisms preserved. Despite this, trends are evident throughout the 4650:
Klymiuk, A. A. (2016). "Paleomycology of the Princeton Chert. III. Dictyosporic microfungi, Monodictysporites princetonensis gen. et sp. nov., associated with decayed rhizomes of an Eocene semi-aquatic fern".
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layers, indicating nearby volcanic activity. It is thought that fossils were pervaded with silicic acid due to this volcanic activity. Subsequently, water charged with minerals flowed from springs or
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Sampling into the Princeton Chert has been carried out, but presently the data has not been analysed in detail. Across the outcrop, trends in taxa can be seen; in the topmost layers fossil organs of
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Pigg, K. B.; Stockey, R. A.; Maxwell, S. L. (1993). ""Paleomyrtinaea", a new genus of permineralized myrtaceous fruits and seeds from the Eocene of British Columbia and Paleocene of North Dakota".
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Moss, PT; Greenwood, DR; Archibald, SB (2005). "Regional and local vegetation community dynamics of the Eocene Okanagan Highlands (British Columbia - Washington State) from palynology".
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Klymiuk, A.A.; Taylor, T.N.; Taylor, E.L.; Krings, M. (2013). "Paleomycology of the Princeton Chert I. Fossil hyphomycetes associated with the early Eocene aquatic angiosperm,
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Ickert, RB; Thorkelson, DJ; Marshall, DD; Ullrich, TD (2009). "Eocene adakitic volcanism in southern British Columbia: Remelting of arc basalt above a slab window".
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Mustoe, G. E. (2010). "Cyclic sedimentation in the Eocene Allenby Formation of south-central British Columbia and the origin of the Princeton Chert fossil beds".
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Dillhoff, RM; Dillhoff, TA; Greenwood, DR; DeVore, ML; Pigg, KB (2013). "The Eocene Thomas Ranch flora, Allenby Formation, Princeton, British Columbia, Canada".
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Bijl, P. K.; Houben, A. J. P.; Schouten, S.; Bohaty, S. M.; Sluijs, A.; Reichart, G.; Damsté, S.; Brinkhuis, H. (2010). "Transient Middle Eocene Atmospheric CO
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Erwin, D.M.; Stockey, R.A. (1994). "Permineralized monocotyledons from the middle Eocene Princeton chert (Allenby Formation) of British Columbia: Arecaceae".
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at this time was warm; it had reached a maximum during a series of warming events during the Early Eocene with the Princeton Chert likely deposited after the
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Cevallos-Ferriz, S. R.; Stockey, R. A. (1989). "Permineralized fruits and seeds from the Princeton chert (Middle Eocene) of British Columbia: Nymphaeaceae".
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Erwin, DM; Stockey, RA (1989). "Permineralized monocotyledons from the Middle Eocene Princeton chert (Allenby Formation) of British Columbia: Alismataceae".
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or lake environment. The plant fossils found show many structural and anatomical adaptations to an aquatic environment, including a reduced vascular system,
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Cevallos-Ferriz, S. R.; Stockey, R. A. (1988). "Permineralized fruits and seeds from the Princeton chert (Middle Eocene) of British Columbia: Lythraceae".
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Little, Stefan A.; Stockey, Ruth A.; Penner, Bonnie (March 2009). "Anatomy and development of fruits of Lauraceae from the Middle Eocene Princeton Chert".
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Pigg, KB; Stockey, RA (1996). "The significance of the Princeton chert permineralized flora to the middle Eocene upland biota of the Okanogan Highlands".
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Cevallos-Ferriz, S. R.; Stockey, R. A. (1990). "Permineralized fruits and seeds from the Princeton chert (Middle Eocene) of British Columbia: Vitaceae".
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Erwin, D. M.; Stockey, R. A. (1991). "Silicified monocotyledons from the Middle Eocene Princeton chert (Allenby Formation) of British Columbia, Canada".
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Close up of Princeton Chert outcrop showing volcanic ash (white layer at base), peaty coal (dark layer), and Chert layers (grey). Layer 36 is labelled.
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Cevallos-Ferriz, S. R.; Stockey, R. A. (1990). "Vegetative remains of the Magnoliaceae from the Princeton chert (middle Eocene) of British Columbia".
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Erwin, D. M.; Stockey, R. A. (1992). "Vegetative body of a permineralized monocotyledon from the Middle Eocene Princeton chert of British Columbia".
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Erwin, D. M.; Stockey, R. A. (1990). "Sapindaceous flowers from the Middle Eocene Princeton chert (Allenby Formation) of British Columbia, Canada".
264:, after a huge ash fall, though few angiosperms occur in these layers. A large number of angiosperms have been found along with several types of 3418:
Karafit, S. J.; Rothwell, G. W.; Stockey, R. A.; Nishida, H. (2006). "Evidence for sympodial vascular architecture in a filicalean fern rhizome:
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Cevallos-Ferriz, S; Stockey, RA (1988). "Permineralized fruits and seeds from the Princeton Chert (Middle Eocene) of British Columbia: Araceae".
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pollen from the Cretaceous and Paleogene of North America and West Greenland: Implications for the origin and palaeobiogeography of the genus"
2232:"A review of paleobotanical studies of the Early Eocene Okanagan (Okanogan) Highlands floras of British Columbia, Canada and Washington, USA" 2054: 381: 330:
Additional support for the aquatic nature of the Princeton Chert deposits comes from animal fossils. Several fossils of a freshwater fish,
4146:"The first Odonata from the early Eocene Allenby Formation of the Okanagan Highlands, British Columbia, Canada (Anisoptera, Aeshnidae and 4726: 4434:
Robison, C. R.; Person, C. P. (1973). "A silicified semiaquatic dicotyledon from the Eocene Allenby Formation of British Columbia".
89: 2609:
Wilson, MVH (1980). "Eocene lake environments: Depth and distance-from-shore variation in fish, insect, and plant assemblages".
4761: 1879: 2491:"Great Canadian Lagerstätten 1. Early Eocene Lagerstätten of the Okanagan Highlands (British Columbia and Washington State)" 195:
decarbonation reactions. This happened because the ocean between India and Asia was disappearing and being replaced by the
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Klymiuk, A. A.; Stockey, R. A.; Rothwell, G. W. (2011). "The first organismal concept for an extinct species of Pinaceae:
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Cevallos-Ferriz, S. R.; Stockey, R. A.; Pigg, K. B. (1991). "The Princeton chert: evidence for in situ aquatic plants".
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LePage, B. A.; Currah, R. S.; Stockey, R. A.; Rothwell, G. W. (1997). "Fossil ectomycorrhizae from the middle Eocene".
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Currah, R.S.; Stockey, R.A.; LePage, B.A. (1998). "An Eocene tar spot on a fossil palm and its fungal hyperparasite".
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gen. et sp. nov., a permineralized monocotyledon from the Middle Eocene Princeton chert of British Columbia, Canada".
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Stockey, R. A.; Nishida, H.; Rothwell, G. W. (1999). "Permineralized ferns from the middle Eocene Princeton chert. I.
2094: 191:
is unknown, but it is hypothesised that it was due to an increase in ocean floor being recycled via volcanic arcs and
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Stockey, RA; Wehr, WC (1996). "Flowering plants in and around Eocene lakes of the interior". In Ludvigsen, R. (ed.).
1250: 2110: 1621: 1292: 658: 276:
The array of floral and faunal fossils found in the Princeton Chert has offered unequivocal evidence that it was a
93: 3899:
Hesse, M.; Zetter, R. (2005). "Ultrastructure and diversity of recent and fossil zona-aperturate pollen grains".
589: 336:(bowfin), have been found in the shale overlying the plant deposits, along with remains of the freshwater fishes 3250:
Currah, RA; Stockey, RA; LePage, BA (1998). "An Eocene tar spot on a fossil palm and its fungal hyperparasite".
2874: 1416: 1132: 1012: 179: 4741: 1779: 972: 934: 626: 2644:
Hills, LV; Baadsgaard, H (1967). "Potassium-argon dating of some Lower Tertiary strata in British Columbia".
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Cevallos-Ferriz, SRS; Stockey, RA; Pigg, KB (1991). "Princeton chert: evidence for in situ aquatic plants".
1813: 557: 4696: 1979: 4736: 2044: 2019: 1207: 868: 2853:
Greenwood, D.R.; Wing, S.L. (1995). "Eocene continental climates and latitudinal temperature gradients".
2415: 1934: 1769: 1442: 757: 1739: 1542: 2084: 1584: 3192:
Pollen Cones from the Middle Eocene Princeton Chert (Allenby Formation) of British Columbia, Canada".
1706: 1378: 1240: 1122: 813: 648: 260: 4731: 4493: 4206: 3908: 3813: 3770: 3587: 3552: 3075: 2967: 2912: 2862: 2817: 2775: 2734: 2725:
Bohaty, SM; Zachos, JC (2003). "Significant Southern Ocean warming event in the late middle Eocene".
2672: 2618: 2583: 2463: 2243: 1332: 791: 109: 2215:
Boneham, R.F. (1968). "Palynology of three Tertiary coal basins in south-central British Columbia".
1282: 835: 223: 1002: 579: 305: 4676: 4632: 4540: 4264: 4243:"Vegetative remains of the Rosaceae from the Princeton chert (Middle Eocene) of British Columbia" 4171: 4126: 4037: 3967: 3924: 3743: 3678: 3603: 3525: 3486: 3439: 3400: 3321: 3305: 3267: 3209: 3170: 3001: 2936: 2878: 2357: 2322: 2070: 1893: 1054: 924: 156: 97: 3340: 1958: 1803: 1551: 1532: 3341:"An annotated catalog of fossil and subfossil Lepidoptera (Insecta: Holometabola) of the world" 1913: 1406: 616: 4668: 4624: 4416: 4336: 3959: 3839: 3508:
gen. et sp. nov.(Blechnaceae): a permineralized fern from the Middle Eocene Princeton Chert".
3478: 3313: 2993: 2928: 2835: 1869: 1348: 215: 164: 137: 59: 55: 51: 2547:
Stockey, R. A. (1987). "A permineralized flower from the Middle Eocene of British Columbia".
2490: 1696: 4660: 4614: 4606: 4570: 4532: 4501: 4484:(Magnoliopsida; family indet.) from the Middle Eocene Princeton chert of British Columbia". 4443: 4406: 4368: 4326: 4291: 4254: 4214: 4161: 4118: 4091: 4064: 4029: 3994: 3951: 3916: 3829: 3821: 3778: 3735: 3670: 3634: 3595: 3560: 3517: 3470: 3431: 3392: 3352: 3297: 3259: 3201: 3162: 3128: 3083: 3041: 2983: 2975: 2920: 2870: 2825: 2783: 2742: 2707: 2680: 2626: 2591: 2556: 2471: 2431: 2391: 2382:, gen. et sp. nov., permineralized flowers (Rosaceae) from the Eocene of British Columbia". 2349: 2314: 2261: 2251: 1729: 1322: 667: 371: 315: 291: 219: 85: 32: 19: 1216: 1197: 1096: 1074: 954: 410: 200: 47: 76: 4701: 4497: 4210: 3912: 3817: 3774: 3591: 3556: 3079: 2971: 2916: 2866: 2821: 2779: 2738: 2676: 2622: 2587: 2467: 2247: 413:
from the fossil record, with the fungi suggested as close to the modern pine symbiotics
4716: 3834: 3797: 3381:
Robison and Person from the Middle Eocene Princeton chert locality of British Columbia"
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Lepage, BA; Currah, RS; Stockey, RA (1994). "The fossil fungi of the Princeton chert".
1687: 943: 376: 4219: 4195:(Cornaceae, Mastixioideae) from the middle Eocene Princeton chert of British Columbia" 4190: 2489:
Archibald, S.B.; Greenwood, D.R.; Smith, R.Y.; Mathewes, R.W.; Basinger, J.F. (2012).
4710: 4505: 4175: 3782: 3564: 3376: 3339:
Sohn, Jae-Cheon; Labandeira, Conrad; Davis, Donald; Mitter, Charles (30 April 2012).
3087: 3005: 2882: 2630: 1998: 1387: 338: 148: 4544: 4268: 4130: 4041: 3971: 3747: 3682: 3607: 3529: 3490: 3443: 3404: 3325: 3213: 3174: 3149:
Smith, SY; Stockey, RA (2003). "Aroid seeds from the Middle Eocene Princeton chert (
2940: 2361: 4680: 4636: 4574: 4016:(Lythraceae) from the Middle Eocene Princeton chert with anatomical comparisons to 3928: 3825: 2036: 2012: 1972: 1951: 1611: 1341: 1313: 1260: 1231: 1063: 915: 739: 300: 296: 228: 168: 129: 40: 360:
have been recorded on the leaves and other organs of some vascular plants. Fossil
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Fossil protection in British Columbia (Land Act: Reserves, Sections 15, 16 or 17)
2684: 2063: 1888: 1860: 1593: 1566: 1554: 1523: 766: 747: 700: 678: 635: 608: 598: 566: 539: 402: 386: 192: 2806:"An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics" 4259: 4242: 3920: 3357: 2140: 2103: 1927: 1905: 1788: 1748: 1368: 1189: 1021: 981: 962: 547: 415: 344: 324: 285: 281: 277: 208: 104:, about 160 km (160,000 m) NNW of the Princeton Chert beds, and the 2595: 2979: 2924: 1752: 1360: 1301: 1273: 1171: 1153: 1141: 1113: 1036: 366: 320: 204: 196: 4672: 4628: 4420: 4340: 4331: 4310: 3963: 3843: 3482: 3317: 2997: 2932: 2839: 2256: 2231: 159:
techniques provided a date of 48.7 mya, placing the Princeton Chert in the
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excellence in both preservation and diversity. Similar aged fossil beds in
4411: 4390: 2711: 254:(pine) and monocotyledons increase in number. There is a huge increase in 183:
warmth is thought to be due to increased greenhouse gases, particularly CO
1822: 1673: 1653: 1630: 1604: 1574: 1398: 776: 265: 160: 101: 4166: 4145: 3955: 2830: 2805: 3599: 3309: 3271: 2988: 2326: 2146: 1024: 993: 686: 421: 310: 232: 175: 152: 141: 4619: 2266: 155:, freshwater fish, and potassium-argon dates. Recently, more accurate 3702:
Contributions from the Museum of Paleontology, University of Michigan
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Miller Jr, C. N. (1973). "Silicified cones and vegetative remains of
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Contributions from the Museum of Paleontology, University of Michigan
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Contributions from the Museum of Paleontology, University of Michigan
1755: 1509: 1489: 1469: 1451: 1433: 495: 332: 81: 44: 36: 4447: 4372: 4295: 4095: 4068: 3998: 3638: 3504:
Smith, S. Y.; Stockey, R. A.; Nishida, H.; Rothwell, G. W. (2006). "
3301: 3263: 3132: 3045: 2787: 2574:
Russell, LS (1935). "A middle Eocene mammal from British Columbia".
2475: 2435: 2395: 2318: 4664: 4610: 4536: 4122: 4033: 3739: 3674: 3578:
Collinson, M. E. (2001). "Cainozoic ferns and their distribution".
3521: 3474: 3435: 3396: 3205: 3166: 2353: 2230:
Greenwood, D.R.; Pigg, K.B.; Basinger, J.F.; DeVore, M.L. (2016).
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Little & Stockey (2003) provided a whole plant reconstruction
1082: 1045: 782: 405:, and found to be very similar. The mycorrhizal relationship with 362: 357: 250: 133: 125: 18: 2196:
Arnold, C. A. (1955). "A Tertiary Azolla from British Columbia".
2173:
Miller, C.N. (1975). "Silicified cones and vegetative remains of
268:, ferns, and several unidentified fossils from various families. 877: 844: 822: 800: 255: 227:
per year. Several of the smaller chert layers are separated by
121: 3796:
Grímsson, F.; Zetter, R.; Halbritter, H.; Grimm, G. W. (2014).
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Ph.D. Dissertation, University of Michigan, Ann Arbor, Michigan
4311:"Establishing a fossil record for the perianthless Piperales: 3106:
Life in Stone: A natural history of British Columbia's Fossils
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sp. nov.(Saururaceae) from the Middle Eocene Princeton Chert"
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trapping more heat. The reason for this sudden increase in CO
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The Princeton Chert is an interbedded sequence consisting of
4480:
Stockey, R. A.; Pigg, K. B. (1991). "Flowers and fruits of
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10.1130/0091-7613(1995)023<1044:ECCALT>2.3.CO;2
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due to the collision of tectonic plates. Also at the time,
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Little, S.A.; Stockey, R.A. (2003). "Vegetative growth of
3019: 3018:
Scotese, C. R. (2003) Paleomap Project. . Available from:
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The Princeton Chert fossils indicate that the area was an
144:, with certain taxa appearing and disappearing with time. 3625:
from the Middle Eocene of southern British Columbia".
3061: 3059: 3057: 3055: 2529:
Stockey, RA (2001). Briggs, DEG; Crowther, PR (eds.).
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from the Princeton chert, British Columbia, Canada".
4588: 4586: 4584: 2420:
from the Middle Eocene of southern British Columbia"
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The Princeton Chert was originally considered to be
4189:Stockey, R. A.; LePage, B. A.; Pigg, K. B. (1998). 3144: 3142: 3652: 3650: 3648: 2542: 2540: 2300: 2298: 2296: 3153:, Araceae): comparisons with extant Lasioideae". 2611:Palaeogeography, Palaeoclimatology, Palaeoecology 369:have tar spot fungi on their leaves described as 284:in tissues (air spaces to provide buoyancy), and 163:stage (47.8–56.0 mya), consistent with the whole 62:, 8.5 km (5.3 mi) south of the town of 54:and diversity. It is located in exposures of the 3621:Basinger, J. F. (1981). "The vegetative body of 2760: 2758: 2756: 401:these associations have been compared to extant 4395:(Vitaceae) and implications for phytogeography" 4354: 4352: 4350: 4241:Cevallos-Ferriz, S. R.; Stockey, R. A. (1990). 3227:Wilson, MVH (1982). "A new species of the fish 4556: 4554: 3717: 3715: 3370: 3368: 3099: 3097: 2894: 2892: 2533:. Oxford, Blackwell Science. pp. 359–362. 2524: 2522: 2520: 2518: 2516: 2514: 2512: 2510: 2508: 2409: 2407: 2405: 2373: 2371: 4747:Eocene paleontological sites of North America 4236: 4234: 4232: 4230: 3876:Cevallos-Ferriz, S. R. S. (1995). "Fruits of 3283: 3281: 3231:from the Middle Eocene of British Columbia". 3188:Phipps, CJ; Osborn, JM; Stockey, RA (1995). " 2899:Pearson, PN (2010). "Increased atmospheric CO 2799: 2797: 8: 4384: 4382: 2804:Zachos, JC; Dickens, GR; Zeebe, ZE (2008). 2449: 2447: 2445: 4144:Archibald, S. B.; Cannings, R. A. (2022). 1838: 893: 717: 518: 431: 4767:Regional District of Okanagan-Similkameen 4618: 4410: 4330: 4258: 4218: 4165: 3833: 3356: 3108:. Vancouver, UBC Press. pp. 234–247. 2987: 2829: 2265: 2255: 167:being now dated radiometrically as being 2531:The Princeton Chert In: Palaeobiology II 4022:International Journal of Plant Sciences 3728:International Journal of Plant Sciences 3510:International Journal of Plant Sciences 3463:International Journal of Plant Sciences 3424:International Journal of Plant Sciences 3385:International Journal of Plant Sciences 3194:International Journal of Plant Sciences 3155:International Journal of Plant Sciences 2342:International Journal of Plant Sciences 2165: 500:Bones preserved in the Princeton Chert 4519:Erwin, D. M.; Stockey, R. A. (1991). " 4463:Courier Forschungsinstitut Senckenberg 4391:"Seed morphology of modern and fossil 3657:Stockey, R. A. (1984). "Middle Eocene 2646:Canadian Petroleum Geologists Bulletin 2177:from the Eocene of British Columbia". 2132:Ectomycorrhizae fungi associated with 470:Not described to family/genus/species 84:lake sediments are found elsewhere in 4486:Review of Palaeobotany and Palynology 4309:Smith, S. Y.; Stockey, R. A. (2007). 4199:Review of Palaeobotany and Palynology 3806:Review of Palaeobotany and Palynology 3763:Review of Palaeobotany and Palynology 3545:Review of Palaeobotany and Palynology 3068:Review of Palaeobotany and Palynology 2055:Cryptodidymosphaerites princetonensis 1633:fruit of uncertain generic placement 389:have also been preserved in roots of 382:Cryptodidymosphaerites princetonensis 7: 4389:Chen, I.; Manchester, S. R. (2007). 1676:fruit of uncertain generic placement 1656:fruit of uncertain generic placement 1346:Not to be confused with the odonate 375:, which is in turn parasitized by a 211:, was beginning to move northwards. 4757:Natural history of British Columbia 3700:from Eocene of British Columbia". 3034:Canadian Journal of Earth Sciences 2768:Canadian Journal of Earth Sciences 2561:10.1002/j.1537-2197.1987.tb08790.x 2456:Canadian Journal of Earth Sciences 2236:Canadian Journal of Earth Sciences 2151:Not described to genus or species 96:in northern British Columbia, the 14: 4150:Cephalozygoptera, Dysagrionidae)" 1792:flower of uncertain affiliation. 849:First described for ovulate cones 4752:Stratigraphy of British Columbia 3661:remains from British Columbia". 3461:gen. et sp. nov.(Athyriaceae)". 3422:gen. et sp. nov.(Athyriaceae)". 2095:Monodictysporites princetonensis 90:Driftwood Canyon Provincial Park 3901:Plant Systematics and Evolution 1622:"Ampelocissus" similkameenensis 1251:Liriodendroxylon princetonensis 4575:10.1080/00275514.1998.12026955 3826:10.1016/j.revpalbo.2013.09.005 3375:Stockey, R.; Pigg, K. (1994). 1880:Palaeoserenomyces allenbyensis 1220:Initially described from seeds 409:was the fist documentation of 348:, plus a soft-shelled turtle. 1: 4702:Princeton Chert website (ASU) 4220:10.1016/S0034-6667(98)00038-4 3859:Palaeontographica Abteilung B 2958:and Temperature Variations". 2111:Dennstaedtiopsis aerenchymata 1825:genus of uncertain placement 1293:Paleomyrtinaea princetonensis 659:Dennstaedtiopsis aerenchymata 248:cease to be represented, yet 116:Location and geologic setting 4506:10.1016/0034-6667(91)90084-G 3783:10.1016/0034-6667(91)90083-F 3565:10.1016/0034-6667(91)90085-H 3088:10.1016/0034-6667(91)90085-H 2631:10.1016/0031-0182(80)90029-2 1503:"Princeton chert species 3" 1483:"Princeton chert species 2" 1463:"Princeton chert species 1" 1176:Briefly described by Little 851:A whole plant reconstruction 3459:Makotopteris princetonensis 2903:during the middle Eocene". 2685:10.1016/j.tecto.2007.10.007 2576:American Journal of Science 590:Makotopteris princetonensis 106:Klondike Mountain Formation 64:Princeton, British Columbia 4783: 4727:Paleogene British Columbia 4436:Canadian Journal of Botany 4399:American Journal of Botany 4361:Canadian Journal of Botany 4319:American Journal of Botany 4284:Canadian Journal of Botany 4191:"Permineralized fruits of 4084:Canadian Journal of Botany 4057:Canadian Journal of Botany 3987:Canadian Journal of Botany 3944:American Journal of Botany 3882:American Journal of Botany 3627:Canadian Journal of Botany 3290:American Journal of Botany 3121:Canadian Journal of Botany 2549:American Journal of Botany 2424:Canadian Journal of Botany 2384:Canadian Journal of Botany 2380:Paleorosa similkameenensis 2307:American Journal of Botany 1417:Paleorosa similkameenensis 704:Not identified to species 272:In situ lacustrine fossils 4260:10.1163/22941932-90001183 4154:The Canadian Entomologist 3921:10.1007/s00606-005-0358-9 3358:10.11646/zootaxa.3286.1.1 2035: 1950: 1685: 1640: 1603: 1514:Not described to species 1494:Not described to species 1474:Not described to species 1431: 1397: 1133:Pararisteapollis stockeyi 1013:Keratosperma allenbyensis 853:includes the synonymized 780: 775: 607: 538: 387:mycorrhizal relationships 313:) and rushes and sedges ( 4482:Princetonia allenbyensis 3506:Trawetsia princetonensis 3151:Keratosperma allenbyense 2596:10.2475/ajs.s5-29.169.54 1891:fungus on the host palm 1780:Princetonia allenbyensis 973:Aponogeton longispinosum 935:Heleophyton helobieoides 627:Trawetsia princetonensis 180:Eocene Thermal Maximum 2 58:on the east bank of the 31:is a fossil locality in 3420:Dickwhitea allenbyensis 3020:http://www.scotese.com/ 2980:10.1126/science.1193654 2925:10.1126/science.1197894 2017:Noted to be similar to 1977:Noted to be similar to 1932:Noted to be similar to 1718:of uncertain affinity. 942:An aquatic or emergent 558:Dickwhitea allenbyensis 468:A lepidopteran forewing 4762:Paleontology in Canada 4521:Soleredera rhizomorpha 4332:10.3732/ajb.94.10.1642 3377:"Vegetative growth of 2378:Basinger, JF (1976). " 2257:10.1139/cjes-2015-0177 2045:Cryptodidymosphaerites 2025:In situ decomposer of 2020:Thielaviopsis basicola 1985:In situ decomposer of 1940:In situ decomposer of 1814:Soleredera rhizomorpha 207:, which was joined to 112:, south of Princeton. 24: 4412:10.3732/ajb.94.9.1534 4018:Decodon verticillatus 2712:10.1139/cjb-2012-0313 2414:Basinger, JF (1984). 1980:Culcitalna achraspora 1424:A rose family flower 1180:(2009) but not named 39:, which comprises an 22: 4722:Eocene North America 4014:Decodon allenbyensis 1333:Allenbya collinsonae 1208:Decodon allenbyensis 869:Pinus princetonensis 299:), water plantains ( 110:Republic, Washington 4498:1991RPaPa..70..163S 4211:1998RPaPa.103..223S 4167:10.4039/tce.2022.16 3956:10.3732/ajb.0800318 3913:2005PSyEv.255..145H 3818:2014RPaPa.200..161G 3775:1991RPaPa..70..147E 3623:Metasequoia milleri 3592:2001Britt..53..173C 3557:1991RPaPa..70..173C 3080:1991RPaPa..70..173C 2972:2010Sci...330..819B 2917:2010Sci...330..763P 2867:1995Geo....23.1044G 2831:10.1038/nature06588 2822:2008Natur.451..279Z 2780:2005CaJES..42..167G 2739:2003Geo....31.1017B 2677:2009Tectp.464..164I 2623:1980PPP....32...21W 2588:1935AmJS...29...54R 2468:2005CaJES..42..187M 2418:Metasequoia milleri 2248:2016CaJES..53..548G 1935:Xylomyces giganteus 1787:A possibly aquatic 1443:Prunus allenbyensis 855:P. similkameenensis 758:Metasequoia milleri 668:dennstaedtioid fern 395:Metasequoia milleri 246:Metasequoia milleri 151:based on data from 43:preserved flora of 3769:((1-2)): 147–162. 3600:10.1007/BF02812700 2283:Washington Geology 2071:Uhlia allenbyensis 1894:Uhlia allenbyensis 1740:Ethela sargentiana 1543:Wehrwolfea striata 1144:pollen morphotype 1055:Uhlia allenbyensis 98:McAbee Fossil Beds 25: 4525:Botanical Gazette 4325:(10): 1642–1657. 4313:Saururus tuckerae 4111:Botanical Gazette 3663:Botanical Gazette 3633:(12): 2379–2410. 2966:(6005): 819–821. 2911:(6005): 763–764. 2861:(11): 1044–1048. 2816:(7176): 279–283. 2733:(11): 1017–1020. 2555:(12): 1878–1887. 2495:Geoscience Canada 2390:(20): 2293–2305. 2158: 2157: 2085:Monodictysporites 1870:Palaeoserenomyces 1832: 1831: 1585:Saururus tuckerae 1217:swamp loosestrife 887: 886: 711: 710: 701:osmundaceous fern 636:blechnacious fern 599:athyriaceous fern 567:athyriaceous fern 507: 506: 216:aquatic ecosystem 165:Allenby Formation 138:Allenby Formation 60:Similkameen River 56:Allenby Formation 52:species abundance 4774: 4685: 4684: 4647: 4641: 4640: 4622: 4595:Eorhiza arnoldii 4590: 4579: 4578: 4558: 4549: 4548: 4516: 4510: 4509: 4492:(1–2): 163–172. 4477: 4471: 4470: 4458: 4452: 4451: 4442:(7): 1373–1377. 4431: 4425: 4424: 4414: 4405:(9): 1534–1553. 4386: 4377: 4376: 4356: 4345: 4344: 4334: 4306: 4300: 4299: 4290:(9): 2025–2034. 4279: 4273: 4272: 4262: 4238: 4225: 4224: 4222: 4205:(3–4): 223–234. 4186: 4180: 4179: 4169: 4141: 4135: 4134: 4106: 4100: 4099: 4079: 4073: 4072: 4063:(6): 1327–1339. 4052: 4046: 4045: 4009: 4003: 4002: 3982: 3976: 3975: 3939: 3933: 3932: 3896: 3890: 3889: 3873: 3867: 3866: 3854: 3848: 3847: 3837: 3812:(100): 161–187. 3793: 3787: 3786: 3758: 3752: 3751: 3719: 3710: 3709: 3693: 3687: 3686: 3654: 3643: 3642: 3618: 3612: 3611: 3575: 3569: 3568: 3551:(1–2): 173–185. 3540: 3534: 3533: 3501: 3495: 3494: 3469:(5): 1047–1055. 3454: 3448: 3447: 3415: 3409: 3408: 3379:Eorhiza arnoldii 3372: 3363: 3362: 3360: 3336: 3330: 3329: 3285: 3276: 3275: 3247: 3241: 3240: 3224: 3218: 3217: 3185: 3179: 3178: 3146: 3137: 3136: 3127:(9): 2636–2645. 3116: 3110: 3109: 3101: 3092: 3091: 3074:(1–2): 173–185. 3063: 3050: 3049: 3029: 3023: 3016: 3010: 3009: 2991: 2951: 2945: 2944: 2896: 2887: 2886: 2850: 2844: 2843: 2833: 2801: 2792: 2791: 2762: 2751: 2750: 2747:10.1130/g19800.1 2722: 2716: 2715: 2695: 2689: 2688: 2671:(1–4): 164–185. 2660: 2654: 2653: 2641: 2635: 2634: 2606: 2600: 2599: 2571: 2565: 2564: 2544: 2535: 2534: 2526: 2503: 2502: 2486: 2480: 2479: 2451: 2440: 2439: 2411: 2400: 2399: 2375: 2366: 2365: 2337: 2331: 2330: 2313:(8): 1099–1113. 2302: 2291: 2290: 2278: 2272: 2271: 2269: 2259: 2227: 2221: 2220: 2212: 2206: 2205: 2193: 2187: 2186: 2170: 2027:Eorhiza arnoldii 1987:Eorhiza arnoldii 1942:Eorhiza arnoldii 1839: 1707:Eorhiza arnoldii 1555:soapberry family 1379:Diplopanax eydei 1241:Liriodendroxylon 1123:Pararisteapollis 894: 814:Pinus andersonii 718: 649:Dennstaedtiopsis 519: 432: 372:Paleoserenomyces 261:Dennstaedtiopsis 86:British Columbia 33:British Columbia 16:Fossilized Flora 4782: 4781: 4777: 4776: 4775: 4773: 4772: 4771: 4707: 4706: 4693: 4688: 4649: 4648: 4644: 4592: 4591: 4582: 4560: 4559: 4552: 4518: 4517: 4513: 4479: 4478: 4474: 4460: 4459: 4455: 4448:10.1139/b73-172 4433: 4432: 4428: 4388: 4387: 4380: 4373:10.1139/b90-039 4358: 4357: 4348: 4308: 4307: 4303: 4296:10.1139/b90-265 4281: 4280: 4276: 4240: 4239: 4228: 4188: 4187: 4183: 4143: 4142: 4138: 4108: 4107: 4103: 4096:10.1139/b93-001 4081: 4080: 4076: 4069:10.1139/b90-169 4054: 4053: 4049: 4011: 4010: 4006: 3999:10.1139/b88-050 3984: 3983: 3979: 3941: 3940: 3936: 3898: 3897: 3893: 3875: 3874: 3870: 3856: 3855: 3851: 3795: 3794: 3790: 3760: 3759: 3755: 3721: 3720: 3713: 3695: 3694: 3690: 3656: 3655: 3646: 3639:10.1139/b81-291 3620: 3619: 3615: 3577: 3576: 3572: 3542: 3541: 3537: 3503: 3502: 3498: 3456: 3455: 3451: 3417: 3416: 3412: 3374: 3373: 3366: 3338: 3337: 3333: 3302:10.2307/2446014 3287: 3286: 3279: 3264:10.2307/3761225 3249: 3248: 3244: 3226: 3225: 3221: 3187: 3186: 3182: 3148: 3147: 3140: 3133:10.1139/b89-340 3118: 3117: 3113: 3103: 3102: 3095: 3065: 3064: 3053: 3046:10.1139/e10-085 3031: 3030: 3026: 3017: 3013: 2957: 2953: 2952: 2948: 2902: 2898: 2897: 2890: 2852: 2851: 2847: 2803: 2802: 2795: 2788:10.1139/E04-100 2764: 2763: 2754: 2724: 2723: 2719: 2697: 2696: 2692: 2662: 2661: 2657: 2643: 2642: 2638: 2608: 2607: 2603: 2573: 2572: 2568: 2546: 2545: 2538: 2528: 2527: 2506: 2488: 2487: 2483: 2476:10.1139/E04-095 2453: 2452: 2443: 2436:10.1139/b84-045 2416:"Seed cones of 2413: 2412: 2403: 2396:10.1139/b76-246 2377: 2376: 2369: 2339: 2338: 2334: 2319:10.2307/2444092 2304: 2303: 2294: 2280: 2279: 2275: 2229: 2228: 2224: 2214: 2213: 2209: 2195: 2194: 2190: 2172: 2171: 2167: 2163: 2150: 2137: 2107: 2067: 2024: 2016: 1984: 1976: 1939: 1931: 1837: 1791: 1714:A semi-aquatic 1677: 1657: 1513: 1493: 1473: 1345: 1221: 1219: 1175: 1100: 1075:Grossulariaceae 955:Aponogetonaceae 892: 852: 850: 848: 792:Pinus allisonii 716: 703: 517: 512: 499: 469: 430: 411:ectomycorrhizae 354: 274: 242: 201:Tibetan plateau 190: 186: 118: 88:, including in 72: 50:age, with rich 29:Princeton Chert 17: 12: 11: 5: 4780: 4778: 4770: 4769: 4764: 4759: 4754: 4749: 4744: 4739: 4734: 4729: 4724: 4719: 4709: 4708: 4705: 4704: 4699: 4692: 4691:External links 4689: 4687: 4686: 4665:10.3852/15-022 4659:(5): 882–890. 4642: 4611:10.3852/12-272 4605:(3): 521–529. 4580: 4569:(4): 667–673. 4550: 4537:10.1086/337885 4531:(2): 231–247. 4511: 4472: 4453: 4426: 4378: 4367:(2): 288–295. 4346: 4301: 4274: 4253:(3): 261–280. 4226: 4181: 4136: 4123:10.1086/337765 4117:(2): 207–217. 4101: 4074: 4047: 4034:10.1086/367811 4028:(3): 453–469. 4004: 3993:(2): 303–312. 3977: 3950:(3): 637–651. 3934: 3907:(3): 145–176. 3891: 3868: 3849: 3788: 3753: 3740:10.1086/657649 3734:(2): 294–313. 3724:Pinus arnoldii 3711: 3688: 3675:10.1086/337455 3669:(2): 262–274. 3644: 3613: 3586:(2): 173–235. 3570: 3535: 3522:10.1086/501034 3516:(3): 711–719. 3496: 3475:10.1086/314191 3449: 3436:10.1086/501036 3430:(3): 721–727. 3410: 3397:10.1086/297199 3391:(5): 606–616. 3364: 3331: 3296:(3): 410–412. 3277: 3258:(4): 667–673. 3242: 3219: 3206:10.1086/297232 3200:(1): 117–124. 3180: 3167:10.1086/346164 3161:(2): 239–250. 3138: 3111: 3093: 3051: 3024: 3011: 2955: 2946: 2900: 2888: 2845: 2793: 2774:(2): 167–185. 2752: 2717: 2706:(8): 514–529. 2690: 2665:Tectonophysics 2655: 2636: 2601: 2582:(169): 54–55. 2566: 2536: 2504: 2481: 2462:(2): 187–204. 2441: 2430:(2): 281–289. 2401: 2367: 2354:10.1086/297221 2348:(6): 828–836. 2332: 2292: 2273: 2242:(6): 548–564. 2222: 2207: 2188: 2185:(10): 101–118. 2164: 2162: 2159: 2156: 2155: 2153: 2129: 2124: 2118: 2117: 2115: 2099: 2089: 2078: 2077: 2075: 2059: 2049: 2039: 2033: 2032: 2030: 2008: 2003: 1993: 1992: 1990: 1968: 1963: 1954: 1948: 1947: 1945: 1923: 1918: 1909: 1901: 1900: 1898: 1884: 1874: 1864: 1856: 1855: 1852: 1849: 1846: 1843: 1836: 1833: 1830: 1829: 1827: 1818: 1808: 1797: 1796: 1794: 1784: 1774: 1763: 1762: 1760: 1744: 1734: 1723: 1722: 1720: 1711: 1701: 1691: 1688:incertae sedis 1683: 1682: 1680: 1678:Not described 1669: 1663: 1662: 1660: 1658:Not described 1649: 1644: 1642:incertae sedis 1638: 1637: 1635: 1626: 1616: 1607: 1601: 1600: 1598: 1589: 1579: 1570: 1562: 1561: 1559: 1547: 1537: 1527: 1519: 1518: 1516: 1505: 1499: 1498: 1496: 1485: 1479: 1478: 1476: 1465: 1459: 1458: 1456: 1447: 1437: 1429: 1428: 1426: 1421: 1411: 1401: 1395: 1394: 1392: 1383: 1373: 1364: 1356: 1355: 1353: 1337: 1327: 1317: 1309: 1308: 1306: 1297: 1287: 1283:Paleomyrtinaea 1277: 1269: 1268: 1266: 1255: 1245: 1235: 1227: 1226: 1224: 1212: 1202: 1193: 1185: 1184: 1182: 1167: 1162: 1157: 1149: 1148: 1146: 1137: 1127: 1117: 1106: 1105: 1103: 1101:Not described 1092: 1087: 1078: 1070: 1069: 1067: 1064:Coryphoid palm 1059: 1050: 1040: 1032: 1031: 1029: 1017: 1007: 997: 989: 988: 986: 977: 967: 958: 950: 949: 947: 944:water-plantain 939: 929: 919: 911: 910: 907: 904: 901: 898: 891: 888: 885: 884: 882: 873: 862: 861: 859: 840: 836:Pinus arnoldii 829: 828: 826: 818: 807: 806: 804: 796: 786: 779: 773: 772: 770: 762: 752: 743: 735: 734: 731: 728: 725: 722: 715: 712: 709: 708: 706: 696: 691: 682: 674: 673: 671: 663: 653: 642: 641: 639: 631: 621: 611: 605: 604: 602: 594: 584: 573: 572: 570: 562: 552: 542: 536: 535: 532: 529: 526: 523: 516: 513: 511: 508: 505: 504: 502: 491: 486: 481: 475: 474: 472: 465: 460: 455: 449: 448: 445: 442: 439: 436: 429: 426: 353: 350: 273: 270: 241: 238: 188: 184: 117: 114: 71: 68: 15: 13: 10: 9: 6: 4: 3: 2: 4779: 4768: 4765: 4763: 4760: 4758: 4755: 4753: 4750: 4748: 4745: 4743: 4740: 4738: 4737:Eocene plants 4735: 4733: 4730: 4728: 4725: 4723: 4720: 4718: 4715: 4714: 4712: 4703: 4700: 4698: 4695: 4694: 4690: 4682: 4678: 4674: 4670: 4666: 4662: 4658: 4654: 4646: 4643: 4638: 4634: 4630: 4626: 4621: 4616: 4612: 4608: 4604: 4600: 4596: 4589: 4587: 4585: 4581: 4576: 4572: 4568: 4564: 4557: 4555: 4551: 4546: 4542: 4538: 4534: 4530: 4526: 4522: 4515: 4512: 4507: 4503: 4499: 4495: 4491: 4487: 4483: 4476: 4473: 4468: 4464: 4457: 4454: 4449: 4445: 4441: 4437: 4430: 4427: 4422: 4418: 4413: 4408: 4404: 4400: 4396: 4394: 4385: 4383: 4379: 4374: 4370: 4366: 4362: 4355: 4353: 4351: 4347: 4342: 4338: 4333: 4328: 4324: 4320: 4316: 4314: 4305: 4302: 4297: 4293: 4289: 4285: 4278: 4275: 4270: 4266: 4261: 4256: 4252: 4248: 4244: 4237: 4235: 4233: 4231: 4227: 4221: 4216: 4212: 4208: 4204: 4200: 4196: 4194: 4185: 4182: 4177: 4173: 4168: 4163: 4159: 4155: 4151: 4149: 4140: 4137: 4132: 4128: 4124: 4120: 4116: 4112: 4105: 4102: 4097: 4093: 4089: 4085: 4078: 4075: 4070: 4066: 4062: 4058: 4051: 4048: 4043: 4039: 4035: 4031: 4027: 4023: 4019: 4015: 4008: 4005: 4000: 3996: 3992: 3988: 3981: 3978: 3973: 3969: 3965: 3961: 3957: 3953: 3949: 3945: 3938: 3935: 3930: 3926: 3922: 3918: 3914: 3910: 3906: 3902: 3895: 3892: 3887: 3883: 3879: 3872: 3869: 3864: 3860: 3853: 3850: 3845: 3841: 3836: 3831: 3827: 3823: 3819: 3815: 3811: 3807: 3803: 3801: 3792: 3789: 3784: 3780: 3776: 3772: 3768: 3764: 3757: 3754: 3749: 3745: 3741: 3737: 3733: 3729: 3725: 3718: 3716: 3712: 3707: 3703: 3699: 3692: 3689: 3684: 3680: 3676: 3672: 3668: 3664: 3660: 3653: 3651: 3649: 3645: 3640: 3636: 3632: 3628: 3624: 3617: 3614: 3609: 3605: 3601: 3597: 3593: 3589: 3585: 3581: 3574: 3571: 3566: 3562: 3558: 3554: 3550: 3546: 3539: 3536: 3531: 3527: 3523: 3519: 3515: 3511: 3507: 3500: 3497: 3492: 3488: 3484: 3480: 3476: 3472: 3468: 3464: 3460: 3453: 3450: 3445: 3441: 3437: 3433: 3429: 3425: 3421: 3414: 3411: 3406: 3402: 3398: 3394: 3390: 3386: 3382: 3380: 3371: 3369: 3365: 3359: 3354: 3350: 3346: 3342: 3335: 3332: 3327: 3323: 3319: 3315: 3311: 3307: 3303: 3299: 3295: 3291: 3284: 3282: 3278: 3273: 3269: 3265: 3261: 3257: 3253: 3246: 3243: 3239:(2): 413–424. 3238: 3234: 3233:Palaeontology 3230: 3223: 3220: 3215: 3211: 3207: 3203: 3199: 3195: 3191: 3184: 3181: 3176: 3172: 3168: 3164: 3160: 3156: 3152: 3145: 3143: 3139: 3134: 3130: 3126: 3122: 3115: 3112: 3107: 3100: 3098: 3094: 3089: 3085: 3081: 3077: 3073: 3069: 3062: 3060: 3058: 3056: 3052: 3047: 3043: 3039: 3035: 3028: 3025: 3021: 3015: 3012: 3007: 3003: 2999: 2995: 2990: 2985: 2981: 2977: 2973: 2969: 2965: 2961: 2950: 2947: 2942: 2938: 2934: 2930: 2926: 2922: 2918: 2914: 2910: 2906: 2895: 2893: 2889: 2884: 2880: 2876: 2872: 2868: 2864: 2860: 2856: 2849: 2846: 2841: 2837: 2832: 2827: 2823: 2819: 2815: 2811: 2807: 2800: 2798: 2794: 2789: 2785: 2781: 2777: 2773: 2769: 2761: 2759: 2757: 2753: 2748: 2744: 2740: 2736: 2732: 2728: 2721: 2718: 2713: 2709: 2705: 2701: 2694: 2691: 2686: 2682: 2678: 2674: 2670: 2666: 2659: 2656: 2651: 2647: 2640: 2637: 2632: 2628: 2624: 2620: 2616: 2612: 2605: 2602: 2597: 2593: 2589: 2585: 2581: 2577: 2570: 2567: 2562: 2558: 2554: 2550: 2543: 2541: 2537: 2532: 2525: 2523: 2521: 2519: 2517: 2515: 2513: 2511: 2509: 2505: 2501:(4): 155–164. 2500: 2496: 2492: 2485: 2482: 2477: 2473: 2469: 2465: 2461: 2457: 2450: 2448: 2446: 2442: 2437: 2433: 2429: 2425: 2421: 2419: 2410: 2408: 2406: 2402: 2397: 2393: 2389: 2385: 2381: 2374: 2372: 2368: 2363: 2359: 2355: 2351: 2347: 2343: 2336: 2333: 2328: 2324: 2320: 2316: 2312: 2308: 2301: 2299: 2297: 2293: 2288: 2284: 2277: 2274: 2268: 2263: 2258: 2253: 2249: 2245: 2241: 2237: 2233: 2226: 2223: 2218: 2211: 2208: 2203: 2199: 2192: 2189: 2184: 2180: 2176: 2169: 2166: 2160: 2154: 2152: 2149: 2148: 2143: 2142: 2135: 2130: 2128: 2125: 2123: 2120: 2119: 2116: 2114: 2113: 2112: 2105: 2100: 2098: 2097: 2096: 2090: 2088: 2087: 2086: 2080: 2079: 2076: 2074: 2073: 2072: 2065: 2060: 2058: 2057: 2056: 2050: 2048: 2047: 2046: 2040: 2038: 2034: 2031: 2029: 2028: 2022: 2021: 2014: 2013:microascalean 2009: 2007: 2004: 2002: 2001: 2000: 1999:Thielaviopsis 1995: 1994: 1991: 1989: 1988: 1982: 1981: 1974: 1973:microascalean 1969: 1967: 1964: 1962: 1961: 1960: 1955: 1953: 1949: 1946: 1944: 1943: 1937: 1936: 1929: 1924: 1922: 1919: 1917: 1916: 1915: 1910: 1908: 1907: 1903: 1902: 1899: 1897: 1896: 1895: 1890: 1885: 1883: 1882: 1881: 1875: 1873: 1872: 1871: 1865: 1863: 1862: 1858: 1857: 1853: 1850: 1847: 1844: 1841: 1840: 1834: 1828: 1826: 1824: 1819: 1817: 1816: 1815: 1809: 1807: 1806: 1805: 1799: 1798: 1795: 1793: 1790: 1785: 1783: 1782: 1781: 1775: 1773: 1772: 1771: 1765: 1764: 1761: 1759: 1757: 1754: 1750: 1745: 1743: 1742: 1741: 1735: 1733: 1732: 1731: 1725: 1724: 1721: 1719: 1717: 1712: 1710: 1709: 1708: 1702: 1700: 1699: 1698: 1692: 1690: 1689: 1684: 1681: 1679: 1675: 1670: 1668: 1665: 1664: 1661: 1659: 1655: 1650: 1648: 1645: 1643: 1639: 1636: 1634: 1632: 1627: 1625: 1624: 1623: 1617: 1615: 1614: 1613: 1608: 1606: 1602: 1599: 1597: 1595: 1594:lizard's-tail 1590: 1588: 1587: 1586: 1580: 1578: 1577: 1576: 1571: 1569: 1568: 1564: 1563: 1560: 1558: 1556: 1553: 1548: 1546: 1545: 1544: 1538: 1536: 1535: 1534: 1528: 1526: 1525: 1521: 1520: 1517: 1515: 1511: 1506: 1504: 1501: 1500: 1497: 1495: 1491: 1486: 1484: 1481: 1480: 1477: 1475: 1471: 1466: 1464: 1461: 1460: 1457: 1455: 1453: 1448: 1446: 1445: 1444: 1438: 1436: 1435: 1430: 1427: 1425: 1422: 1420: 1419: 1418: 1412: 1410: 1409: 1408: 1402: 1400: 1396: 1393: 1391: 1389: 1384: 1382: 1381: 1380: 1374: 1372: 1371: 1370: 1365: 1363: 1362: 1358: 1357: 1354: 1352: 1351: 1350: 1343: 1338: 1336: 1335: 1334: 1328: 1326: 1325: 1324: 1318: 1316: 1315: 1311: 1310: 1307: 1305: 1303: 1298: 1296: 1295: 1294: 1288: 1286: 1285: 1284: 1278: 1276: 1275: 1271: 1270: 1267: 1265: 1263: 1262: 1256: 1254: 1253: 1252: 1246: 1244: 1243: 1242: 1236: 1234: 1233: 1229: 1228: 1225: 1223: 1218: 1213: 1211: 1210: 1209: 1203: 1201: 1200: 1199: 1194: 1192: 1191: 1187: 1186: 1183: 1181: 1179: 1173: 1168: 1166: 1163: 1161: 1158: 1156: 1155: 1151: 1150: 1147: 1145: 1143: 1138: 1136: 1135: 1134: 1128: 1126: 1125: 1124: 1118: 1116: 1115: 1112: 1108: 1107: 1104: 1102: 1098: 1093: 1091: 1088: 1086: 1085: 1084: 1079: 1077: 1076: 1072: 1071: 1068: 1066: 1065: 1060: 1058: 1057: 1056: 1051: 1049: 1048: 1047: 1041: 1039: 1038: 1034: 1033: 1030: 1028: 1026: 1023: 1018: 1016: 1015: 1014: 1008: 1006: 1005: 1004: 998: 996: 995: 991: 990: 987: 985: 983: 982:Cape-pondweed 978: 976: 975: 974: 968: 966: 965: 964: 959: 957: 956: 952: 951: 948: 946: 945: 940: 938: 937: 936: 930: 928: 927: 926: 920: 918: 917: 913: 912: 908: 905: 902: 899: 896: 895: 889: 883: 881: 879: 874: 872: 871: 870: 864: 863: 860: 858: 856: 846: 841: 839: 838: 837: 831: 830: 827: 825: 824: 819: 817: 816: 815: 809: 808: 805: 803: 802: 797: 795: 794: 793: 787: 785: 784: 778: 774: 771: 769: 768: 763: 761: 760: 759: 753: 751: 750: 749: 744: 742: 741: 737: 736: 732: 729: 726: 723: 720: 719: 713: 707: 705: 702: 697: 695: 692: 690: 689: 688: 683: 681: 680: 676: 675: 672: 670: 669: 664: 662: 661: 660: 654: 652: 651: 650: 644: 643: 640: 638: 637: 632: 630: 629: 628: 622: 620: 619: 618: 612: 610: 606: 603: 601: 600: 595: 593: 592: 591: 585: 583: 582: 581: 575: 574: 571: 569: 568: 563: 561: 560: 559: 553: 551: 550: 549: 543: 541: 537: 533: 530: 527: 524: 521: 520: 515:Pteridophytes 514: 509: 503: 501: 497: 492: 490: 487: 485: 482: 480: 477: 476: 473: 471: 466: 464: 461: 459: 456: 454: 451: 450: 446: 443: 440: 437: 434: 433: 427: 425: 424: 423: 418: 417: 412: 408: 404: 400: 396: 392: 388: 384: 383: 378: 374: 373: 368: 365: 364: 359: 351: 349: 347: 346: 341: 340: 335: 334: 328: 326: 322: 318: 317: 312: 308: 307: 302: 298: 294: 293: 287: 283: 279: 271: 269: 267: 263: 262: 257: 253: 252: 247: 239: 237: 234: 230: 225: 221: 218:, growing in 217: 212: 210: 206: 202: 198: 194: 181: 177: 172: 170: 166: 162: 158: 154: 150: 149:Middle Eocene 145: 143: 139: 135: 131: 127: 123: 115: 113: 111: 107: 103: 99: 95: 91: 87: 83: 78: 69: 67: 65: 61: 57: 53: 49: 46: 42: 38: 34: 30: 21: 4742:Lagerstätten 4656: 4652: 4645: 4602: 4598: 4594: 4566: 4562: 4528: 4524: 4520: 4514: 4489: 4485: 4481: 4475: 4466: 4462: 4456: 4439: 4435: 4429: 4402: 4398: 4393:Ampelocissus 4392: 4364: 4360: 4322: 4318: 4312: 4304: 4287: 4283: 4277: 4250: 4247:IAWA Journal 4246: 4202: 4198: 4192: 4184: 4157: 4153: 4147: 4139: 4114: 4110: 4104: 4087: 4083: 4077: 4060: 4056: 4050: 4025: 4021: 4017: 4013: 4007: 3990: 3986: 3980: 3947: 3943: 3937: 3904: 3900: 3894: 3885: 3881: 3877: 3871: 3862: 3858: 3852: 3809: 3805: 3799: 3791: 3766: 3762: 3756: 3731: 3727: 3723: 3705: 3701: 3697: 3691: 3666: 3662: 3658: 3630: 3626: 3622: 3616: 3583: 3579: 3573: 3548: 3544: 3538: 3513: 3509: 3505: 3499: 3466: 3462: 3458: 3452: 3427: 3423: 3419: 3413: 3388: 3384: 3378: 3348: 3344: 3334: 3293: 3289: 3255: 3251: 3245: 3236: 3232: 3228: 3222: 3197: 3193: 3189: 3183: 3158: 3154: 3150: 3124: 3120: 3114: 3105: 3071: 3067: 3040:(1): 25–43. 3037: 3033: 3027: 3014: 2963: 2959: 2949: 2908: 2904: 2858: 2854: 2848: 2813: 2809: 2771: 2767: 2730: 2726: 2720: 2703: 2699: 2693: 2668: 2664: 2658: 2649: 2645: 2639: 2614: 2610: 2604: 2579: 2575: 2569: 2552: 2548: 2530: 2498: 2494: 2484: 2459: 2455: 2427: 2423: 2417: 2387: 2383: 2379: 2345: 2341: 2335: 2310: 2306: 2286: 2282: 2276: 2239: 2235: 2225: 2216: 2210: 2201: 2197: 2191: 2182: 2178: 2174: 2168: 2145: 2139: 2133: 2131: 2127:Undescribed 2126: 2122:Undescribed 2121: 2109: 2101: 2093: 2091: 2083: 2081: 2069: 2061: 2053: 2051: 2043: 2041: 2037:Pleosporales 2026: 2018: 2010: 2006:undescribed 2005: 1997: 1996: 1986: 1978: 1970: 1966:undescribed 1965: 1957: 1956: 1952:Microascales 1941: 1933: 1925: 1921:undescribed 1920: 1912: 1911: 1904: 1892: 1886: 1878: 1876: 1868: 1866: 1859: 1820: 1812: 1810: 1802: 1800: 1789:magnoliopsid 1786: 1778: 1776: 1768: 1766: 1746: 1738: 1736: 1728: 1726: 1713: 1705: 1703: 1695: 1693: 1686: 1674:grape family 1671: 1666: 1654:grape family 1651: 1646: 1641: 1631:grape family 1628: 1620: 1618: 1612:Ampelocissus 1610: 1609: 1591: 1583: 1581: 1573: 1572: 1565: 1549: 1541: 1539: 1531: 1529: 1522: 1507: 1502: 1487: 1482: 1467: 1462: 1449: 1441: 1439: 1432: 1423: 1415: 1413: 1405: 1403: 1385: 1377: 1375: 1367: 1366: 1359: 1347: 1339: 1331: 1329: 1321: 1319: 1314:Nymphaeaceae 1312: 1299: 1291: 1289: 1281: 1279: 1272: 1264:-like wood. 1261:Liriodendron 1259: 1257: 1249: 1247: 1239: 1237: 1232:Magnoliaceae 1230: 1214: 1206: 1204: 1196: 1195: 1188: 1177: 1169: 1165:Undescribed 1164: 1160:Undescribed 1159: 1152: 1139: 1131: 1129: 1121: 1119: 1109: 1094: 1090:Undescribed 1089: 1081: 1080: 1073: 1061: 1053: 1052: 1044: 1042: 1035: 1019: 1011: 1009: 1003:Keratosperma 1001: 999: 992: 979: 971: 969: 961: 960: 953: 941: 933: 931: 923: 921: 916:Alismataceae 914: 875: 867: 865: 854: 842: 834: 832: 821:A 3-needled 820: 812: 810: 799:A 2-needled 798: 790: 788: 781: 767:dawn redwood 764: 756: 754: 746: 745: 740:Cupressaceae 738: 698: 694:Undescribed 693: 685: 684: 677: 665: 657: 655: 647: 645: 633: 625: 623: 615: 613: 596: 588: 586: 580:Makotopteris 578: 576: 564: 556: 554: 546: 544: 493: 489:undescribed 488: 484:Undescribed 483: 479:Undescribed 478: 467: 463:Undescribed 462: 458:Undescribed 457: 453:Undescribed 452: 420: 414: 406: 398: 394: 390: 385:. Symbiotic 380: 377:mycoparasite 370: 361: 355: 343: 337: 331: 329: 314: 306:Keratosperma 304: 301:Alismataceae 297:Nymphaeaceae 290: 275: 259: 249: 245: 243: 229:volcanic ash 213: 173: 169:Early Eocene 146: 130:volcanic ash 119: 77:Lagerstätten 73: 41:anatomically 28: 26: 4732:Eocene fish 2989:1874/385803 2204:(4): 37–45. 2138:similar to 2104:ascomycotan 2064:ascomycetan 1928:jahnulalean 1889:ascomycetan 1861:Dothideales 1770:Princetonia 1749:cyperaceous 1567:Saururaceae 1552:dodonaecous 1550:A possible 1524:Sapindaceae 1140:A possible 1027:seed genus 1025:arum family 925:Heleophyton 890:Angiosperms 748:Metasequoia 679:Osmundaceae 609:Blechnaceae 540:Athyriaceae 403:mycorrhizae 399:Metasequoia 356:Pathogenic 240:Known biota 224:subtropical 193:metamorphic 157:radiometric 4711:Categories 4620:1808/14620 4469:: 309–327. 4193:Diplopanax 4160:(1): e29. 4090:(1): 1–9. 3800:Aponogeton 3708:: 101–118. 2652:: 138–149. 2267:1807/71961 2161:References 2141:Rhizopogon 2108:hosted on 2068:hosted on 1959:Culcitalna 1906:Jahnulales 1804:Soleredera 1753:juncaceous 1533:Wehrwolfea 1390:relative. 1369:Diplopanax 1302:Myrtaceous 1190:Lythraceae 1172:lauraceous 1142:iridaceous 963:Aponogeton 548:Dickwhitea 510:Paleoflora 428:Paleofauna 416:Rhizopogon 345:Libotonius 325:Cyperaceae 303:), arums ( 286:protoxylem 282:aerenchyma 278:lacustrine 258:, such as 209:Antarctica 4653:Mycologia 4599:Mycologia 4563:Mycologia 4176:250035713 3726:Miller". 3580:Brittonia 3351:(1): 59. 3252:Mycologia 3006:206528256 2883:129182092 2617:: 21–44. 1914:Xylomyces 1823:lilialean 1667:"Type 2" 1647:"Type 1" 1407:Paleorosa 1361:Nyssaceae 1344:relative. 1342:waterlily 1274:Myrtaceae 1154:Lauraceae 1114:Iridaceae 1037:Arecaceae 878:pinaceous 617:Trawetsia 321:Juncaceae 205:Australia 197:Himalayas 4673:27302048 4629:23233506 4545:85180086 4421:21636520 4341:21636361 4269:85023353 4131:86651676 4042:83630351 3972:38272445 3964:21628220 3865:: 19–40. 3844:24926107 3748:84137991 3683:85063424 3608:19984401 3530:85160532 3491:33465214 3483:10506480 3444:85348245 3405:85094707 3326:29913925 3318:21708594 3214:84598167 3175:84905098 2998:21051636 2941:20253252 2933:21051620 2840:18202643 2362:85107282 2289:: 32–36. 1848:species 1758:monocot 1605:Vitaceae 1596:species 1575:Saururus 1399:Rosaceae 1349:Allenbya 1323:Allenbya 903:Species 843:A basal 777:Pinaceae 727:Species 714:Conifers 528:species 441:species 292:Allenbya 266:conifers 220:tropical 199:and the 161:Ypresian 102:Kamloops 100:west of 94:Smithers 4681:7871220 4637:3450242 4494:Bibcode 4207:Bibcode 3929:1964359 3909:Bibcode 3835:4047627 3814:Bibcode 3771:Bibcode 3588:Bibcode 3553:Bibcode 3345:Zootaxa 3310:2446014 3272:3761225 3076:Bibcode 2968:Bibcode 2960:Science 2913:Bibcode 2905:Science 2863:Bibcode 2855:Geology 2818:Bibcode 2776:Bibcode 2735:Bibcode 2727:Geology 2673:Bibcode 2619:Bibcode 2584:Bibcode 2464:Bibcode 2327:2444092 2244:Bibcode 2147:Suillus 1854:Images 1756:poalean 1697:Eorhiza 1557:flower 1510:prunoid 1490:prunoid 1470:prunoid 1452:prunoid 1198:Decodon 1097:current 1022:lasioid 994:Araceae 984:pollen 909:Images 897:Family 733:Images 721:Family 687:Osmunda 534:Images 522:Family 447:Images 435:Family 422:Suillus 311:Araceae 233:geysers 176:climate 153:mammals 142:outcrop 136:in the 108:around 70:History 4679:  4671:  4635:  4627:  4543:  4419:  4339:  4267:  4174:  4129:  4040:  3970:  3962:  3927:  3842:  3832:  3746:  3681:  3606:  3528:  3489:  3481:  3442:  3403:  3324:  3316:  3308:  3270:  3212:  3173:  3004:  2996:  2939:  2931:  2881:  2838:  2810:Nature 2700:Botany 2360:  2325:  2106:fungus 2066:fungus 2015:fungi. 1975:fungi. 1930:fungi. 1851:Notes 1845:Genus 1842:Order 1730:Ethela 1454:wood. 1434:Prunus 1304:fruit 1174:fruit. 906:Notes 900:Genus 730:Notes 724:Genus 531:Notes 525:Genus 496:turtle 444:Notes 438:Genus 339:Amyzon 316:Ethela 132:, and 82:Eocene 45:Eocene 37:Canada 4717:Chert 4677:S2CID 4633:S2CID 4541:S2CID 4265:S2CID 4172:S2CID 4127:S2CID 4038:S2CID 3968:S2CID 3925:S2CID 3878:Ribes 3744:S2CID 3698:Pinus 3679:S2CID 3659:Pinus 3604:S2CID 3526:S2CID 3487:S2CID 3440:S2CID 3401:S2CID 3322:S2CID 3306:JSTOR 3268:JSTOR 3210:S2CID 3190:Pinus 3171:S2CID 3002:S2CID 2937:S2CID 2879:S2CID 2358:S2CID 2323:JSTOR 2175:Pinus 2136:roots 2134:Pinus 1835:Fungi 1716:dicot 1512:seed. 1492:seed. 1472:seed. 1388:tuplo 1178:et al 1099:fruit 1083:Ribes 1046:Uhlia 880:cone 783:Pinus 407:Pinus 397:. 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Index


British Columbia
Canada
anatomically
Eocene
Epoch
species abundance
Allenby Formation
Similkameen River
Princeton, British Columbia
Lagerstätten
Eocene
British Columbia
Driftwood Canyon Provincial Park
Smithers
McAbee Fossil Beds
Kamloops
Klondike Mountain Formation
Republic, Washington
coal
shale
volcanic ash
chert
Allenby Formation
outcrop
Middle Eocene
mammals
radiometric
Ypresian
Allenby Formation

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