Evolution of tropical watersheds and continental hydrology during the Late Cretaceous greenhouse; impact on marine carbon burial and possible implications for the future

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doi: 10.1016/j.epsl.2008.06.011
Author(s): Flögel, S.; Beckmann, B.; Hofmann, P.; Bornemann, A.; Westerhold, T.; Norris, R. D.; Dullo, C.; Wagner, T.
Author Affiliation(s): Primary:
Leibniz-Institute of Marine Science, Kiel, Federal Republic of Germany
Other:
University of Cologne, Federal Republic of Germany
University of Leipzig, Federal Republic of Germany
Bremen University, Federal Republic of Germany
Scripps Institution of Oceanography, United States
Newcastle University, United Kingdom
Volume Title: Earth and Planetary Science Letters
Source: Earth and Planetary Science Letters, 274(1-2), p.1-13. Publisher: Elsevier, Amsterdam, Netherlands. ISSN: 0012-821X CODEN: EPSLA2
Note: In English. 80 refs.; illus., incl. 1 table, sketch map
Summary: Regional climate modelling for the Late Cretaceous greenhouse and high-resolution marine stratigraphic records from both sides of the low latitude Atlantic show that tropical South American and African hydrology and watersheds had a strong effect on freshwater transfer into the Equatorial Atlantic and subsequently the marine carbon record. This conclusion is derived from new detailed geochemical records from Demerara Rise off Suriname drilled at Ocean Drilling Program (ODP) Site 1261 combined with frequency analyses and climate simulations providing evidence for mainly eccentricity-driven changes in carbon burial in the western tropical Atlantic. Shorter orbital frequencies, in particular precession, clearly dominating black shale cycles off tropical Africa (ODP Site 959), are far less dominant at Demerara Rise despite comparable time resolution of the geochemical records. We suggest that these different frequency patterns in carbon burial were related to the regional evolution of Cretaceous watersheds and hydrology in tropical South America and Africa. River discharge deduced from simulations indicates higher and less variable discharge from South America compared to western Africa at that time. This runoff pattern would have supported more permanent anoxic conditions off South America compared to Africa, at least indirectly, and caused the lack of strong higher frequency geochemical cycles in the western sector of the Equatorial Atlantic. Furthermore, climate simulations show a general switch of primary runoff from either side of the Cretaceous Equatorial Atlantic every half precession cycle (i.e. every ≈10 kyr). Similarities between the developments of Cretaceous and Holocene hydrology in the tropical Atlantic area imply that orbital-scale evolution of watersheds is a robust feature through time that is independent from the mean global climate state. Based upon the comparison of Cretaceous and Holocene trends in hydrology we infer that future hydrology in the study region may develop in a comparable direction to the one observed in the Cretaceous. If true, this suggests that the modern Amazon rain forest could shrink over the next millennium due to a ≈30% loss of moisture while the Congo rain forest in Africa is likely to expand in response to a 14% gain in moisture. Abstract Copyright (2008) Elsevier, B.V.
Year of Publication: 2008
Research Program: ODP Ocean Drilling Program
Key Words: 12 Stratigraphy, Historical Geology and Paleoecology; 22 Environmental Geology; Africa; Atlantic Ocean; Biostratigraphy; Burial; Carbon; Carbon dioxide; Climate change; Climate forcing; Cretaceous; Demerara Rise; Discharge; Eccentricity; Eh; Equatorial Atlantic; Forests; Fresh water; Future; Geochemical cycle; Geochemistry; Greenhouse effect; Hydrology; Leg 159; Leg 207; Marine environment; Mesozoic; Models; Moisture; North Atlantic; Northwest Atlantic; ODP Site 1261; ODP Site 959; Ocean Drilling Program; Orbital forcing; Paleoclimatology; Paleogeography; Paleohydrology; Precession; Rain forests; Sedimentation rates; Simulation; South America; Upper Cretaceous; Watersheds
Coordinates: N033740 N033740 W0024408 W0024408
N090300 N090300 W0541900 W0541900
Record ID: 2009016876
Copyright Information: GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from CAPCAS, Elsevier Scientific Publishers, Amsterdam, Netherlands