APPENDIX TABLE 1. Extended information from each site, their location, age and some additional data and the principal references. Also are shown the sample name of this work to facilitate the acronym navigation in the paper.
Site Name | Location | Age | Lithology/Facies/Formations | Description | Samples | References |
Pedrera de Meià & Co. | Montsec de Meià, Spain | Upper Hauterivian - Barremian | Laminated and massive lithographic limestones. | 19th century lithographic quarry. Limestones result of fresh-water coastal lakes system sedimentation of small extension. | R, R-drk, R-wht, C | Barale et al., 1984; Gil-Delgado et al., 2023; Martínez-Delclòs et al., 1991; Martín-Closas & López-Morón, 1995. |
Alcover | Tarragona, Spain | Triassic | Dolomicrites and dolomites from the Upper Muschelkalk. | Thin-bedded and laminated dolostones result of the infill of inter-reef depresions in anoxic conditions. | Mnt-Alc | Calvet & Tucker, 1995. |
Rubielos de Mora | Rubielos de Mora, Spain | Miocene - Early Pliocene | Laminated and massive mudstones of delta and lake facies. | Marls and mudstones of transitional facies that forms a tertiary basin of variably 400 m thick. | RMr | Anadón, 1983; Anadón et al. 1988; Moissenet and Gautienr, 1971. |
Las Hoyas | Cuenca, Spain | Barremian | Finely-laminated limestones of La Huérguina Formation. | Limestones formed in a ponds of microbial mats bottom. Is a freshwater carbonate environment influenced by season regulation. | LH1, LH2 | Bailleul et al., 2011; Barrios-de Pedro et al., 2018; Briggs et al., 1997; Fregenal and Melendez, 1992; Fregenal-Martínez and Meléndez 2016; Galobart et al., 2022; Gupta et al., 2008; Poyato-Ariza and Buscalioni, 2016. |
Cerin | Cerin, France | Late Kimmerigian | Lithographic limestones. | Result of lagoon system in-filled with the accion of supra-, intertidal, phreatic features and microbial processes. | Crn | Bernier et al., 1994. |
Canjuers | Haute Provence (Les Bessons), France | Tithonian | Fine-layered lithographic limestones from lagoon facies. | The fossils are situated in the basal layers of these paleolagoon and corresponds to the first phase of sedimentation. | MCFO-0352 | Peyer et al., 2014. |
Les Plâtrières | Aix-en-Provence, France | Oligocene | Limestones, marls and gypsum from Aix-en-Provence formation. | 18th century quarry of laminated rocks, result of a lacustrine/lagoon environment of brackish waters with punctual sea connections. | Aix-P1, Aix-P2, Aix-P3 | Gaudant et al., 2017. |
Ockley (Smokejacks Brickworks) | Surrey, England | Early Barremian | Sideritic siltstone and mudstone lenses below sandstone-bed of the Upper Weald Clay. | Industrial exploitation in a changing sequence from a lacustrine/lagoonal to fluvial/mudplain environment (B. walken site from). | Ock | Ross & Cook, 1995. |
Solnhofen | Solnhofen-Eichstätt, Germany | Early Tithonian | Lithographic limestones rhythmically laminated, alternation of pure limestone (Flinze) and shaly calcareous marls (Fäulen). | The Bavarian sites pertains to the Solnhofen Plattenkalk, which occupies an area of more than 2000 km2 and records 500.000 years . | MCFO-0435, MCFO-0723b, MCFO-0528, MCFO-0530, MCFO-0526, MGB P R-10378, MGB P R-10347, Slnhf-1 and Slnhf-2 | Keupp et al. 2007. |
Kelheim | Kelheim, Germany | Tithonian | Alternation of Flinze (97-99% CaCO3) and Fäulen (80-90% CaCO3). | The formation of Solnhofen Plattenkalk starts at east of the Solnhofen town and prograde to west during Early Tithonian. Is the reason because there are very similar fossil sites in the zone, as Kelheim, at 150 kilometers at east. | MCFO-0436 | Keupp et al. 2007. |
Hakel | east of Jbail, Lebanoon | Late Cenomanian | Lithographic limestones. | Sites are interpreted as small basins of shallow waters like intra-shelf depressed zones. There appears carbonates of shallow-waters between laminated mudstones as a result of sea-level oscillations. | MCFO-0521, MCFO-0523 | Ejel and Dubertret, 1966; Ferry et al., 2007; Forey et al., 2003. |
Hadjoula | east of Jbail, Lebanoon | Late Cenomanian | Lithographic limestones. | " | MCFO-0372, MCFO-0527, MCFO-0522, MCFO-0524 and MCFO-0525 | Ejel and Dubertret, 1966; Ferry et al., 2007; Forey et al., 2003. |
Sahel Alma | south of Jbail, Lebanoon | Late Santonian | Fine-grained, chalky limestones that broke in slabs. | Fossil site deposits are from deeper Santonian waters. | MCFO-0520 | Jattiot et al., 2015; Meister, 1993. |
Karatau | Big Karatau Range, Kazakhstan | Callovian - Kimmeridgian / Oxfordian - Kimmeridgian | Lithographic shales in Karabatau Formation. | The fossil site is composed by very laminated fissile claystone of lacustrine deposits that can preserve soft parts of taxa. | Kr | Doludenko and Orlovskaya, 1976; Doludenko et al., 1990; Liu et al., 2015. |
Daohugou | Daohugou, China | Callovian - Oxfordian | Grey tuff, tuffaceous siltstone and mudstone situated in Daohugou Beds of Langi Formation. | The fossils are preserved in the mudstones among fresh water environment indicators. Is the most important Lagerstäte of insects from Mesozoic. | Dhg | Liu et al., 2015; Ponomarenko and Ren, 2010; Rasnitsyn and Zhang, 2004; Wang et al., 2013. |
Green River | Wyoming, USA | Early Eocene - Middle Eocene | Laminated calcite limestone, limestones, marlstones and iron-stained mudstones principally . | Lake system with different basins and all their facies. In general terms, in Wyoming there are two paleolakes represented, the Fossil Lake and Lake Gosiute. | MCFO-0143, MCFO-0395 | Grande, 1984; Lundberg and Case, 1970; Rosen and Patterson, 1969. |
Crato | Crato, Brazil | Aptian | Laminated limestones of microbial mats in Crato Formation of lacustrine facies. | Site generated by the carbonate deposition in a hypersaline lacustrine system emplaced on the basin associated with the Gondwana rifting, considered a wetland with seasonal changes. | Crt-Brsl | Arai and Assine, 2020; Brito Neves et al., 2000; Dias and Carvalho, 2022; Ribeiro et al., 2021; Varejao et al., 2021. |
APPENDIX TABLE 2. Intensity of the main XRF peaks detected for all the samples investigated in this work. The intensities were extracted by fitting the spectra as described in (Ibáñez-Insa, 2017). All intensity values are normalized to that of the Compton peak observed for each spectra.
SAMPLE | ID | Si | P | S | K | Ca | Ti | Cr | Fe | Cu | Zn | Pb | Rb | Sr | Zr |
MCFO-0143 | Green River | 0.0040 | 0.0398 | 0.0134 | 0.0098 | 3.6275 | 0.0023 | 0.0012 | 0.0521 | 0.0057 | 0.0064 | 0.0107 | 0.0000 | 0.7690 | 0.0322 |
MCFO-0143 | Green River F | 0.0017 | 0.0435 | 0.0094 | 0.0091 | 2.4378 | 0.0561 | 0.0010 | 0.2545 | 0.0107 | 0.0140 | 0.0090 | 0.0000 | 1.5172 | 0.0115 |
MCFO-0435 | Solnhofen | 0.0035 | 0.0439 | 0.0154 | 0.0376 | 4.0263 | 0.0068 | 0.0020 | 0.1745 | 0.0047 | 0.0091 | 0.0085 | 0.0000 | 0.1193 | 0.0070 |
MCFO-0436 | Kelheim | 0.0015 | 0.0309 | 0.0073 | 0.0467 | 2.4534 | 0.0144 | 0.0016 | 0.8939 | 0.0045 | 0.0068 | 0.0065 | 0.0143 | 0.2154 | 0.0107 |
MCFO-0436 | Kelheim | 0.0019 | 0.0269 | 0.0059 | 0.0484 | 2.3883 | 0.0147 | 0.0014 | 0.8573 | 0.0041 | 0.0084 | 0.0037 | 0.0084 | 0.2090 | 0.0126 |
MCFO-0723b | Solnhofen | 0.0020 | 0.0444 | 0.0059 | 0.0262 | 4.1467 | 0.0029 | 0.0017 | 0.1269 | 0.0051 | 0.0056 | 0.0034 | 0.0000 | 0.0827 | 0.0069 |
MCFO-0527 | Hjoula | 0.0122 | 0.0088 | 0.0048 | 0.0054 | 0.1822 | 0.0037 | 0.0006 | 0.0818 | 0.0031 | 0.0048 | 0.0019 | 0.0000 | 0.0394 | 0.0090 |
MCFO-0527 | Hjoula | 0.0003 | 0.0357 | 0.0082 | 0.0310 | 3.4217 | 0.0046 | 0.0006 | 0.0903 | 0.0050 | 0.0071 | 0.0019 | 0.0000 | 0.2205 | 0.0042 |
MCFO-0521 | Haqel | 0.0022 | 0.0335 | 0.0080 | 0.0433 | 2.6311 | 0.0115 | 0.0011 | 0.2634 | 0.0046 | 0.0068 | 0.0077 | 0.0000 | 0.4253 | 0.0113 |
MCFO-0528 | Solnhofen | 0.0000 | 0.0450 | 0.0107 | 0.0277 | 3.8885 | 0.0036 | 0.0013 | 0.2137 | 0.0060 | 0.0040 | 0.0053 | 0.0000 | 0.1326 | 0.0078 |
MCFO-0527 | Hjoula | 0.0013 | 0.0356 | 0.0092 | 0.0347 | 3.4503 | 0.2378 | 0.0005 | 0.1564 | 0.0062 | 0.0071 | 0.0038 | 0.0000 | 0.2452 | 0.0152 |
MCFO-0530 | Solnhofen | 0.0022 | 0.0451 | 0.0118 | 0.0268 | 3.8685 | 0.0067 | 0.0010 | 0.1968 | 0.0056 | 0.0040 | 0.0035 | 0.0000 | 0.1306 | 0.0104 |
MCFO-0522 | Hjoula | 0.0014 | 0.0360 | 0.0129 | 0.0355 | 3.1842 | 0.0067 | 0.0006 | 0.2252 | 0.0052 | 0.0052 | 0.0033 | 0.0000 | 0.3644 | 0.0159 |
MCFO-0352 | Haute-Provence | 0.0018 | 0.0164 | 0.0069 | 0.0309 | 1.4130 | 0.0130 | 0.0011 | 0.6059 | 0.0083 | 0.0086 | 0.0046 | 0.0031 | 0.5530 | 0.0027 |
MCFO-0395 | Green River | 0.0024 | 0.0352 | 0.0115 | 0.0296 | 3.6251 | 0.0019 | 0.0014 | 0.0520 | 0.0085 | 0.0054 | 0.0067 | 0.0000 | 0.6383 | 0.0085 |
MCFO-0520 | Sahel Alma | 0.0017 | 0.0340 | 0.0062 | 0.0423 | 2.7029 | 0.0081 | 0.0019 | 0.2853 | 0.0062 | 0.0104 | 0.0089 | 0.0000 | 0.4291 | 0.0145 |
MCFO-0524 | Hjoula | 0.0033 | 0.0341 | 0.0080 | 0.0304 | 3.1934 | 0.0050 | 0.0009 | 0.1357 | 0.0048 | 0.0081 | 0.0081 | 0.0000 | 0.4126 | 0.0192 |
MCFO-0525 | Hjoula | 0.0036 | 0.0314 | 0.0084 | 0.0354 | 2.8704 | 0.0081 | 0.0011 | 0.2655 | 0.0056 | 0.0104 | 0.0071 | 0.0000 | 0.3288 | 0.0096 |
MCFO-0523 | Haqel | 0.0035 | 0.0288 | 0.0085 | 0.0403 | 2.9374 | 0.0066 | 0.0016 | 0.2329 | 0.0051 | 0.0088 | 0.0052 | 0.0000 | 0.4494 | 0.0083 |
MCFO-0526 | Solnhofen | 0.0022 | 0.0391 | 0.0115 | 0.0222 | 4.0393 | 0.0043 | 0.0008 | 0.1237 | 0.0035 | 0.0058 | 0.0053 | 0.0000 | 0.2268 | 0.0054 |
R-drk | Montsec | 0.0029 | 0.0353 | 0.0106 | 0.0227 | 3.7724 | 0.0071 | 0.0005 | 0.1867 | 0.0046 | 0.0057 | 0.0054 | 0.0000 | 0.1678 | 0.0103 |
R-wht | Montsec | 0.0032 | 0.0380 | 0.0102 | 0.0300 | 3.7859 | 0.0128 | 0.0015 | 0.3440 | 0.0049 | 0.0052 | 0.0046 | 0.0000 | 0.1211 | 0.0052 |
C | Montsec | 0.0015 | 0.0388 | 0.0137 | 0.0208 | 4.0036 | 0.0049 | 0.0003 | 0.1698 | 0.0044 | 0.0061 | 0.0051 | 0.0000 | 0.1453 | 0.0041 |
LH1 | Las Hoyas | 0.0016 | 0.0376 | 0.0166 | 0.0196 | 3.4479 | 0.0079 | 0.0012 | 0.2988 | 0.0041 | 0.0092 | 0.0047 | 0.0000 | 0.6435 | 0.0125 |
LH2 | Las Hoyas | 0.0015 | 0.0390 | 0.0155 | 0.0167 | 3.5759 | 0.0047 | 0.0017 | 0.2196 | 0.0062 | 0.0067 | 0.0082 | 0.0000 | 0.7874 | 0.0109 |
MGB PR-10378 | Solnhofen | 0.0009 | 0.0430 | 0.0196 | 0.0070 | 4.3715 | 0.0011 | 0.0012 | 0.0304 | 0.0069 | 0.0069 | 0.0145 | 0.0000 | 0.2242 | 0.0185 |
GB PR-10347 | Solnhofen | 0.0003 | 0.0474 | 0.0140 | 0.0132 | 4.2524 | 0.0023 | 0.0014 | 0.0826 | 0.0057 | 0.0061 | 0.0301 | 0.0000 | 0.2181 | 0.0218 |
paraloid 10% | Montsec | 0.0003 | 0.0342 | 0.0093 | 0.0161 | 3.2536 | 0.0079 | 0.0008 | 0.1865 | 0.0066 | 0.0060 | 0.0080 | 0.0000 | 0.1333 | 0.0049 |
paraloid 5% | Montsec | 0.0016 | 0.0341 | 0.0090 | 0.0180 | 3.4406 | 0.0105 | 0.0010 | 0.2283 | 0.0039 | 0.0049 | 0.0070 | 0.0000 | 0.1358 | 0.0046 |
paraloid 0% | Montsec | 0.0021 | 0.0445 | 0.0099 | 0.0145 | 4.1477 | 0.0060 | 0.0007 | 0.1299 | 0.0039 | 0.0044 | 0.0053 | 0.0000 | 0.1355 | 0.0139 |
Crn | Cerin | 0.0000 | 0.0401 | 0.0126 | 0.0061 | 3.8339 | 0.0046 | 0.0012 | 0.0305 | 0.0042 | 0.0024 | 0.0066 | 0.0000 | 0.1043 | 0.0080 |
Kr | Karatu | 0.0008 | 0.0172 | 0.0062 | 0.0095 | 1.1201 | 0.0151 | 0.0024 | 0.9903 | 0.0053 | 0.0036 | 0.0119 | 0.0065 | 1.5199 | 0.0390 |
Mnt-Alc | MontRal-Alcover | 0.0086 | 0.0058 | 0.0042 | 0.0324 | 0.5287 | 0.0353 | 0.0032 | 0.5737 | 0.0066 | 0.0025 | 0.0052 | 0.0012 | 0.2251 | 0.0122 |
Ock | Ockley | 0.0060 | 0.0040 | 0.0008 | 0.0774 | 0.0839 | 0.2013 | 0.0348 | 14.8936 | 0.0066 | 0.0138 | 0.0112 | 0.0604 | 0.0536 | 0.0144 |
Ock | Ockley | 0.0080 | 0.0040 | 0.0001 | 0.0808 | 0.0849 | 0.2028 | 0.0359 | 15.7104 | 0.0093 | 0.0146 | 0.0107 | 0.0618 | 0.0564 | 0.0213 |
RMr | Rubielos de Mora | 0.0026 | 0.0077 | 0.0058 | 0.0618 | 0.7595 | 0.0286 | 0.0050 | 1.3111 | 0.0060 | 0.0100 | 0.0097 | 0.0812 | 0.3793 | 0.0110 |
Dhg | Daohugou | 0.0064 | 0.0036 | 0.0035 | 0.0430 | 0.0338 | 0.0159 | 0.0021 | 0.7439 | 0.0031 | 0.0070 | 0.0061 | 0.0859 | 0.0881 | 0.0261 |
Slnhf-1 | Solnhofen | 0.0119 | 0.0201 | 0.0053 | 0.0038 | 1.7998 | 0.0027 | 0.0007 | 0.0257 | 0.0033 | 0.0117 | 0.0113 | 0.0000 | 0.0823 | 0.0051 |
Slnhf-2 | Solnhofen | 0.0059 | 0.0162 | 0.0059 | 0.0086 | 1.5040 | 0.0053 | 0.0007 | 0.2299 | 0.0062 | 0.0097 | 0.0039 | 0.0000 | 0.0502 | 0.0066 |
Crt-Brsl | Crato | 0.0017 | 0.0460 | 0.0138 | 0.0103 | 4.0442 | 0.0035 | 0.0012 | 0.4043 | 0.0072 | 0.0395 | 0.0101 | 0.0000 | 0.5558 | 0.0031 |
Aix-P1 | Aix-en-Provence | 0.0054 | 0.0295 | 0.0146 | 0.0107 | 2.6703 | 0.0034 | 0.0008 | 0.1194 | 0.0057 | 0.0049 | 0.0083 | 0.0000 | 3.2992 | 0.0204 |
Aix-P2 | Aix-en-Provence | 0.0068 | 0.0060 | 0.0037 | 0.0101 | 0.6566 | 0.0040 | 0.0007 | 0.1401 | 0.0024 | 0.0017 | 0.0028 | 0.0000 | 0.1710 | 0.0036 |
Aix-P3 | Aix-en-Provence | 0.0088 | 0.0190 | 0.0075 | 0.0227 | 2.0929 | 0.0054 | 0.0004 | 0.2497 | 0.0034 | 0.0034 | 0.0052 | 0.0000 | 0.2797 | 0.0073 |