Knowledge (XXG)

Mid-Piacenzian Warm Period

Source 📝

47: 106: 33: 119: 87:
The global average temperature in the mid-Pliocene was 2–3 °C higher than today, global sea level 25 meters higher, and the Northern Hemisphere ice sheet was ephemeral before the onset of extensive glaciation over Greenland that occurred in the late Pliocene around 3 Ma. Global precipitation was
138:
data indicating a northward shift of the tundra and taiga and an expansion of savanna and warm-temperate forest in Africa and Australia. The increased intensity of tropical cyclones during the mPWP has been cited as evidence that intensification of such storms will occur as anthropogenic global
134:. Model simulations of mid-Pliocene climate produce warmer conditions at middle and high latitudes, as much as 10–20 °C warmer than today above 70°N. They also indicate little temperature variation in the tropics. Model-based biomes are generally consistent with Pliocene 834: 645: 102:
of fossilised leaves, although lower estimates of between 330 and 394 ppm over the course of the whole mPWP and 391 ppm in the KM5c interglacial, during the warmest phase of the mPWP, have been given.
775:
Salzmann, U.; Haywood, A. M.; Lunt, D. J. (2009). "The past is a guide to the future? Comparing Middle Pliocene vegetation with predicted biome distributions for the twenty-first century".
898: 777: 286: 541:
Kurschner, W. M.; van der Burgh, J.; Visscher, H.; Dilcher, D. L. (1996). "Oak leaves as biosensors of late Neogene and early Pleistocene paleoatmospheric CO
126:
The mPWP is considered a potential analogue of future climate. The intensity of the sunlight reaching the Earth, the global geography, and
278: 461: 360: 227: 455:
Prescott, Caroline L.; Haywood, Alan M.; Dolan, Aisling M.; Hunter, Stephen J.; Pope, James O.; Pickering, Steven J. (15 August 2014).
158: 403: 130:
concentrations were similar to present. Furthermore, many mid-Pliocene species are extant, helping calibrate paleotemperature
98:
concentration during the Middle Pliocene has been estimated at around 400 ppmv from C/C ratio in organic marine matter and
279:"Mid-Pliocene sea level and continental ice volume based on coupled benthic Mg/Ca palaeotemperatures and oxygen isotopes" 639:
Burke, K. D.; Williams, J. W.; Chandler, M. A.; Haywood, A. M.; Lunt, D. J.; Otto-Bliesner, B. L. (26 December 2018).
506:; Grant, B.; Horowitz, M.; Rau, G. H. (1996). "Mid-Pliocene warmth: Stronger greenhouse and stronger conveyor". 79:, was an interval of warm climate during the Pliocene epoch that lasted from 3.3 to 3.0 million years ago (Ma). 92:, glacial-interglacial cycles existed during the mPWP and it was not a uniform and stable climatic interval. 828:
Yan, Qing; Wei, Ting; Korty, Robert L.; Kossin, James P.; Zhang, Zhongshi; Wang, Huijun (15 November 2016).
580:
De la Vega, Elwyn; Chalk, Thomas B.; Wilson, Paul A.; Bysani, Ratna Priya; Foster, Gavin L. (9 July 2020).
714: 184: 89: 843: 786: 723: 654: 595: 554: 515: 470: 412: 369: 295: 244: 193: 178:
Scotese, Christopher R.; Song, Haijun; Mills, Benjamin J. W.; van der Meer, Douwe G. (1 April 2021).
46: 810: 586: 457:"Assessing orbitally-forced interglacial climate variability during the mid-Pliocene Warm Period" 456: 329: 179: 180:"Phanerozoic paleotemperatures: The earth's changing climate during the last 540 million years" 893: 869: 861: 802: 757: 739: 690: 672: 621: 430: 337: 321: 260: 851: 794: 747: 731: 680: 662: 611: 603: 562: 523: 478: 474: 420: 377: 373: 311: 303: 252: 201: 99: 131: 847: 790: 727: 658: 599: 558: 519: 416: 397:
Rosenbloom, N. A.; Otto-Bliesner, B. L.; Brady, E. C.; Lawrence, P. J. (26 April 2013).
299: 248: 197: 105: 752: 709: 685: 640: 616: 581: 127: 95: 887: 710:"Integrating geological archives and climate models for the mid-Pliocene warm period" 566: 527: 503: 235: 830:"Enhanced intensity of global tropical cyclones during the mid-Pliocene warm period" 814: 205: 32: 333: 135: 398: 118: 88:
marginally increased by 0.09 mm/yr according to CCSM4 simulations. As during the
17: 835:
Proceedings of the National Academy of Sciences of the United States of America
646:
Proceedings of the National Academy of Sciences of the United States of America
607: 482: 382: 355: 153: 865: 743: 676: 582:"Atmospheric CO2 during the Mid-Piacenzian Warm Period and the M2 glaciation" 434: 856: 829: 667: 873: 806: 798: 761: 708:
Haywood, Alan M.; Dowsett, Harry J.; Dolan, Aisling M. (16 February 2016).
694: 625: 425: 325: 307: 356:"Final closure of Panama and the onset of northern hemisphere glaciation" 256: 148: 70: 735: 316: 641:"Pliocene and Eocene provide best analogs for near-future climates" 38:
Mid-Pliocene reconstructed annual sea surface temperature anomaly
399:"Simulating the mid-Pliocene Warm Period with the CCSM4 model" 109:
Mid-Pliocene reconstructed terrain and ice sheet elevation
226:
Robinson, M.; Dowsett, H. J.; Chandler, M. A. (2008).
228:"Pliocene role in assessing future climate impacts" 778:Philosophical Transactions of the Royal Society A 287:Philosophical Transactions of the Royal Society A 8: 899:History of climate variability and change 855: 751: 684: 666: 615: 424: 381: 315: 117: 104: 170: 277:Dwyer, G. S.; Chandler, M. A. (2009). 114:Comparison with present global warming 7: 492:– via Elsevier Science Direct. 215:– via Elsevier Science Direct. 159:Five Million Years of Climate Change 462:Earth and Planetary Science Letters 361:Earth and Planetary Science Letters 25: 354:Bartoli, G.; et al. (2005). 45: 31: 404:Geoscientific Model Development 206:10.1016/j.earscirev.2021.103503 67:) (prior to 2009 known as the 52:δO Benthic foraminifera 0–7 Ma 1: 567:10.1016/0377-8398(95)00067-4 528:10.1016/0377-8398(95)00048-8 915: 608:10.1038/s41598-020-67154-8 483:10.1016/j.epsl.2014.05.030 383:10.1016/j.epsl.2005.06.020 61:Mid-Piacenzian Warm Period 547:Marine Micropaleontology 508:Marine Micropaleontology 77:Pliocene Thermal Maximum 857:10.1073/pnas.1608950113 668:10.1073/pnas.1809600115 475:2014E&PSL.400..261P 374:2005E&PSL.237...33B 799:10.1098/rsta.2008.0200 426:10.5194/gmd-6-549-2013 308:10.1098/rsta.2008.0222 123: 110: 715:Nature Communications 185:Earth-Science Reviews 121: 108: 90:Quaternary glaciation 257:10.1029/2008EO490001 848:2016PNAS..11312963Y 842:(46): 12963–12967. 791:2009RSPTA.367..189S 736:10.1038/ncomms10646 728:2016NatCo...710646H 659:2018PNAS..11513288B 653:(52): 13288–13293. 600:2020NatSR..1011002D 559:1996MarMP..27..299K 520:1996MarMP..27..313R 417:2013GMD.....6..549R 300:2009RSPTA.367..157D 249:2008EOSTr..89..501R 198:2021ESRv..21503503S 139:warming continues. 587:Scientific Reports 124: 111: 785:(1886): 189–204. 294:(1886): 157–168. 16:(Redirected from 906: 878: 877: 859: 825: 819: 818: 772: 766: 765: 755: 705: 699: 698: 688: 670: 636: 630: 629: 619: 577: 571: 570: 553:(1–4): 299–312. 545:concentration". 538: 532: 531: 514:(1–4): 313–326. 500: 494: 493: 491: 489: 452: 446: 445: 443: 441: 428: 394: 388: 387: 385: 351: 345: 344: 342: 336:. Archived from 319: 283: 274: 268: 267: 265: 259:. Archived from 232: 223: 217: 216: 214: 212: 175: 122:Pliocene biomes. 100:stomatal density 49: 35: 21: 18:Pliocene climate 914: 913: 909: 908: 907: 905: 904: 903: 884: 883: 882: 881: 827: 826: 822: 774: 773: 769: 707: 706: 702: 638: 637: 633: 579: 578: 574: 544: 540: 539: 535: 502: 501: 497: 487: 485: 454: 453: 449: 439: 437: 396: 395: 391: 353: 352: 348: 340: 281: 276: 275: 271: 263: 243:(49): 501–502. 230: 225: 224: 220: 210: 208: 177: 176: 172: 167: 145: 136:palaeobotanical 116: 85: 57: 56: 55: 54: 53: 50: 41: 40: 39: 36: 23: 22: 15: 12: 11: 5: 912: 910: 902: 901: 896: 886: 885: 880: 879: 820: 767: 700: 631: 572: 542: 533: 495: 447: 411:(2): 549–561. 389: 368:(1–2): 33–44. 346: 343:on 2011-10-21. 269: 266:on 2011-10-22. 218: 169: 168: 166: 163: 162: 161: 156: 151: 144: 141: 128:carbon dioxide 115: 112: 96:Carbon dioxide 84: 81: 51: 44: 43: 42: 37: 30: 29: 28: 27: 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 911: 900: 897: 895: 892: 891: 889: 875: 871: 867: 863: 858: 853: 849: 845: 841: 837: 836: 831: 824: 821: 816: 812: 808: 804: 800: 796: 792: 788: 784: 780: 779: 771: 768: 763: 759: 754: 749: 745: 741: 737: 733: 729: 725: 721: 717: 716: 711: 704: 701: 696: 692: 687: 682: 678: 674: 669: 664: 660: 656: 652: 648: 647: 642: 635: 632: 627: 623: 618: 613: 609: 605: 601: 597: 593: 589: 588: 583: 576: 573: 568: 564: 560: 556: 552: 548: 537: 534: 529: 525: 521: 517: 513: 509: 505: 499: 496: 484: 480: 476: 472: 468: 464: 463: 458: 451: 448: 436: 432: 427: 422: 418: 414: 410: 406: 405: 400: 393: 390: 384: 379: 375: 371: 367: 363: 362: 357: 350: 347: 339: 335: 331: 327: 323: 318: 313: 309: 305: 301: 297: 293: 289: 288: 280: 273: 270: 262: 258: 254: 250: 246: 242: 238: 237: 229: 222: 219: 207: 203: 199: 195: 191: 187: 186: 181: 174: 171: 164: 160: 157: 155: 152: 150: 147: 146: 142: 140: 137: 133: 129: 120: 113: 107: 103: 101: 97: 93: 91: 82: 80: 78: 74: 72: 66: 62: 48: 34: 19: 839: 833: 823: 782: 776: 770: 722:(1): 10646. 719: 713: 703: 650: 644: 634: 594:(1): 11002. 591: 585: 575: 550: 546: 536: 511: 507: 504:Raymo, M. E. 498: 486:. Retrieved 466: 460: 450: 438:. Retrieved 408: 402: 392: 365: 359: 349: 338:the original 291: 285: 272: 261:the original 240: 234: 221: 211:13 September 209:. Retrieved 189: 183: 173: 125: 94: 86: 76: 68: 64: 60: 58: 469:: 261–271. 73:Warm Period 888:Categories 317:10161/6586 192:: 103503. 165:References 75:), or the 866:0027-8424 744:2041-1723 677:0027-8424 435:1991-9603 894:Pliocene 874:27799528 815:20422374 807:18854302 762:26879640 695:30530685 626:32647351 488:26 April 440:26 April 326:18854304 149:Pliocene 143:See also 71:Pliocene 844:Bibcode 787:Bibcode 753:4757764 724:Bibcode 686:6310841 655:Bibcode 617:7347535 596:Bibcode 555:Bibcode 516:Bibcode 471:Bibcode 413:Bibcode 370:Bibcode 334:3199617 296:Bibcode 245:Bibcode 194:Bibcode 154:El Niño 132:proxies 83:Climate 69:Middle 872:  864:  813:  805:  760:  750:  742:  693:  683:  675:  624:  614:  433:  332:  324:  811:S2CID 341:(PDF) 330:S2CID 282:(PDF) 264:(PDF) 231:(PDF) 870:PMID 862:ISSN 803:PMID 758:PMID 740:ISSN 691:PMID 673:ISSN 622:PMID 490:2024 442:2024 431:ISSN 322:PMID 213:2023 65:mPWP 59:The 852:doi 840:113 795:doi 783:367 748:PMC 732:doi 681:PMC 663:doi 651:115 612:PMC 604:doi 563:doi 524:doi 479:doi 467:400 421:doi 378:doi 366:237 312:hdl 304:doi 292:367 253:doi 236:Eos 202:doi 190:215 890:: 868:. 860:. 850:. 838:. 832:. 809:. 801:. 793:. 781:. 756:. 746:. 738:. 730:. 718:. 712:. 689:. 679:. 671:. 661:. 649:. 643:. 620:. 610:. 602:. 592:10 590:. 584:. 561:. 551:27 549:. 522:. 512:27 510:. 477:. 465:. 459:. 429:. 419:. 407:. 401:. 376:. 364:. 358:. 328:. 320:. 310:. 302:. 290:. 284:. 251:. 241:89 239:. 233:. 200:. 188:. 182:. 876:. 854:: 846:: 817:. 797:: 789:: 764:. 734:: 726:: 720:7 697:. 665:: 657:: 628:. 606:: 598:: 569:. 565:: 557:: 543:2 530:. 526:: 518:: 481:: 473:: 444:. 423:: 415:: 409:6 386:. 380:: 372:: 314:: 306:: 298:: 255:: 247:: 204:: 196:: 63:( 20:)

Index

Pliocene climate


Pliocene
Quaternary glaciation
Carbon dioxide
stomatal density


carbon dioxide
proxies
palaeobotanical
Pliocene
El Niño
Five Million Years of Climate Change
"Phanerozoic paleotemperatures: The earth's changing climate during the last 540 million years"
Earth-Science Reviews
Bibcode
2021ESRv..21503503S
doi
10.1016/j.earscirev.2021.103503
"Pliocene role in assessing future climate impacts"
Eos
Bibcode
2008EOSTr..89..501R
doi
10.1029/2008EO490001
the original
"Mid-Pliocene sea level and continental ice volume based on coupled benthic Mg/Ca palaeotemperatures and oxygen isotopes"
Philosophical Transactions of the Royal Society A

Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.