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[1] The Pacific Ocean is the largest water body on Earth, and circulation in the Pacific contributed significantly to climate evolution in the latest Cretaceous, the culmination of a period of long-term cooling. Here, we present new high-resolution late Campanian to Maastrichtian benthic and planktic foraminiferal stable isotope data and a neodymium (Nd) isotope record obtained from sedimentary ferromanganese oxide coatings of Ocean Drilling Program Hole 1210B from the tropical Pacific Ocean (Shatsky Rise). These new records resolve 13 million years in the latest Cretaceous, providing insights into changes in surface and bottom water temperatures and source regions of deep to intermediate waters covering the carbon isotope excursions of the Campanian-Maastrichtian Boundary Event (CMBE) and the Mid-Maastrichtian event (MME). Our new benthic foraminiferal δ 18O and Nd isotope records together with published Nd isotope data show markedly parallel trends across the studied interval over a broad range of bathyal to abyssal water depths interpreted to reflect changes in the intensity of deep-ocean circulation in the tropical Pacific. In particular, we observe a three-million-year-long period of cooler conditions in the early Maastrichtian (72.5 to 69.5 Ma) when a concomitant change toward less radiogenic seawater Nd isotope signatures probably marks a period of enhanced admixture and northward flow of deep waters with Southern Ocean provenance. We suggest this change to have been triggered by intensified formation and convection of deep waters in the high southern latitudes, a process that weakened during the MME (69.5 to 68.5 Ma). The early Maastrichtian cold interval is closely related to the negative and positive carbon isotope trends of the CMBE and MME. The millions-of-years long duration of these carbon cycle perturbations suggests a tectonic forcing of climatic cooling, possibly related to changes in ocean basin geometry and bathymetry.

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Chronic treatment with the LHRH agonist D-Ser(TBU)6-LHRH (1-9)-EA (buserelin) has been suggested as a contraceptive method since it has been shown to inhibit ovulation. To elucidate the mechanism of this paradoxical action, we investigated the pattern of gonadotrophin and steroid secretion after the daily intranasal application of 300 micrograms of the agonist. Ten volunteers with ovulatory cycles received the analogue from Day 1 to Day 22 and 5 mg norethisterone acetate from Day 16 to Day 22. Blood samples were taken on Day 1, 15, and 21 every 15 min for 6 h after the application of the agonist. LH secretion was increased nine-fold on the first treatment day as compared to Day 2 of the preceding control cycle. Thereafter, it decreased slowly but was still elevated five-fold on Day 21 of treatment. FSH release increased three-fold on Day 1 but decreased thereafter to values similar to those of the controls. During treatment with the analogue, the LH/FSH ratio changed from 1.3 (controls) to 3.8 on Day 1 and to 5.5 on Day 15 and 21 of treatment. Although the ovary retained follicular activity, ovulation was inhibited in every treatment cycle. This seemed to be due to an impairment of follicular steroid synthesis as indicated by a significant increase of 17 alpha-hydroxyprogesterone and testosterone levels for several hours after the application of the analogue. It appears that at least during the first treatment cycle of daily administration of buserelin the abolishment of pulsatile gonadotrophin release, and the abnormally increased ratio of LH/FSH secretion may possibly impair follicular maturation and thus contribute to the inhibition of ovulation.