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Carotane

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123:. The two guesses as to the reason were that it was a biological phenomenon within the species or that the species had just degraded. Using chromatography with He as a carrier gas, degradation was visible in the samples. There was found to be a presence of beta and gamma carotane derivatives. The derivatives were cross-referenced with synthesized derivatives that were produced via the catagenesis of beta carotene through hydrous pyrolysis. 36: 25: 101:
Carotane was first measures in the Green River Formation. It was discovered using gas-liquid chromatography and GC/MS. The sample was purified with a thin layer of Ag silica, and larger samples of 5 μg were used to give more accurate results and reduce the noise in the MS peaks. What was found was
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Given its long degradation time, carotane acts as an important biomarker Given how long it is preserved. It remains best in sediment and oil environments where it can last years. Beta-carotane, in specific, acts as a biomarker for saline and low lacustrine environments. This means carotane can be
88:. However, where carotene has double bonds, carotane only has single bonds. This is the only difference in the structure given that carotane represents the degradation of carotene. Given the length of time it takes to degrade carotane, the species allows for a more extensive geologic record. 81:. These colors are beneficial to their host species that tend to be plants and algae. Within plants, carotenoids play the major roles of allowing light to be absorbed via photosynthesis as well ad providing photoprotection through a non-photochemical quenching. 120: 334:"Identification of carotane breakdown products in the 1.64billion year old Barney Creek Formation, McArthur Basin, northern Australia" 279:"Geochemical significance of β-carotane in lacustrine oils from the Shahejie Formation of the Dongying Depression, eastern China" 390: 140: 333: 278: 84:
The tetraterpene is also a product of the degradation of carotene and thus represents an important
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The Barney Creek Study was set up to determine why deep levels of carotane did not exist in the
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Wang, Qianru; Huang, Haiping; Li, Zheng; Ma, Yong; Zeng, Jianhui; Larter, Steve (2021-06-01).
223: 385: 345: 290: 235: 8: 349: 294: 239: 314: 259: 204: 77:. These tetraterpenes are known for their yellow, orange, and red colors as these are 361: 357: 318: 306: 302: 251: 196: 188: 263: 208: 353: 298: 243: 178: 247: 167:"Carotenoids 2: Genetics and molecular biology of carotenoid pigment biosynthesis" 78: 183: 166: 379: 365: 310: 192: 255: 70: 200: 74: 85: 111:
used as a biomarker to identify previous water-based habitats.
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Murphy, Mary T. J.; McCormick, A.; Eglinton, G. (1967-09-01).
24: 221: 165:Armstrong, G. A.; Hearst, J. E. (February 1996). 377: 164: 224:"Perhydro-β-Carotene in the Green River Shale" 69:is a plant pigment that belongs to a class of 332:Lee, Carina; Brocks, Jochen J. (2011-05-01). 276: 331: 182: 91: 96: 378: 102:the degradation results of carotene. 13: 14: 402: 52:) compared to that of carotene (C 358:10.1016/j.orggeochem.2011.02.006 303:10.1016/j.orggeochem.2021.104241 34: 23: 114: 105: 325: 270: 215: 158: 133: 1: 248:10.1126/science.157.3792.1040 126: 44:The structure of carotane (C 7: 184:10.1096/fasebj.10.2.8641556 10: 407: 145:Linus Pauling Institute 121:Barney Creek Formation 92:Measurement techniques 391:Green River Formation 97:Green River Formation 338:Organic Geochemistry 283:Organic Geochemistry 350:2011OrGeo..42..425L 295:2021OrGeo.15604241W 240:1967Sci...157.1040M 234:(3792): 1040–1042. 398: 370: 369: 329: 323: 322: 274: 268: 267: 219: 213: 212: 186: 162: 156: 155: 153: 152: 137: 79:organic pigments 38: 27: 406: 405: 401: 400: 399: 397: 396: 395: 376: 375: 374: 373: 330: 326: 275: 271: 220: 216: 163: 159: 150: 148: 139: 138: 134: 129: 117: 108: 99: 94: 64: 63: 62: 61: 59: 55: 51: 47: 41: 40: 39: 30: 29: 28: 17: 12: 11: 5: 404: 394: 393: 388: 372: 371: 344:(4): 425–430. 324: 269: 214: 177:(2): 228–237. 157: 131: 130: 128: 125: 116: 113: 107: 104: 98: 95: 93: 90: 57: 53: 49: 45: 43: 42: 33: 32: 31: 22: 21: 20: 19: 18: 15: 9: 6: 4: 3: 2: 403: 392: 389: 387: 384: 383: 381: 367: 363: 359: 355: 351: 347: 343: 339: 335: 328: 320: 316: 312: 308: 304: 300: 296: 292: 288: 284: 280: 273: 265: 261: 257: 253: 249: 245: 241: 237: 233: 229: 225: 218: 210: 206: 202: 198: 194: 190: 185: 180: 176: 172: 171:FASEB Journal 168: 161: 146: 142: 141:"Carotenoids" 136: 132: 124: 122: 112: 103: 89: 87: 82: 80: 76: 72: 71:tetraterpenes 68: 37: 26: 16:Plant pigment 341: 337: 327: 286: 282: 272: 231: 227: 217: 174: 170: 160: 149:. Retrieved 147:. 2014-04-28 144: 135: 118: 115:Barney Creek 109: 106:Preservation 100: 83: 66: 65: 386:Carotenoids 75:carotenoids 380:Categories 289:: 104241. 151:2021-09-26 127:References 366:0146-6380 319:235582921 311:0146-6380 193:0892-6638 86:biomarker 264:40339193 256:17770425 209:22385652 67:Carotane 346:Bibcode 291:Bibcode 236:Bibcode 228:Science 201:8641556 73:called 364:  317:  309:  262:  254:  207:  199:  191:  315:S2CID 260:S2CID 205:S2CID 362:ISSN 307:ISSN 252:PMID 197:PMID 189:ISSN 354:doi 299:doi 287:156 244:doi 232:157 179:doi 382:: 360:. 352:. 342:42 340:. 336:. 313:. 305:. 297:. 285:. 281:. 258:. 250:. 242:. 230:. 226:. 203:. 195:. 187:. 175:10 173:. 169:. 143:. 60:). 58:56 54:40 50:78 46:40 368:. 356:: 348:: 321:. 301:: 293:: 266:. 246:: 238:: 211:. 181:: 154:. 56:H 48:H

Index

Carotane
β-Carotene
tetraterpenes
carotenoids
organic pigments
biomarker
Barney Creek Formation
"Carotenoids"
"Carotenoids 2: Genetics and molecular biology of carotenoid pigment biosynthesis"
doi
10.1096/fasebj.10.2.8641556
ISSN
0892-6638
PMID
8641556
S2CID
22385652
"Perhydro-β-Carotene in the Green River Shale"
Bibcode
1967Sci...157.1040M
doi
10.1126/science.157.3792.1040
PMID
17770425
S2CID
40339193
"Geochemical significance of β-carotane in lacustrine oils from the Shahejie Formation of the Dongying Depression, eastern China"
Bibcode
2021OrGeo.15604241W
doi

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